chia-ray seng, kenneth h. stokoe, ii, and jose m. roesset · ft3 a cub~c feet 0.0328 meters cubed...

127
CTR 2/3-18-88/1-1175-5 EFFECT OF DEPTH TO BEDROCK ON THE ACCURACY OF BACKCALCULATED MODULI OBTAINED WITH DYNAFLECT AND FWD TESTS Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset RESEARCH REPORT 1175-5 Project 2/3-18-88/1-1175 CENTER FOR TRANSPORTATION RESEARCH BUREAU OF ENGINEERING RESEARCH THE UNIVERSITY OF TEXAS AT AUSTIN JANUARY 1993

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Page 1: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

CTR 2/3-18-88/1-1175-5

EFFECT OF DEPTH TO BEDROCK ON THE

ACCURACY OF BACKCALCULATED

MODULI OBTAINED WITH

DYNAFLECT AND FWD TESTS

Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset

RESEARCH REPORT 1175-5

Project 2/3-18-88/1-1175

CENTER FOR TRANSPORTATION RESEARCH BUREAU OF ENGINEERING RESEARCH THE UNIVERSITY OF TEXAS AT AUSTIN

JANUARY 1993

Page 2: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

1. Report No. 2. Government Accession No.

FHWA/TX-93+ 1175-5

4. Title and Subtitle

EFFECT OF DEPTH TO BEDROCK ON THE ACCURACY OF BACKCALCULATED MODULI OBTAINED WITH DYNAFLECT AND FWD TESTS

7. Author(s)

Chia-Ray Seng, Kenneth H. Stokoe II, and jose M. Roesset

9. Performing Organization Name and Address

Center for Transportation Research The University of Texas at Austin Austin, Texas 78712-1075

' CENTER

3.1

5. Report Date january 1993

6. Performing Organization Code

8. Performing Organization Report No.

Research Report 117 5-5

1 0. Work Unit No. (TRAIS)

11. Contract or Grant No. Research Study 2/3-18-88/1-11 7 5

1-~--------~~-=------------------1 13. Type of Report and Period Covered 12. Sponsoring Agency Name and Address

Texas Department of Transportation Transportation Planning Division P. 0. Box 5051 Austin, Texas 78763-5051

-_

15. Supplementary Notes

Interim

14. Sponsoring Agency Code

Study conducted in cooperation with the U.S. Department of Transportation, Federal Highway Administration. Research Study Title: "Development of Dynamic Analysis Techniques for Falling Weight Deflectometer Data"

16. Abstract

The main objective of this study is to investigate the importance of depth to bedrock in surface loading tests. Two surface loading tests, the Dynaflect and Falling Weight Deflectometer (FWD), were investigated analytically using four typical in-service Texas highway pavement profiles.

The dynamic effect of these surface loading tests was in terms of deflection ratios, "dynamic" deflections di­vided by static deflections. "Dynamic" deflections represent those deflections which are actually measured when these tests are performed on real pavements. The amplitude of the deflection ratio is an important index of the potential error generated in any static interpretation procedure. The results show that the stiffness of the subgrade has the most significant effect on the maximum amplitude of the deflection ratio (deflection ratio at resonant conditions). The softer the subgrade is, the higher is the amplitude of the maximum deflection ratio. This behavior agrees with the trend in backcalculated layer moduli using static interpretation programs.

Equations for estimating the resonant depth to bedrock (depth to bedrock corresponding to the maximum deflection ratio) based on the subgrade stiffness are suggested for both the Dynaflect and FWD tests.

For the FWD test, equations are developed for estimating the actual depth to bedrock based on the damped natural period on the free vibrations of the pavement system immediately after the FWD load application. In these equations, the stiffness of the subgrade has a major effect while the degree of saturation of the subgrade is only marginally important.

An approach for estimating the stiffness of the subgrade based on the offset time of the first pulses in the de­flection-time recordings in the FWD test is suggested. The most important advantage of this approach is that the stiffness of the subgrade can be determined simultaneously with performance of the FWD test. Therefore, the actual depth to bedrock and resonant depth to bedrock can be determined and the dynamic effect can be taken into account.

17. Key Words

Field Testing, Analytical Study, Falling Weight Deflectometer, Bedrock Depth, Backcalculated Moduli, Pavements, Subgrades

18. Distribution Statement

No restrictions. This document is available to the public through the National Technical Information Service, Springfield, Virginia 22161.

19. Security Classif. (of this report)

Unclassified

20. Security Classif. (of this page)

Unclassified

21 . No. of Pages 22. Price

124

Form DOT F 1700.7 (8-72) Reproduction of completed page authorized

Page 3: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

EFFECT OF DEPTH TO BEDROCK ON THE ACCURACY OF BACKCALCULATED MODULI OBTAINED WITH

DYNAFLECT AND FWD TESTS

by

Chia-Ray Seng Kenneth H. Stokoe, II

Jose M. Roesset

Research Report 117 S-5

Development of Dynamic Analysis Techniques for Falling Weight Deflectometer Data Research Project 2/3-18-88/1-1175

conducted for the

Texas Department of Transportation

in cooperation with the

U.S. Department of Transportation Federal Highway Administration

by the

CENTER FOR TRANSPORTATION RESEARCH

Bureau of Engineering Research THE UNIVERSITY OF TEXAS AT AUSTIN

january 1993

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ii

Page 5: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

IMPLEMENTATION STATEMENT

In this study, the depth to bedrock is shown to have potentially a significant adverse effect on backcalculated layer moduli in the FWD test. This adverse effect occurs around the resonant bedrock depth, the depth at which reflections from the bedrock create the largest surface motions. Backcalcu­lated subgrade moduli obtained with FWD deflection basins at the resonant depth to bedrock under­estimate the actual subgrade moduli by 20 to SO percent. This results in the backcalculated base moduli being too high (generally 2 times the actual base moduli).

A new procedure for performing the FWD test is suggested. In this new procedure, the stiffness of the subgrade is found in a new way, the actual bedrock depth is found from free vibrations in the test, and the impact of bedrock depth is evaluated in the field. This procedure needs field verification and will require modification of the data acquisition system in the FWD device.

Prepared in cooperation with the Texas Department of Transportation and the U.S. Department of Transportation

DISCLAIMERS

The contents of this report reflect the views of the authors, who are responsible for the facts and the accuracy of the data presented herein. The contents do not necessarily reflect the official views or policies of the Federal Highway Administration or the Texas Department of Transportation. This re­port does not constitute a standard, specification, or regulation.

NOT INTENDED FOR CONSTRUCTION, BIDDING, OR PERMIT PURPOSES

Kenneth H. Stokoe, II (Texas No. 49095) Research Supervisor

iii

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METRIC (SI*) CONVERSION FACTORS

APPROXIMATE CONVERSIONS TO Sl UNITS APPROXIMATE CONVERSIONS FROM Sl UNITS

Symbol When You Know Multiply by To Find Symbol Symbol When You Know Multiply by To Find Symbol

LENGTH "' LENGTH

in Inches 2.54 centimeters em mm millimeters 0.039 Inches in It feet 0.3048 meters m m meters 3.28 feet ft yd yards 0.914 meters m m meters 1.09 yards yd mi miles 1.61 kilometers km km kilometers 0.621 miles mi

"' AREA

AREA mm2 millimeters squared 0.0016 square inches in2

m2 meters squared 10.764 square feet ft2

~ m2 meters squared 1.20 square yards yd 2

in 2 square inches 645.2 millimeters squared mm2 =§ ~ km2 kilometers squared 0.39 square miles mi 2

1t2 square feet 0.0929 meters squared m2 ... ha hectares (10,000 m2) 2.53 acres ac yd2 square yards 0.836 meters squared m2 ml 2 square miles 2.59 kilometers squared km2 ~ ~ MASS (weight) ac acres 0.395 hectares ha

.,. g grams 0.0353 ounces oz

MASS (weight) ---1 L kg kilograms 2.205 pounds lb "' Mg megagrams (1,000 kg) 1.103 short tons T

"' oz ounces 28.35 grams 9 _ . VOLUME lb pounds 0.454 kilograms kg T short tons (2,000 lb) 0.907 megagrams Mg =

mL milliliters 0.034 fluid ounces II oz L liters 0.264 gallons gal m3 meters cubed 35.315 cubic feet ft3

VOLUME ~ ~ m3 meterscubed 1.308 cubicyards yd3

~ §-- TEMPERATURE (exact) II oz fluid ounces 29.57 milliliters mL gal gallons 3.785 liters L -=I ~ OC Celsius 9/5 (then Fahrenheit oF ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

NOTE: Volumes greater than 1,000 l shall be shown in m3. OF OF

32 98.6 212 -40 0 40 80 ~ 120 180 2001

TEMPERATURE(exact) ~ E I 1 1111, •I 1 I 1 1 , 11, 1 I, 1 11,, 1 - I I I I I I I I I !'f -40 -20 0 20 0 60 80 1 00

°F Fahrenheit 5/9 (after Celsius oc ~ 5 OC 3

OC temperature subtracting 32) temperature These factors conform to the requirement of FHWA Order 5190.1 A.

* Sl is the svmbol for the International

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E Q)

E ~ ::i UJ Cd Q)

::.:?! 0 E Q)

1ii 6) cu c 0

~ E .s .E Q)

.r:. -'-0 -0

..0 E ~ Q)

.r:. -.!8 Ci5

TABLE OF CONTENTS

IMPLEMENTATION STATEMENT ....................................................................................... iii

DISCLAIMERS .......................................................................................................................... iii

METRICATION PAGE ............................................................................................................ iv

SUMMARY ................................................................................................................................ vii

CHAPTER 1. INTRODUCTION 1.1 BACKGROUND ............................................................................................................... 1 1.2 OBJECTIVES .................................................................................................................... 2 1.3 ORGANIZATION ............................................................................................................. 2

CHAPTER 2. TEST METHODS, MODEL PROFILES AND COMPUTER ANALYSES 2.1 INTRODUCTION ............................................................................................................ 3 2.2 TEST METHODS ............................................................................................................. 3 2.3 MODEL PROFILES .......................................................................................................... 4 2.4 COMPUTER ANALYSES ................................................................................................. 4

CHAPTER 3. PARAMETRIC STUDY OF THE DYNAFLECT TEST 3.1 INTRODUCTION ............................................................................................................ 7 3.2 MODEL PARAMETERS ................................................................................................... 7 3.3 DEFLECTION BASINS .................................................................................................... 7 3.4 RESONANT DEPTH TO BEDROCK .............................................................................. 9 3.5 AMPLITUDE OF THE MAXIMUM DEFLECTION RATIO ........................................ 14 3.6 SUMMARY ..................................................................................................................... 17

CHAPTER 4. PARAMETRIC STUDY OF THE FALLING WEIGHT DEFLECTOMETER TEST

4.1 INTRODUCTION .......................................................................................................... 19 4.2 MODEL PARAMETERS ................................................................................................. 19 4.3 DEFLECTION BASINS .................................................................................................. 22 4.4 RESONANT DEPTH TO BEDROCK ............................................................................ 23 4.5 AMPLITUDE OF THE MAXIMUM DEFLECTION RATIO ........................................ 25 4.6 ESTIMATION OF DEPTH TO BEDROCK FROM THE FWD TEST ........................ 26

4.6.1 Unsaturated Sub grade Conditions .................................................................... 26 4.6.2 Saturated Sub grade Conditions ........................................................................ 30

4.7 ESTIMATION OF THE SUBGRADE STIFFNESS FROM FWD TESTS .................................................................................. 31

4.8 SUMMARY ..................................................................................................................... 32

v

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CHAPTER 5. INFLUENCE OF DYNAMIC DEFLECTIONS ON BACKCALCULATED LAYER MODULI IN THE FWD TEST

5.1 INTRODUCTION .......................................................................................................... 35 5.2 MODEL PARAMETERS ................................................................................................. 35 5.3 DEFLECTION BASINS .................................................................................................. 35 5.4 BACKCALCULATION OF LAYER MODULI OBTAINED FROM

PROGRAM MODULUS ................................................................................................. 37 5.4.1 Profile 1 ............................................................................................................ 37

Subgrade Moduli of Profile 1 ........................................................................... 37 Base Moduli of Profile 1 .................................................................................. 42 AC Moduli of Profile 1 .................................................................................... 42

5.4.2 Profile 2 ............................................................................................................ 43 Sub grade Moduli of Profile 2 ........................................................................... 43 Base Moduli of Profile 2 .................................................................................. 43 AC Moduli of Profile 2 .................................................................................... 43

5.4.3 Profile 3 ............................................................................................................ 44 Sub grade Moduli of Profile 3 ........................................................................... 44 Base Moduli of Profile 3 .................................................................................. 44 A C Moduli of Profile 3 .................................................................................... 45

5.4.4 Profile 4 ............................................................................................................ 45

i ,;

Subgrade Moduli of Profile 4 ........................................................................... 45 Subbase Moduli of Profile 4 ............................................................................ 45 AC Base Moduli of Profile 4 ........................................................................... 45 CRC Moduli of Profile 4 .................................................................................. 45

5.5 SUMMARY ..................................................................................................................... 46

CHAPTER 6. CONCLUSIONS AND RECOMMENDATIONS 6.1 CONCLUSIONS REGARDING THE DYNAFLECT TEST .......................................... .47 6.2 CONCLUSIONS REGARDING THE FWD TEST ....................................................... .47 6.3 RECOMMENDATIONS ................................................................................................. 48

BIBLIOGRAPHY .............................................. , ....................................................................... 51 ·

APPENDIX A. RESULTS OF ANALYTICAL SIMULATION OF THE DYNAFLECT TEST .............................................. , .......................... 53

APPENDIX B. RESULTS OF ANALYTICAL SIMULATION OF THE FWD TEST ........................................................... .......................... 1 03

APPENDIX C. DEFLECTION-TIME RECORDS IN THE FWD TEST .................... 113

vi

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SUMMARY

Analytical simulations of the Dynaflect and Falling Weight Deflectometer (FWD) tests were performed on four typical in-service pavement profiles (three flexible pavements and one rigid pavement). Stiffnesses of the pavement surface layer, base, subbase, and subgrade were varied over ranges typical of in-service pavements. Depths to bedrock below the pavement surface varied from a few feet to over 100 feet (30 m).

The effect of depth to bedrock (also referred to as the "dynamic" effect) was expressed in terms of deflection ratios ("dynamic" deflections divided by static deflections). "Dynamic" deflections represent those deflections which are actually measured when these tests are performed on pavements. The amplitude of the deflection ratio is an important index of the potential error generated in any static interpretation procedure. The results show that the stiffness of the subgrade has the most significant effect on the maximum amplitude of the deflection ratio (deflection ratio at resonant conditions). The softer the subgrade, the higher the amplitude of the maximum deflection ratio. This behavior agrees with the trend in backcalculated layer moduli using static interpretation programs.

In the Dynaflect test, the resonant depth to bedrock (the depth to bedrock corresponding to the maximum deflection ratio) is determined predominately by the stiffness of the subgrade layer. Two sets of equations (one for the flexible pavements and one for the rigid pavement) were developed for esti­mating the resonant depth to bedrock based on the subgrade stiffness. For these pavements, Young's modulus of the subgrade varied from 16 to 142 ksi (0.11 to 0.98 MN/m2), and the resonant depth to bedrock ranged from 25 to 85 feet (7.8 to 26.3 m).

As in the case of the Dynaflect test, the maximum deflection ratio at a given depth to bedrock also occurs at the farthest measurement station (station 7) in the FWD test. However, the resonant peak exhibited in the FWD deflection ratios is much wider than that in the Dynaflect test, and decreases more slowly to 1 when compared with the sharp decrease in the deflection ratio in the FWD test. The reason for these differences is that the FWD test contains a wide range in frequencies, while the Dynaflect test contains one frequency (8 Hz).

The resonant depth to bedrock obtained with the FWD test varied from 5.5 to 20 feet (1.7 to 6.2 m) when Young's modulus of the subgrade varied from 16 to 142 ksi (0.11 to 0.98 MN/m2). These reso­nant depths to bedrock are much shallower than those obtained with the Dynaflect test (varied from 25 to 85 feet [7.8 to 26.3 m}). This trend occurs because the predominate frequency in the FWD test is about 30 Hz, while the frequency used in the Dynaflect test is 8 Hz. Therefore, the resonant depths to bedrock obtained with the FWD test are approximately one fourth of those obtained with the Dynaflect test. Equations for estimating the resonant depth to bedrock for the FWD test were devel­oped for both the flexible and rigid pavements.

vii

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CHAPTER 1.

1.1 BACKGROUND

In the last two decades, nondestructive testing has become widely used for the structural evalua­tion of pavement systems and the backcalculation of layer moduli. Nondestructive tests for this pur­pose can be divided into two main categories: sur­face loading tests and stress wave tests. Surface loading tests are by far the most widely used. In these tests, pavement structure and layer moduli are interpreted from the load-deformation response of the pavement system. Dynamic loading devices (e.g., Road Rater, Dynaflect, and Falling Weight Deflectometer) have become popular devices for performing surface loading tests. In particular, the Falling Weight Deflectometer (FWD) has gained wide acceptance in the past decade. Some of the primary reasons for its popularity are that:

1. field operation is relatively simple, fast, and economical;

2. relatively large loads can be applied to the pavement surface; and

3. simplified procedures have been developed for depth analysis.

The other general category of nondestructive pavement tests for structural evaluation and layer moduli is stress wave tests. These tests are based on generating stress waves at one point in the pavement structure and measuring the times re­quired for the waves to propagate to other points in the pavement structure. Some examples of stress wave tests are:

1. the impact-echo test for measuring the thick­nesses of concrete slabs which are similar to the surface layer of rigid pavements (Sansa­lone and Carino, 1989);

2. the crosshole seismic method for evaluating the moduli of the pavement layers (Heisey, 1981); and

3. the Spectral-Analysis-of-Surface-Waves Method (SASW) for evaluating layer moduli of pave­ments (Nazarian and Stokoe, 1984).

INTRODUCTION

1

Even though these methods have a strong theo­retical basis, they have been used sparingly in pavement studies because they can be time con­suming to use in the field, they presently require significant expertise to interpret, and they only load the pavement materials at very small strains.

In the case of surface loading tests, the main problem in pavement evaluations arises in inter­pretation of the field data that has been per­formed in the simplified analyses. The field data are motions of the pavement surface at various distances from the dynamically loaded area. In­terpretation of these motions has been based on static analyses. However, the Road Rater, Dyna­flect, and Falling Weight Deflectometer all load the pavement dynamically, and static analyses cannot take the dynamic response of the pave­ment system into account (Roesset and Shao, 1985; Uzan et al, 1989). Previous work has shown that the static and dynamic responses of a pavement may be significantly different (Davies and Mamlouk, 1985; and Roesset and Shao, 1985).

Besides dynamic effects, nonlinear behavior of the pavement, base, and subgrade may also oc­cur in the surface loading tests. Early work per­formed by Nazarian and Stokoe (1987) using an approximate nonlinear characterization shows that nonlinear behavior in the base and subgrade can be significant at large amplitude loadings, such as the 20-kip (89 kN) load applied in the FWD test. Chang et al (1992), using refined non­linear models combined with a finite element analysis, conducted a series of studies on the effects of nonlinear behavior on the dynamic response of pavements. They showed that non­linear behavior can be significant and localized around a heavily loaded area if testing is per­formed on a flexible pavement with a rather thin surface layer and a soft subgrade. However, they also showed that only the dynamic response of the pavement system needs to be considered at small to intermediate loads for many pavement systems, and that very little nonlinearity can be generated in heavy, rigid pavements.

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i'

1.2 OBJECTIVES

The main objective of this study is to investi­gate the importance of dynamic loading in surface loading tests. Two surface loading tests, the Dynaflect and Falling Weight Deflectometer, have been investigated using computer programs devel­oped by J. M. Roesset and his graduate students at The University of Texas at Austin (Chang, 1991; Chang et al, 1992). Testing was simulated at pave­ment profiles modeled after four pavement sys­tems in Texas. The dynamic character of the sur­face loading tests was properly taken into account in these analytical studies. Therefore, surface motions measured under the dynamic loads could be compared with movements which would be determined by a static analysis of the surface test, as presently done in the profession.

For both Dynaflect and FWD tests, the deflec­tion basins obtained from the dynamic surface loading were compared with deflection basins which would be obtained if a static loading had occurred. The differences between the basins were studied because they imply the magnitude of errors which result from backcalculation of moduli by static interpretations. As it turns out, the depth to bedrock (distance from the pave­ment surface to the top of bedrock) is an impor­tant factor in dynamic surface loading tests. Depth to bedrock was, therefore, also studied by using the four model pavement systems and varying the thickness of the subgrade in each pavement system.

1.3 ORGANIZATION

The test methods, model profiles, and com­puter analyses are presented in Chapter 2.

2

Parametric studies on the effect of depth to bed­rock on the pavement motions measured in the Dynaflect and FWD tests are presented in Chapter 3 and Chapter 4, respectively. The differences of dynamic motions and static motions are expressed in terms of deflection ratios; that is, the dynamic deflections measured during testing divided by the deflections under an equivalent static load (called the static deflections). For each test, variations in the amplitude of deflection ratios with various depths to bedrock and different stiffness combina­tions of the pavement layers are presented.

To aid in identifying problems in applying the Dynaflect and FWD tests at sites with shallow bedrock conditions, equations to predict the depth to bedrock where the maximum dynamic effect will occur is suggested for the Dynaflect test in Chapter 3 and for the FWD test in Chapter 4. An approach to determining if bedrock conditions are adversely affecting the FWD measurements in the field and an approach to estimating the depth to bedrock from the free vibration of the pave­ment system in extended deflection-time records in the FWD test are also developed in Chapter 4. Finally, a new way of estimating the stiffness of the subgrade from the time lag between deflec­tions measured at station 5 and station 7 in the FWD test is presented in Chapter 4.

Potential errors in layer moduli from backcal­culations based on static analyses can be related to the magnitude of the deflection ratios. These errors were investigated in the FWD test with the aid of the static analysis program, MODULUS (Uzan et al, 1989). These results are presented in Chapter 5.

Conclusions and recommendations for use in field testing with the Dynaflect and FWD tests are presented in Chapter 6.

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CHAPTER 2. TEST METHODS, MODEL PROFILES AND COMPUTER ANALYSES

2.1 INTRODUCTION

The two surface loading tests which were stud­ied analytically herein are the Dynaflect and FWD tests. The characteristics of each loading system which were modeled are discussed in this chap­ter. The pavement profiles that were used in the studies are then presented. Finally, the assump­tions and limitations of the computer programs used in these studies are discussed.

2.2 TEST METHODS

The Dynaflect was the first nondestructive test studied. The loading system of the Dynaflect con­sists of two counter-rotating eccentric masses, each of which generates a 500-pound (2.24-kN) harmonic (steady-state) load at a frequency of 8 Hz. The deflection basin is measured with five vertical velocity transducers spaced at 12-inch (30 em) intervals along a center line. The position of the geophones (vertical velodty transducers) with

respect to the loading wheels is shown schemati­cally in Figure 2.1a.

The FWD was the second nondestructive test studied. The analyses that were conducted used the FWD test more often than the Dynaflect test because the FWD test is more widely used. The FWD test has a hydraulically lifted drop weight that generates an impulsive force on the pave­ment surface. The resulting deflections are mea­sured by a set of seven vertical velocity transduc­ers. The configuration of the FWD test is shown schematically in Figure 2.1b. The simplified load­ing history of the FWD test and its correspond­ing load spectrum are shown in Figure 2.2. It should be noted that the peak magnitude of the load is taken as one unit, where the unit can be 1 pound (0.44 N). Since a linear system is as­sumed (see Section 2.4), one only has to multiply the calculated deflections by the magnitude of the actual load to obtain the actual deflections that would be measured under that load, assuming no nonlinear behavior.

X Peak Load = 500 lb, f = 8 Hz

Impulsive Load (Shown in Fig. 2.2)

P(t)

I I I

Receiver Number and Location

,/ Scale: 1.0 ft ,... ...,

5

~Peak Load = 500 lb, f = 8 Hz

(a) Plan view of Dynaflect test

2 3 4 5

(b) Cross-sectional view of FWD test

Figure 2. 7 Schematic configurations of Dynaflect and FWD tests

3

6 7

Scale: 1 .0 ft ,... ...1

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--~----------------------------------------------------~--------------------~-------

1.2 .----.,.---.-----,r-----r----.

1.0

Q) 0.8 "0 ;:, ...., '2 0.6 C'l (tS

2 0.4

0.2

8

Q)

-g 6 ...., '2 C'l (tS 4 2

2

Note: peak amplitude is 1 unit.

0.02 0.04 0.06 0.08 0.10 Time (sec)

(a) Loading history of FWD test

OL_~~-L~~~~==~~ 0 40 60 80 100 120

Frequency (Hz)

(b) Load spectrum of FWD test

Figure 2.2 Simplified loading history of FWD test and its corresponding load spectrum (from Chang, 1991)

2.3 MODEL PROFILES

Four typical in-service Texas highways were se­lected for use as models in these analyses. They are: FM137 (Profile 1) near Paris, FM195 (Profile 2) near Paris, Route 1 (Profile 3) near Austin, and Interstate Highway 10 (Profile 4) near El Paso. Each profile is modeled as a horizontally layered stratum which is infinitely wide. The infinite width has essentially no effect on the results from surface loading tests, as long as the test is per­formed at least 4 feet (1.2 m) from the pavement edge (Kang, 1990; Kang et al, 1991). Therefore, all tests on these model profiles are assumed to meet the above requirement.

The idealized cross-sections of the four test profiles are illustrated in Figure 2.3. Three of the

4

profiles (Profiles 1, 2, and 3) are flexible pavement systems composed of an asphalt concrete (AC) layer, a granular base, and a soil subgrade. Profile 4 is a rigid pavement system which is composed of a continuously reinforced concrete (CRC) layer, an AC base, a granular subbase, and a soil sub­grade. The material properties of the four pave­ment profiles are given in Table 2.1. As can be seen in the table, the thicknesses of all layers except the subgrade layer were fixed. The thick­ness of the subgrade layer was varied from 5 to 120 feet (1.5 to 36 m) for the study of the Dynaflect test, and varied from 5.5 to 90 feet (1.7 to 27.4 m) for the study of the FWD test. A smaller range of depth to bedrock was used in the study of the FWD test because the resonant con­ditions of the FWD test occur at shallow depths.

The stiffnesses of the pavement layers were varied in these studies. The stiffnesses used in the Dynaflect and FWD studies are presented in Chapter 3 and Chapter 4, respectively.

2.4 COMPUTER ANALYSES

Computer programs UTDYNF and UTFWD were used in the Dynaflect and FWD studies, respec­tively. These programs were developed by J. M. Roesset and Der-Wen Chang at The University of Texas at Austin (Chang, 1991; Chang et al, 1992). Both UTDYNF and UTFWD use a Green's flexibil­ity influence function to simulate the dynamic response corresponding to a vertical disk load applied on a simplified pavement system. In the computer programs, the pavement profiles are modeled as an axisymetric and horizontally lay­ered stratum. The effect of finite width cannot be taken into account. As mentioned in Section 2.3, Kang et al (1991) suggested that, as long as the test is conducted 4 feet (1.2 m) from the edge of pavement, the effect of finite width is insignifi­cant. Hence, it will be assumed that all testing modeled herein is performed at least 4 feet (1.2 m) from the edge of the pavement (or any signifi­cant joint or crack).

To backcalculate layer moduli from the static and dynamic motions predicted with UTFWD, a microcomputer-based program developed for the Texas Department of Transportation was used. This program, named MODULUS (Uzan et al, 1989), is capable of backcalculating pavement layer moduli from the deflection basins obtained with the FWD test. As with UTFWD, it uses a lin­ear elastic approach. However, one of the key as­pects of MODULUS is that it involves a static in­terpretation method to backcalculate layer moduli. The dynamic characteristic of the FWD is thus ignored.

Page 15: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

ACP

Base

Subgrade

<,,,~~~''""'"~"· Bedrock

(a) Profile 1 (FM 137 near Paris, TX)

ACP

Base

Subgrade

Bedrock

(b) Profile 2 (FM 195 near Paris, TX)

ACP

Base

Subgrade

Bedrock

(c) Profile 3 (Route 1 near Austin, TX)

CRC

ACP

Subbase

Subgrade

Bedrock

(d) Profile 4 (IH 10 near EI Paso, TX)

Figure 2.3 Idealized cross-sections of the four pavement profiles

5

i I·

!

I I

Page 16: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

~ -------"--·~--

;~:ii . ll

1',;1'· Table 2.1 Material properties of the four pavement profiles i'' '~I

·'i,l· II': Unit ''·I' "I Thickness Poisson's Weight Damping ·.;1'

Profile No. Modelled After Material Type (in.) Ratio (pcf) Ratio -1 FM137 ACP 1 0.27 140 0.02

(near Paris, Base 12 0.25 125 0.02 Tx) Subgrade * 0.33 125 0.02

2 FM195 ACP 4 0.27 140 0.02 (near Paris, Base 6 0.25 125 0.02

Tx) Subgrade * 0.33 110 0.02

3 Route 1 ACP 7 0.27 145 0.02 (near Austin, Base 6 0.25 130 0.02

Tx) Subgrade * 0.33 130 0.02

4 IH10 CRC 10 0.2 145 0.02 (near El Paso, AC Base 6 0.27 145 0.02

Tx) Subbase 12 0.25 125 0.02 Subgrade * 0.33 125 0.02

* Subgrade thickness was varied from 5 to 120ft for the Dynaflect test and was varied from 5.5 to 90 ft for the FWD test.

Page 17: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

CHAPTER 3. PARAMETRIC STUDY OF THE DYNAFLECT TEST

3.1 INTRODUCTION

Analytical simulations of the Dynaflect test were conducted using computer program UTDYNF (Chang, 1991; Chang et al, 1992). The four pave­ment profiles shown in Figure 2.2 were studied. The main purposes of these studies were:

1. to determine the resonant depth to bedrock with various stiffness combinations of pave­ment layers,

2. to develop an equation for estimating the resonant depth to bedrock, the depth where use of a static interpretation method involves the largest errors, and

3. to study the variations of the deflection ra­tios (pavement surface motions under dy­namic loading divided by surface motions under an equivalent static load) as a func­tion of various stiffness combinations of pavement layers.

3.2 MODEL PARAMETERS

The material properties of the four pavement profiles are given in Table 2.1. The stiffness of each pavement layer is represented by its shear wave velocity (V s) and Young's modulus (E). The rela­tionship between V5 and E can be expressed by:

(3.1)

where v = Poisson's ratio, and p mass density of the material (to­

tal unit weight divided by gravi­tational acceleration).

Young's modulus of the subgrade layer was varied from 16 to 142 ksi (0.11 to 0.98 MN/m2)

(V5 = 500 to 1500 fps (125.5 to 457.5 m/s)) to simulate variations in subgrade material, density, and moisture content. Young's modulus of the granular base or granular subbase was varied from 70 to 300 ksi (0.48 to 2.07 MN/m2) (Vs = 1000 to 2000 fps ( 305 to 610 m/s)) to consider the effects of moisture and density changes.

7

Young's modulus of the asphalt concrete layer was varied from 312 to 1920 ksi (2.15 to 13.2 MN/m2) (V5 = 2000 to 5000 fps (610 to 1525 m/ s)) to consider the effects of temperature and density changes on the asphalt. The stiffness of the CRC was the only pavement layer not varied. Young's modulus of the CRC was set to a con­stant value of 5425 ksi (37.4 MN/m2) (V5 = 8500 fps (2592.5 m/s)).

The ranges of stiffnesses used for the pavement layers are listed in Table 3.1. The depth to bed­rock at each profile was varied from 5 to 120 feet (1.5 to 36.6 m) in increments of 2.5 feet (0.76 m). This depth is the distance from the top of the pavement surface to the top of bedrock.

Table 3.1

Material Type

CRC

Ranges in stiffnesses used for the pavement layers in the four pavement profiles

Shear Approx. Wave Assumed Young's

Velocity Poisson's Modulus* (fps) Ratio (ksi)

8,500 0.20 5,425

Asphalt Concrete 2,000 0.27 312

Granular Base or Subbase

Sub grade

3,000 4,000 5,000

1,000 1,500 2,000

500 750

1,000 1,500

0.27 0.27 0.27

0.25 0.25 0.25

0.33 0.33 0.33 0.33

3.3 DEFLECTION BASINS

690 1,225 1,920

67 152 270

16 36 63

142

Deflection basins were obtained with com­puter program UTDYNF for both static and dy­namic loadings. For static loading, a very small

Page 18: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

~- ----------------------------

II I.

frequency (0.75 Hz) was used. For dynamic load­ing, a frequency of 8 Hz was used. A typical plot of the dynamic deflections at the Dynaflect mea­surement stations as a function of depth to bed­rock is shown in Figure 3.1a. A similar plot of static deflections as a function of depth to bed­rock is shown in Figure 3.1b. The ratios of dy­namic deflections to static deflections are called the deflection ratios and are shown in Figure 3.1c. The depth to bedrock corresponding to the maximum deflection ratio is called the resonant depth to bedrock.

First consider the variation in static deflec­tions with depth to bedrock as shown for Pro­file 1 in Figure 3.1b. Initially, static deflections at all measurement stations increase as subgrade thickness increases, simply because a thicker section of subgrade material is being strained. This effect is very pronounced for depths to bedrock ranging from 5 to about 15 feet (l.S to 4.6 m). As the thickness of the subgrade in­creases above 15 feet (4.6 m), the effect de­creases significantly because of the stress distri­bution associated with a small loaded area. Any backcalculation method based on a static inter­pretation of the Dynaflect assumes exactly this response (Figure 3.1b).

On the other hand, the dynamic loading from the Dynaflect results in the surface mea­surement stations changing with depth to bed­rock as shown in Figure 3.la. For shallow depths to bedrock, say 5 to 15 feet (l.S to 4.6 m) in Profile 1, surface dynamic motions in­crease more rapidly than the static motions as the subgrade thickness increases. More impor­tantly, this increase is followed by a predomi­nate peak which, in turn, is followed by a de­crease in dynamic motions. This significant peak in the dynamic motions occurs in the bed­rock depth range of IS to 35 feet (4.6 to 10.7 m). This is the dynamic amplification effect. At depths greater than about 40 feet (12.2 m), the dynamic deflections are quite similar to the static deflections. This dynamic behavior is eas­ily seen in the deflection ratio as a function of depth to bedrock in Figure 3.lc.

The significant amplifications in the dynamic motions compared with the static motions are easily seen in bedrock depth ranges of about 10 to 30 feet (3.1 to 9.2 m) for Profile 1 with a soft subgrade layer (E = 16 ksi (0.11 MN/m2)). More­over, the maximum deflection ratio always oc­curs at the farthest measurement station (sta­tion 5), which indicates that the further away from the source the measurement station is in the Dynaflect test, the larger the relative dy­namic effect is.

8

-Station 1 - Station2 --Station 3

1.6 -- Station4

1.4

~ --Station 5

0 :;:::; 1.2 l'l c::: 1.0 c 0.8 0 ·.;::; 0.6 u

Q) 0.4 ~ Cl 0.2

0.0 0 20 40 60 80 100 120

Depth to Bedrock (ft)

(a) Dynamic deflections

-Station 1 - Station2 --Station 3

1.6 -- Station4 Station 5

0 1.4 ·.;::;

1.2 l'l

{; c::: 1.0 c 0.8 0

'.;::; 0.6 u

~ Q) 0.4 ~ Cl 0.2

0.0 0 20 40 60 80 100 120

Depth to Bedrock (ft)

(b) Static deflections

2.2 0

2.0 '.;::;

-Station 1 - Station2

l'l c::: 1.8 c

1.6 0 '.;::;

- Station3 -- Station4 -- Station 5

u 1.4 Q)

(jj 1.2 Cl

1.0 0 20 40 60 80 100 120

Depth to Bedrock (ft)

(c) Deflection ratios

Figure 3.1 Delfection basins and deflection ratios as a function of depth to bedrock obtained for Dynaflect testing at Profile 1 (E of AC = 312 ksi, E of base= 67 ksi, and E of subgrade • 16 ksi)

Dynamic and static deflection basins as a function of distance from the source obtained at the peak deflection ratio (termed the resonant depth to bedrock) are shown in Figures 3.2 and 3.3 for Profile 1 (flexible pavement) and Profile 4 (rigid pavement), respectively. As can be seen, the dynamic deflections at all measurement sta­tions are approximately 0.35 mils (0.0089 mm) larger than the static deflections for the soft

Page 19: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

subgrade condition in Profile 1, as shown in Figure 3.2a. This difference represents more than a 100 percent difference (error) in the static measurement at station 5 and about a 30 percent difference at station 1. These differences are clearly shown by the deflection ratios in Figure 3.1c.

0.0

~ 0.2 D ·e 0.4 Cl

....... 0.6 Cl • § 0.8 • ".;:::; D • u 1.0 QJ

Cl ~ 1.2 • • Dynamic Deflection Basins 0 1.4 D Static Deflection Basins • 1.6 El-__ _._ __ __,...._ __ .._ __ _._ __ __,

0 1 2 3 4 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 500 fps (E = 16 ksi)

0.0 0 0

0 ~ 0.2 0 ·e 0.4 -0.6 § 0.8

".;:::; 1.0 u

QJ

5

w 1.2 • Dynamic Deflection Basins 0 1.4 Cl Static Deflection Basins

1.6 0 1 2 3 4 5

Distance from the Source (ft)

(b) S-wave velocity of subyrade = 1,500 fps (E = 142 ksi)

Figure 3.2 Dynamic and static deflection basins obtained at the resonant depth to bedrock for Dynaflect testing at profile 1 (V5 of AC = 3,000 fps (E = 690 ksi), V5 of base= 1,000 fps (E = 647 ksi))

When the stiffest subgrade condition is used at Profile 1, the dynamic deflections are only about 0.018 mils (0.000046 mm) larger than the static deflections, as shown in Figure 3.2b. In this case, the difference between dynamic and static deflec­tions ranges from about 17 percent at station 5 to about 7 percent at station 1. These differences are shown by the deflection ratios in Figure A.1d.

For Profile 4, there is less variation in the deflec­tion basins with distance from the source than in Profile 1. This response can be seen by comparing Figures 3.2a and 3.3a. This occurs because Profile 4 represents a rigid pavement while Profile 1 rep­resents a very flexible pavement. However, there is still a significant difference between the static and dynamic deflection basins for Profile 4 with the

softest subgrade condition. This difference is about 0.4 mils (0.0102 mm) at the resonant bedrock depth (Figure 3.3a) and represents about a 175 percent difference at station 5 and 120 percent difference at station 1. There is little difference (less than 16 percent) between the dynamic and static deflections for the stiffest subgrade condition at Profile 4, as shown in Figure 3.3b.

0.0

~ 0.2 Cl D D Cl D ·e o.4

-0.6 • • • • c • 0 0.8 ".;:::;

1.0 u QJ

w 1.2 • Dynamic Deflection Basins 0 1.4 Cl Static Deflection Basins

1.6 b..... __ _._ __ __._ __ __, ___ .__ _ ___,

0 1 2 3 4 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 500 fps (E = 16 ksi)

0.0 ~ 0.2

0 0

·e 0.4 ....... 0.6 § 0.8

·.;:::; ~ 1.0

5

w 0

1.2 1.4

• Dynamic Deflection Basins CJ Static Deflection Basins

1.6 0 1 2 3 4

Distance from the Source (ft) 5

(b) S-wave velocity of subgrade = 1,500 fps (E = 142 ksi)

Figure 3.3 Dynamic and static deflection basins obtained at the resonant depth to bedrock for Dynaflect testing at Profile 4 (V5 of CRC = 8,500 fps (E = 5425 ksi), V5 of AC = 3,000 fps (E = 690 ksi) and V5 of subbase= 1,000 fps (E = 67 ksi))

The complete results of all simulations of the Dynaflect test with various stiffness combina­tions for the four pavement profiles are pre­sented in Appendix A, Figures A.1 through A.48. These results are discussed in more detail in the next two sections.

3.4 RESONANT DEPTH TO BEDROCK

As shown in Section 3.3, use of a static inter­pretation method with the deflection basins ob­tained from Dynaflect tests with bedrock depths near the resonant depth can lead to significant errors in the deflections and, hence, to significant

Page 20: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

errors in the backcalculations of layer moduli. (The magnitude of the errors in the backcalcula­tions is studied in Chapter 5 with regard to the FWD test and are not studied with regard to the Dynaflect test.) Therefore, it is important to know the resonant depth to bedrock and how it varies with various stiffness combinations of the pave­ment layers.

The resonant bedrock depths as a function of the various stiffness combinations for Profile 1 are shown in Figure 3.4. It is interesting to find that the resonant depths to bedrock are predomi­nately determined by the stiffness of the sub­grade layer. The variations of the stiffnesses of the AC and granular base layers have little effect

"'"' ~100 ,.;,: e 80

~ 60 co .s 40

.r:. 0.. ~ 0

"'"' ~100 ,.;,:

80 u e "0 60 Q) co .s 40

.r:. 20 ..... c.. Q) 0 Cl

Base Material: V5

(E)

• 1,000 (67) 0 1,500(152) 121 2,000 (270)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(a) V5 of subgrade = 500 (E = 16 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(b) V5 of subgrade = 750 (E = 36 ksi)

on the resonant depths to bedrock. For instance, in Figure 3.4c, for a subgrade with shear wave velocity of 1000 fps (305 m/s) (corresponding to E = 63 ksi (0.43 MN/m2)), the resonant depths ranged from 55 to 57.5 feet (16.8 to 17.5 m), while the stiffnesses of the base varied by four and the stiffnesses of the asphalt varied by about six. On the other hand, when the stiffness of the subgrade was increased by 2.25 times (going from E = 63 ksi to E = 142 ksi (0.43 to 0.98 MN/ m2)), the average resonant depth increased from 56 feet (17.1 m) (Figure 3.4c) to 85 feet (26.0 m) (Figure 3.4d). This comparison clearly illustrates the importance of the stiffness of the subgrade in Profile 1.

-~ 100 ,.;,:

80 u e "0 60 Q) co .s 40

.r:. 20 ..... Q.. Q) 0 Cl

-~100 ,.;,: e 80

~ 60 co .s 40

£ 20 Q.. Q) 0 Cl

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(c) V5 of subgrade = 1,000 (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1 ,225) 5,000 (1,920)

V5

of AC (E of AC)

(d) V5 of subgrade = 1,500 (E = 142 ksi)

Figure 3.4 Resonant depths to bedrock for Dynaflect testing at Profile 1 with various stiffness combinations of the pavement layer (units: Vs = fps, E = ksi)

Page 21: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

A similar importance of the subgrade stiffness in the resonant depths to bedrock was found for the other three pavement profiles, as shown in Figures 3.5, 3.6, and 3.7. A list of the ranges in depths and average depths for all profiles is given in Table 3.2. As one can see in the table, Profile 4, which is a

g 100 ~

80 u e ~ 60 co 0 40 ....

.r:. .... c.. <11 0

-::5. 100 ~

80 u e "C 60 <11 co 0 40 ....

.r:. 20 .... c.. <11 0 0

Base Material: V5 (E)

.1,000 (67) D 1,500 (152) lJ 2,000 (270)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(a) Vs of subgrade = 500 (E = 16 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(b) Vs of subgrade = 750 (E = 36 ksi)

rigid pavement, exhibits slightly shallower reso­nant depths to bedrock compared with the other pavement profiles. The resonant depths are about 3 percent to 9 percent less than the other profiles and result from Profile 4 being composed of the stiffest and thickest surface layers.

-::5. 100

-n 80 e ~ co 0 ....

.r:. ...., c.. <11 0

-::5.100

iJ 80 e "C

<11 co .8 £ 20 c.. <11 0 0

2,000 (312) 3,000 (690) 4,000 (1 ,225) 5,000 (1 ,920)

V5 of AC (E of AC)

(c) V5 of subgrade = 1,000 (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(d) V5 of subgrade = 1,500 (E = 142 ksi)

Figure 3.5 Resonant depths to bedrock for Dynoflect testing at Profile 2 with various stiffness combinations of the pavement Ioyer (units: Vs = fps, E = ksi)

11

Page 22: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

:I' I IF !l'i

i f:

-i!:-100

'"" 80 v e "0 60 (l) co 0 40 ..... .I::. 20 ..... 0.. (l) 0 Cl

-t.lOO

'"" 80 v e "0 60

C1l co .s 40

.r; 20 ..... 0.. C1l 0 Cl

Base Material: V5

(E) • 1,000 (67) D 1,500 (152) !I 2,000 (270)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5 of AC (E of AQ

(a) V5 of subgrade = 500 (E = 16 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(b) V5 of subgrade = 750 (E = 36 ksi)

,...., t.. 100

u 80 e ~ 60

.s 40

.r; 20 0.. C1l 0 Cl

-t,.100

'"" 80 v e "0 60 C1l co .s 40

.r; 20 ..... 0.. C1l 0 Cl

2,000 (312) 3,000 (690) 4,000 (1 ,225) 5,000 (1,920)

V5 of AC (E of AC)

(c) V5 of subgrade = 1, 000 (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5 of AC (E of AC)

(d) V5 of subgrade = 1,5 00 (E = 142 ksi)

Figure 3.6 Resonant depths to bedrock for Dynaflect testing at Profile 3 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

To develop an equation for predicting the reso­nant depth to bedrock, the average resonant depth to bedrock (RDb) for each profile for each subgrade stiffness was plotted versus the subgrade shear wave velocity, as shown in Figure 3.8. This was done because the stiffnesses of the other lay­ers had little effect on the results. As can be seen, the results appear to form two groups, one is for Profiles 1, 2, and 3 (all are flexible pavements) and the other is Profile 4 (the rigid pavement). Two straight lines were fitted through the two data groups, which resulted in:

RDb = 0. 056V s (3.2)

for the flexible pavements with the resonant depth to bedrock, RDb, in feet and V5 in feet per second (fps). For the rigid pavement, the equation becomes:

12

RDb = 0.052V5 (3.3)

with RDb in feet and V5 in fps. Equation 3.1 and 3.2 can be expressed in term of Young's modu­lus as:

RDb = 0.019-F£ (3.4)

for the flexible pavement with the unit weight of the subgrade material assumed to be 110 pounds per cubic foot (pcf), Poisson's ratio assumed to be 0.33, RDb in feet and E in pounds per square foot (psf), and

RDb = 0.017-F£ (3.5)

for the rigid pavements with RDb in feet and E in psf.

Page 23: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

-t.. 100 ..::.!.

80 u e \J 60 Q) a:l

.s 40

.r::. 20 ..... c.. Q) 0 Cl

-t.. 100 ..::.!. u 80 e \J 60 ~ .s .r::. 20 '5.. Q) 0 Cl

2,000 (312)

Base Material: V5

(E) • 1,000 (67) 0 1,500 (152) i!l 2,000 (270)

3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5 of AC (E of AC)

(a) V5 of subgrade = 500 (E = 16 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225)5,000 (1,920)

V5 of AC (E of AC) .

(b) V5 of subgrade = 750 (E = 36 ksi)

g 100 ..::.!. u 80 e ~ 60 a:l

0 ..... :5 20 c.. ~ 0

-t.. 100 ..::.!. u 80 e ~ 60 a:l

.s 40

:5 20 c.. Q)

Cl 0

2,000 (312) 3,000 (690) 4,000 (1,225)5,000 (1,920)

V5 of AC (E of AC)

(c) V5 of subgrade = 1,000 (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225)5,000 (1,920)

V5 of AC (E of AC)

(d) V5 of subgrade = 1,5 00 (E = 142 ksi)

Figure 3.7 Resonant depths to bedrock for Dynaflect testing at profile 4 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

Table 3.2 Variations in the average resonant depths to bedrock obtained with dynaflect testing at the four pavement profiles

Shear Wave Approximate Range Resonant Depth to Bedrock* (ft) Velocity of Young's in

Subgrade Modulus Depths Profile 1 Profile 2 Profile 3 Profile 4 (fps) (ksi) (ft) FM137 FM195 Route 1 IHlO

500 16 Maximum 27.50 27.50 27.50 25.00 Minimum 27.50 27.50 25.00 25.00 Average 27.50 27.50 25.83 25.00

750 36 Maximum 42.50 42.50 42.50 37.50 Minimum 40.00 40.00 40.00 37.50 Average 40.79 41.25 40.83 37.50

1,000 63 Maximum 57.50 57.50 55.00 52.50 Minimum 55.00 55.00 55.00 52.50 Average 56.04 56.04 55.00 52.50

1,500 142 Maximum 85.00 85.00 85.00 80.00 Minimum 85.00 85.00 85.00 80.00 Average 85.00 85.00 85.00 80.00

* The depth represents the thickness from the pavement surface to the top of the bedrock.

13

l!

I

I :'

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------------------

Young's Modulus of Subgrade (ksi)

£90 16 36 63 1 00 142

.._, -o 80

e 70 "C

~ 60

.s 50 ..t::. Q.40 Q)

Cl 30 ..... ~ 20 o Profiles 1, 2 and 3 (Flexible Pavement) § 1 0 c Profile 4 (Rigid Pavement)

"' ~ 0~------~----~------~------~ 500 7 50 1 ,000 1 ,250 1 ,500

Shear Wave Velocity of Subgrade (fps)

Figure 3.8 Average resonant depth to bedrock versus the stiffness of the subgrade obtained with Dynaflect testing at the four pavement profiles

Davies and Mamlouk (1985) conducted an ana­lytical investigation for the Road Rater test, which is also a steady-state surface loading test, on a rigid pavement profile. They developed the fol­lowing equation for predicting the resonant thick­ness of subgrade (H):

v H=OA*...:....i.

f

with H in feet, V5 in fps, and fin Hz.

(3.6)

In order to compare with the equation sug­gested by Davies and Mamlouk (1985), the reso­nant depth to bedrock (RDb) was expressed in terms of the resonant thickness of the subgrade (H) as a function of the shear wave velocity of subgrade, as shown in Figure 3.9. Again, the re­sults form clearly two groups: one for the flexible pavements (Profiles 1, 2, and 3) and the other for the rigid pavement (Profile 4) (Fig. 3.9a). Two­straight lines were fitted through the two data groups, which resulted in:

H = O.OSSV5 (3.7)

for the flexible pavement with H in feet, and V5

in fps, and

(3.8)

for the rigid pavement, with H in feet and V 5 in fps. Following the approach used by Davies and

14

Mamlouk (1985), Equation 3.8 can be expressed in terms of frequency (f) as:

v H=OA*f (3.9)

which is identical to the equation proposed by Davies and Mamlouk (1985) .

Young's Modulus of Subgrade (ksi) 0' ~ 16 36 63 100 142 ~ 90~------~-----,,------,~----~

e so 0')

-§ 70

~ 60

~ 50 "' ~ 40 iS 30

~ 20 ..... ~ 10

• Profile 1 • Profile 2 o Profile 3 c Profile 4

§ o~ ______ ._ ____ ~~----~------~ ::3 500 750 1,000 1,250 1,500

c:: Shear Wave Velocity of Subgrade (fps)

Figure 3.9 Average resonant thickness of subgrade versus the subgrade stiffness obtained with Dynaflect testing at the four pavement profiles

3.5 AMPLITUDE OF THE MAXIMUM DEFLECTION RATIO

As discussed earlier, the amplitude of the de­flection ratio (dynamic deflection divided by static deflection) at each Dynaflect measurement station is an important index of the potential error generated in any static interpretation proce­dure (as discussed in Chapter 5 for the FWD test). Figure 3.10 shows the maximum deflection ratios as a function of various stiffnesses combinations of Profile L It should be noted that the maximum ratios are for measurements at station 5. Varia­tions of the stiffnesses of the AC and base layers have little effect on the values of the maximum deflection ratio, as shown in Table 3.3. For ex­ample, if V5 of the AC varies from 2000 to 5000 fps (610 to 1525 m/s) (E = 312 to 1920 ksi (2.15 to 13.2 MN/m2)), the deflection ratio only varies from 2.24 to 2.04 (approximately a 10 percent de­crease) when V5 of the base is 1000 fps (305 m/s) (E = 70 ksi (0.48 MN/m2)) and V5 of the subgrade is 500 fps (152.5 m/s) (E = 16 ksi (0.11 MN/m2)),

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as shown in Figure 3.10a. Moreover, if V5 of the base varies from 1000 to 2000 fps (305 to 610 m/ s) (E = 67 to 270 ksi (0.46 to 1.86 MN/m2)), the deflection ratio varies from 2.24 to 1.98 (approxi­mately a 13 percent decrease) when V5 of the AC is 2000 fps (610 m/s) (E = 270 ksi (1.86 MN/m2))

and V5 of the subgrade is 500 fps (152.5 m/s) (E = 16 ksi (0.11 MN/m2)), as shown in Figure 3.10a.

Variations in the stiffness of the subgrade layer have the most significant effect on the amplitudes of the maximum deflection ratios. If V s of the subgrade varies from 500 to 750 fps (152.5 to 228.8 m/s) (E = 16 to 36 ksi (0.11 to 0.25 MN/ m2)), there is an approximately 17 percent de­crease in the deflection ratios. If V s of the sub­grade varies from 500 to 1500 fps (125.5 to 457.5 m/s) (E =16 to 142 ksi (0.11 to 0.98 MN/m2)),

there is a SO percent reduction in the deflection ratios. Again, it is important to keep in mind that the deflection ratio at station 5 is being discussed above and changes in the deflection ratio are con­siderably less for station 1 (and other stations), as shown in Appendix A. However, station 5 is criti­cal in backcalculating layer moduli and, hence, was chosen for discussion.

4

4

Base Material: V5

(E) • 1,000 (67) 0 1,500 (152) li!'l 2,000 (270)

3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5 of AC (E of AC)

(a) V5 of subgrade = 5 00 fps (E = 18 ksi)

2,000 (312) 3,000 ( 690) 4,000 (1 ,225) 5,000 (1 ,920)

V5

of AC (E of AC)

(b) V5 of subgrade = 750 fps (E = 36 ksi)

Profile 2 and Profile 3 exhibit trends similar to those of Profile 1 (Figures 3.11 and 3.12). For Profile 4, the amplitudes of the deflection ratios obtained at the softest subgrade condition are about SO percent higher than those obtained at Profiles 1, 2, and 3. This relationship is only true for the softest subgrade at Profile 4, as shown in Table 3.3. For the three other sub­grade stiffnesses, the deflection ratios are about equal to or slightly less than those at Profiles 1, 2, and 3 (see Table 3.3 and Figure 3.3). It is in­teresting to see that the deflection ratios of Pro­file 4 are larger than the other three pavements for the softest subgrade because Profile 4 has the thickest and the stiffest upper layers (Figure 3.13). However, as can be seen in Figures 3.2a and 3.3a in Section 3.3, the differences in dy­namic and static deflections obtained at Profile 4 are larger than the differences of dynamic and static deflections obtained at Profile 1. This ex­plains why the deflection ratios (dynamic de­flections divided by static deflections) obtained at Profile 4 with the softest subgrade condition are larger than the deflection ratios obtained at a flexible pavement (Profile 1).

4

4 0

·.;:::;

"' c::3 c: 0

"Z.'l

~ 2 li 0

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(c) V5 of subgrade = 1,000 fps (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5 of AC (E of AC)

(d) V5 of subgrade = 1,500 fps (E = 142 ksi)

Figure 3.10 Maximum deflection ratios for Dynaf/ect testing at Profile 7 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

15

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j,

I' 4

0

i 0::3 c:: 0 ~

~2 1ii 0

Base Material: V s (E) • 1,000 (67) D 1,500 (152) 1Z1 2,000 (270)

(a) V5 of subgrade = 500 fps (E = 18 ksi)

2,000 (312)

(b) V5 of subgrade = 750 fps (E = 36 ksi)

4 0 ~

("<:!

0::3 c:: 0 ~

~2 1ii 0

4

(c) V5 of subgrade = 1,000 fps (E = 63 ksi)

2,000 (312)

(d) V5 of subgrade = 1,5 00 fps (E = 142 ksi)

Figure 3.11 Maximum deflection ratios for Dynaflect testing at Profile 2 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

0 ·,p

4

("<:!

0::3 c:: 0 ~ u aJ2 ~ 0

4

Base Material: Vs (E) • 1,000 (67) D 1,500 (152) r::l 2,000 (270)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(a) V5 of subgrade = 500 fps (E = 18 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(b) V5 of subgrade = 750 fps (E = 36 ksi)

0 ~

("<:!

4

0::3 c:: 0 •,p

~2 ~ 0

4

2,000 (312)

(c) V5 of subgrade = 7,000 fps (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

V5

of AC (E of AC)

(d) V5 of subgrade = 1,500 fps (E = 142 ksi)

Figure 3.12 Maximum deflection ratios for Dynaflect testing at Profile 3 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

16

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Table 3.3 Variations in the deflection ratios obtained at station 5 for Dynaflect testing at the resonant depth to bedrock at the four pavement profiles

Shear Wave Approximate Velodty of Young's Range Subgrade Modulus in

(fps) (ksi) Ratio

500 16 Maximum Minimum Average

750 36 Maximum Minimum Average

1,000 63 Maximum Minimum Average

1,500 142 Maximum Minimum

Average

3.6 SUMMARY

The Dynaflect test was studied analytically using computer program UTDYNF (Chang, 1991; Chang et al, 1992). Four typical in-ser­vice pavement profiles (three flexible pave­ments and one rigid pavement) were studied (Figure 2.2). The stiffness of. each pavement layer was varied to simulate expected variations in the pavement materials.

The dynamic effect of the Dynaflect test was expressed in terms of the deflection ratios (dy­namic deflections divided by static deflections). The resonant depth to bedrock (the depth to bedrock corresponding to the maximum deflec­tion ratio) is determined predominately by the stiffness of the subgrade layer. Variations in the stiffnesses of the other pavement layers have little effect on the resonant bedrock depth. The maximum variations in resonant bedrock depths

Maximum Deflection Ratio

Profile 1 Profile 2 Profile 3 Profile 4

17

FM137 FM195 Route 1 IHlO

2.24 2.20 2.10 2.92 1.92 1.92 1.86 2.72 2.03 2.03 1.93 2.83

1.92 1.88 1.82 1.82 1.68 1.69 1.68 1.72 1.77 1.75 1.71 1.78

1.70 1.68 1.66 1.60 1.57 1.55 1.52 1.50 1.63 1.60 1.57 1.56

1.47 1.45 1.46 1.34 1.43 1.41 1.39 1.28 1.46 1.44 1.43 1.31

were 25 feet (7 .8 m) to 85 feet (26.4 m) for the Dynaflect test at 8 Hz.

Two equations (one for flexible pavements and one for rigid pavements) were developed for esti­mating the resonant depth to bedrock. The equa­tion for rigid pavements is in good agreement with the equation proposed by Davies and Mamlouk (1985). They did similar studies for the Road Rater test (also a steady-state test) on a rigid pavement.

The amplitude of the deflection ratio is an important index of the potential error generated in any static interpretation procedure of the Dynaflect test. The stiffness of the subgrade layer has the most significant effect on the amplitudes of the maximum deflection ratios. The softer the subgrade, the higher the amplitude of the maxi­mum of deflection ratio. This indicates that the error generated in a static interpretation proce­dure of the Dynaflect test will decrease as the subgrade stiffness increases.

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4

4

Base Material: Vs (E) • 1,000 (67) 0 1,500 (152) !] 2,000 (270)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(a) V5 of subgrade = 500 fps (E = 18 ksi)

2,000 (312) 3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(b) V5 of subgrade = 750 fps (E:::::: 36 ksi)

0 ·.;::~ ('(!

4

0:::3 c: 0 ;:;

d!2 ~ 0

3,000 (690) 4,000 (1,225) 5,000 (1,920)

Vs of AC (E of AC)

(c) V5 of subgrade = 1,000 fps (E = 63 ksi)

2,000 (312) 3,000 (690) 4,000 (1 ,225) 5,000 (1 ,920)

V5 of AC (E of AC)

(d) V5 of subgrade = 1,5 00 fps (E = 142 ksi)

Figure 3.13 Maximum deflection ratios for Dynaflect testing at Profile 4 with various stiffness combinations of the pavement layer (units: V5 = fps, E = ksi)

18

I

I I

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CHAPTER 4. PARAMETRIC STUDY OF THE FALLING WEIGHT DEFLECTOMETER TEST

4.1 INTRODUCTION

Analytical simulations of the FWD test were conducted using the UTFWD program (Chang, 1991; Chang et al, 1992). The four pavement pro­files shown in Figure 2.3 were studied. These pro­files are the same ones used in the Dynaflect study presented in Chapter 3. The main purposes of these studies were:

1. to determine the resonant depth to bedrock with various stiffnesses of the subgrade, in­cluding unsaturated and saturated conditions;

2. to develop equations for estimating the reso­nant depth to bedrock;

3. to develop a method for estimating the depth to bedrock based on the free vibrations of the pavement system created by the FWD test; and

4. to develop an approach for estimating the stiffness of the subgrade layer based on the phase shift between the first pulses at two measurement stations in the deflection-time records of the FWD test.

The loading in the FWD test is described in Section 2.2 of this report. The deflection basins presented herein are normalized with respect to the load. Therefore, actual deflections under any load are simply calculated by multiplying the normalized deflection by the desired load.

4.2 MODEL PARAMETERS

Based on the earlier studies with the Dynaflect test, variations in the stiffnesses of the surface and

19

base layers had little effect on the deflection basins. Therefore, only the subgrade stiffness was varied in this study of the FWD test. The stiffnesses of the other pavement layers were kept constant, such that the shear wave velocity of the CRC equaled 8500 fps (2593 m/s) (E = 5425 ksi (37.4 MNJmZ)), the shear wave velocity of the AC equaled 3000 fps (915 m/s) (E = 690 ksi (4.8 MN/mZ)), and the shear wave velocity of the base equaled 1000 fps (305 m/s) (E = 67 ksi (0.46 MN/m2)). The shear wave velocity of the subgrade layer was varied from 500 to 1500 fps (150 to 450 m/s) and the corresponding Young's modulus was varied from 16 to 142 ksi (0.11 to 0.98 MN/m2). In addition, the depths to bedrock of the four pavement profiles were varied from 5.5 to 90 feet (1.65 to 27 m).

To simulate an unsaturated subgrade, a Poisson's ratio of 0.33 was used. The material properties of the four pavement profiles with unsaturated subgrade conditions are given in Table 4.1. To simulate a saturated subgrade, the P­wave velocity of the subgrade was set equal to 5000 fps (1525 m/s). This velocity represents typi­cal field conditions for uncemented saturated soils (Richart et al, 1970). The shear wave velocities of the saturated subgrades were varied from 500 to 1500 fps (150 to 450 m/s), as in the unsaturated subgrade condition. As a result, Poisson's ratio varied from 0.495 to 0.451, as S-wave velocity of the subgrade varied from 500 to 1500 fps (150 to 450 M/s). Hence, Young's modulus for the satu­rated subgrade varied from 18 to 155 ksi (0.12 to 1.07 MN/m2). The material properties of the four pavement profiles with saturated subgrades are given in Table 4.2.

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Table 4.1 Material properties of the four pavement profiles with unsaturated subgrade conditions

a) FM137 (Profile 1)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

ACP 1 0.27 140 0.02 3,000 5,345 690.4 Base 12 0.25 125 0.02 1,000 1,732 67.4

Subgrade* h** 0.33 110 0.02 500 993 15.8 0.33 110 0.02 750 1,488 35.5 0.33 110 0.02 1,000 1,985 63.1 0.33 110 0.02 1,500 2,978 142.0

b) FM195 (Profile 2)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

ACP 4 0.27 140 0.02 3,000 5,345 690.4 Base 6 0.25 125 0.02 1,000 1,732 67.4

Sub grade h 0.33 110 0.02 500 993 15.8 0.33 110 0.02 750 1,488 35.5 0.33 110 0.02 1,000 1,985 63.1 0.33 110 0.02 1,500 2,978 142.0

c) Route 1 (Profile 3)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

ACP 7 0.27 145 0.02 3,000 5,345 715.1 Base 6 0.25 130 0.02 1,000 1,732 70.1

Subgrade h 0.33 130 0.02 500 993 18.7 0.33 130 0.02 750 1,489 42.0 0.33 130 0.02 1,000 1,985 74.6 0.33 130 0.02 1,500 2,979 167.9

d) IH 10 (Profile 4)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

CRC 10 0.2 145 0.02 8,500 13,880 5424.2 ACP 6 0.27 145 0.02 3,000 5,345 715.1 Base 12 0.25 125 0.02 1,000 1,732 67.4

Subgrade h 0.33 110 0.02 500 993 15.8 0.33 110 0.02 750 1,488 35.5 0.33 110 0.02 1,000 1,985 63.1 0.33 110 0.02 1,500 2,978 142.0

*There are four different S-wave velocities for each subgrade. **Thickness of subgrade (h) was varied from 5.5 to 90ft.

20

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.... -_,,...,..,._,.,._""""'--""'-""'~.......-~------------------------------- ~·----··---

Table 4.2 Material properties of the four pavement profiles with saturated subgrade conditions

a) FM 137 (Profile 1)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

ACP 1 0.270 140 0.02 3,000 5,345 690.4 Base 12 0.250 125 0.02 1,000 1,732 67.4

Subgrade* h** 0.495 110 0.05 500 5,000 17.4 0.489 110 0.05 750 5,000 39.5 0.479 110 0.05 1,000 5,000 69.8 0.451 110 0.05 1,500 5,000 154.8

b) FM 195 (Profile 2)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio (fps) (fps) (ksi)

ACP 4 0.270 140 0.02 3,000 5,345 690.4 Base 6 0.250 125 0.02 1,000 1,732 67.4

Subgrade h 0.495 110 0.05 500 5,000 17.7 0.489 110 0.05 750 5,000 39.5 0.479 110 0.05 1,000 5,000 69.8 0.451 110 0.05 1,500 5,000 154.8

c) Route 1 (Profile 3)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio {fps) {fps) (ksi)

ACP 7 0.270 145 0.02 3,000 5,345 715.1 Base 6 0.250 130 0.02 1,000 1,732 70.1

Subgrade h 0.495 130 0.05 500 5,000 21.0 0.489 130 0.05 750 5,000 46.7 0.479 130 0.05 1,000 5,000 82.5 0.451 130 0.05 1,500 5,000 183.0

d) IH 10 (Profile 4)

Unit S-wave P-wave Young's Material Thickness Poisson's Weight Damping Velocity Velocity Modulus

Type (in.) Ratio (pcf) Ratio {fps) {fps) (ksi)

CRC 10 0.200 145 0.02 8,500 13,880 5424.2 ACP 6 0.270 145 0.02 3,000 5,345 715.1 Base 12 0.250 125 0.02 1,000 1,732 67.4

h 0.495 110 0.05 500 5,000 17.7 Subgrade 0.489 110 0.05 750 5,000 39.5

0.479 110 0.05 1,000 5,000 69.8 0.451 110 0.05 1,500 5,000 154.8

* There are four different S-wave velocities for each subgrade. **Thickness of subgrade (h) was varied from 5.5 to 90ft.

21

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The results of the analytical simulation of the FWD test were expressed in terms of deflection ra­tios (ratios of dynamic deflections to static deflec­tions) as a function of depth to bedrock. These re­sults are presented in Appendix B and are discussed below.

4.3 DEFLECTION BASINS

A typical example of the deflection basins created by the FWD test as a function of depth to bedrock is shown in Figure 4.1. The dynamic deflections at all measurement stations (receiv­ers) vary only at shallow bedrock depths, depths ranging from 5.5 to about 10 feet (1.7 to 3.1 m), as shown in Figure 4.1a. This is quite different from the Dynaflect test, in which large varia­tions in bedrock depth, ranging from 25 to 85 feet (7.8 to 26.3 m), influenced the measured dynamic deflections.

As in the case of the Dynaflect test, the maxi­mum deflection ratio also occurs at the farthest receiver station in the FWD test. However, the resonance peak exhibited in the FWD deflection ratios is much wider than that in the Dynaflect test and decreases more slowly to 1 when com­pared with the sharp decrease in the deflection ratio in the Dynaflect test. This difference is easily seen by comparing Figures 3.1c and 4.1c. The reason for this difference is that the FWD test contains a wide range in frequencies, while the Dynaflect test contains mainly one fre­quency (8 Hz).

A second observation about the deflection ra­tio in the FWD test is that the deflection ratio at the first measurement station (under the load) remains nearly equal to 1 throughout the entire range of bedrock depths. This indicates that there is little dynamic effect on the measured surface motions at the FWD source.

Dynamic and static deflection basins as a function of distance from the source obtained at the peak deflection ratio (termed the resonant depth to bedrock) are shown in Figure 4.2 and 4.3 for Profile 1 (flexible pavement) with unsat­urated and saturated subgrade conditions, respec­tively. As can be seen, there is little difference at the source between dynamic deflections and static deflections for Profile 1 with the softest subgrade (Figure 4.2a). The differences between dynamic deflections and static deflections be­come larger as the distance from the source in­creases. This behavior explains why the deflec­tion ratio at the nearest station is the smallest and the deflection ratio at the farthest station is the largest, as illustrated in Figure 4.1 c.

22

2.0

-<>- Station 1 .........,.. Station 2 --- Station 3 -o- Station 4 ~StationS -o- Station 6 -Station 7

.-................................. .

10 20 30 40 so 60 70 80 90 100 Depth to Bedrock (ft)

(a) Dynamic deflections

0 1 0 30 40 so 60 70 80 90 1 00

0

Figure 4.1

Depth to Bedrock (ft)

(b) Static deflections

20 40 60 80 Depth to Bedrock (ft)

(c) Deflection ratios

Deflection basins obtained with FWD testing for Profile 1 with unsaturated subgrade conditions (V5 of subgrade = 500 fps (155 m/s) and E = 16 ksi (0.11 MN/m2))

100

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0.0 ~0.2 = 0.4 _so.6 c: 0.8 gl.O u 1.2 ~1.4 ~ 1.6

1.8

• tJ

• 0

• tJ • IJ

• IJ

o Dynamic Deflections • Static Deflections

2.0 c;_ __ ..~.-__ '-----L---'----'-----'

0 1 2 3 4 5 6 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 500 fps (E = 16 ksi)

0.0 ~0.2 = 0.4 _so.6 c: 0.8

.Q 1.0 ti 1.2 ~1.4 ~ 1.6

1.8

Iii Iii

a Dynamic Deflections • Static Deflections

2.0 D----..1.-----''---...... --...... --....... ----' 0 1 2 3 4 5 6

Distance from the Source (ft)

(b) S-wave velocity of subgrade = 1,5 00 fps (E = 142 ksi)

Figure 4.2 Deflection basins as a function of distance from the FWD source for Profile 7 with unsaturated subgrade conditions

For the stiffest subgrade condition, there is little difference between the dynamic deflections and the static deflections, as shown in Figure 4.2b. This indicates that deflection ratios obtained from stiff subgrade conditions are smaller than those ob­tained from soft subgrade conditions. For the satu­rated subgrade conditions at Profile 1, the trends are similar to those first described for the unsatur­ated subgrade conditions, as shown in Figure 4.3.

Similar plots of deflection basins as a function of distance from the source for Profile 4 (rigid pavement) are shown in Figures 4.4 and 4.5 for unsaturated and saturated subgrade conditions, re­spectively. The amplitudes of the deflection basins are much smaller than those obtained with Pro­file 1, because the surface layer of Profile 4 is much thicker and stiffer than that of Profile 1. There is also less variation in the deflection ba­sins with the distance from the source than in Profile 1. This response can be seen by compar­ing Figures 4.2a and 4.4a. This occurs because Profile 4 represents a rigid pavement, while Pro­file 1 represents a very flexible pavement. For saturated subgrade conditions (Figure 4.5), the trends are similar to those just described for the unsaturated subgrade conditions (Figure 4.4).

23

0.0 -;;:)' 0.2 = 0.4 5o.6 c: 0.8

.Q 1.0 ti 1.2 ~1.4 ~ 1.6

1.8

• []

• 0

• 0

o Dynamic Deflections • Static Deflections

2.0 ....___ __ ..___ ........ __ __,_ __ _._ __ ..~.-_---J

0 1 2 3 4 5 6 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 500 fps (E = 16 ksi)

0.0 -;;:)' 0.2 = 0.4 ..§,o.6 c: 0.8 .Q 1.0 ti 1.2 ~ 1.4 ~ 1.6

1.8

i i i i i

c Dynamic Deflections • Static Deflections

2.0 D.------''---......1..---'------''------L.---' 0 1 2 3 4 5 6

Distance from the Source (ft)

(b) S-wave velocity of subgrade = 1,500 fps (E = 142 ksi)

Figure 4.3 Deflection basins as a function of distance from the FWD source for Profile 7 with saturated subgrade conditions

4.4 RESONANT DEPTH TO BEDROCK

The analytical simulations of the FWD tests for the four pavement profiles were expressed in terms of deflection ratios (ratios of dynamic de­flections to static deflection) as a function of depth to bedrock. The resonant depth to bedrock for each pavement profile with each subgrade stiffness was determined as the depth to bedrock corresponding to the maximum deflection ratio. These results are presented in Appendix B.

The resonant depths to bedrock as a function of various subgrade stiffnesses for the four pave­ment profiles are summarized in Figure 4.6. The resonant depths to bedrock obtained with the FWD test varied from 5.5 to 20 feet (1.7 to 6.2 m), which are much shallower depths when compared with the resonant depths to bedrock obtained with the Dynaflect test (varied from 25 to 85 feet (7 .8 to 26.3 m)). This is because the predominate frequency in the FWD test is about 30 Hz, so the resonant depths to bedrock ob­tained with the FWD test are approximately one fourth of those obtained with the Dynaflect test (f = 8 Hz).

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0.0 -:;;-0.2 = 0.4 _§,0.6 c 0.8 .Q 1.0 ~1.2 ;:;::::1.4 ~ 1.6

1.8 o Dynamic Deflections • Static Deflections

2.0e,_ _ __. __ ..... __ ....__~--"---...J

0 1 2 3 4 5 6 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 5 00 fps (E = 16 ksi)

0.0 -:;;- 0.2 = 0.4 _§,o.6 c 0.8 .Q 1.0 ~ 1.2 ;:;:::: 1.4 ~ 1.6

1.8

0 0 0

o Dynamic Deflections • Static Deflections

2.0 c.... _ __..__ _ __._ __ .._ _ __..__ _ __._ _ __,

0 1 2 3 4 5 6 Distance from the Source (ft)

(b) S-wave velocity of subgrade = 1,5 00 fps (E = 142 ksi)

Figure 4.4 Deflection basins as a function of distance from the FWD source for Profile 4 with unsaturated subgrade conditions

~ 25 ......, ..::t! e 20

~ .s 15

-:5 0.. ~ 10 +-' c til c 0

~ 5

0

• Profile 1

8 Profile 2 0 Profile 3 121 Profile 4

500 (16) 750 (36) 1,000 (63) 1,500 (142)

V5 of Subgrade, fps (E, ksi)

(a) Unsaturated subgrade conditions

0.0 -:;;- 0.2 = 0.4 _§,o.6 c 0.8

.Q 1.0 ti 1.2 £ 1.4 ~ 1.6

1.8

0 0 0

c Dynamic Deflections • Static Deflections

2.0 .._ _ __. __ ..... _ ___..___~--.&.-----J

0 2 3 4 5 6 Distance from the Source (ft)

(a) S-wave velocity of subgrade = 500 fps (E = 16 ksi)

0.0 -:;;-0.2 ::: 0.4 _§,o.6 c 0.8 .Q 1.0 ti 1.2 £ 1.4 ~ 1.6

1.8

0

c Dynamic Deflections • Static Deflections

2.0c....._ ....... __ .._ _ __. __ _._ __ ...._ _ __,

0 2 3 4 5 6 Distance from the Source (ft)

(b) S-wave velocity of subgrade = 1,5 00 fps (E = 142 ksi)

Figure 4.5

g 25

..::t! e 20 "C

QJ al

.s -:5

15

fr 10 0

5

0

Deflection basins as a function of distance from the FWD source for Profile 4 with saturated subgrade conditions

• Profile 1 !;;1 Profile 2

0 Profile 3 r..;!l Profile4

500 (16) 750 (36) 1,000 (63) 1,500 (142)

V5 of Subgrade, fps (E, ksi)

(b) Saturated subgrade conditions

Figure 4.6 Resonant depths to bedrock for FWD testing at the four pavement profiles with various subgrade stiffnesses

Page 35: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

T I

As can be seen in Figure 4.7, the resonant depths to bedrock (RDb) form two groups: one for the flex­ible pavements (Profiles 1, 2, and 3) and the other for the rigid pavement (Profile 4). For flexible pave­ments, a straight line was fitted, which resulted in:

ROb = 0. 013V s (4.1)

with H in feet and Vs in feet per seconds (fps). For the rigid pavement, a second-order polyno­mial curve was fitted, which resulted in:

ROb= 0.011V5 (4.2)

with RDb in feet and V5 in fps. Equations 4.1 and 4.2 can also be expressed in terms of Young's Modulus (E) as:

ROb= 0.0043-JE (4.3)

for flexible pavements with the unit weight of the subgrade material assumed to be 110 pounds per cubic foot (pcf), Poisson's ratio assumed to be 0.33, RDb in feet and E in pounds per square foot (psf), and

RDb = 0. 0036-JE (4.4)

for the rigid pavement with RDb in feet and E in psf.

4.5 AMPLITUDE OF THE MAXIMUM DEFLECTION RATIO

The amplitude of the deflection ratio (dy­namic deflection divided by static deflection) at each measurement station is an important index of the potential error generated in any static in­terpretation procedure. Figure 4.8 shows the maximum deflection ratios as a function of vari­ous subgrade stiffnesses for the four pavement profiles. It should be noted that, as in the Dynaflect test, the maximum deflection ratio of the FWD test always occurs at the farthest mea­surement station (station 7).

As can be seen in Figure 4.8, the amplitudes of the maximum deflection ratios of the four pavement profiles decrease as the stiffness of the subgrade increases (for both unsaturated and saturated subgrade conditions). This means that the accuracy of backcalculated layer moduli based on the static interpretation method should

25

improve as the subgrade stiffness increases. The results of backcalculated layer moduli using the MODULUS program (presented in Chapter 5) show this trend.

Young's Modulus of Subgrade (ksi) 16 36 63 100 142

25n-------~------~------r-------n

4? ........ ~ 20 u e

"C CIJ al 15 0 ......

..c: ...... c.. (LI 10 0

...... c:: o Profile 1 !!:S c:: c Profile 2 0 5 • Profile 3 VI (LI

• Profile 4 0:::

ou_ ______ ._ ______ ~------~----~ 500 750 1,000 1,250 1,500

Shear Wave Velocity of Subgrade (fps)

Figure 4.7 Curve fitting of the resonant depth to bedrock for FWD testing at the four pavement profiles with various subgrade stiffnesses

There are some numerical problems with satu­rated subgrade conditions at shallow depths to bedrock (see Appendix B). The amplitudes of the maximum deflection ratio of station 7 were esti­mated according to the trend of the first three measurement stations (which were not affected by the numerical problems).

The estimated amplitudes of the maximum deflection ratios of the four pavement profiles obtained with saturated subgrade conditions are generally larger than those obtained with unsat­urated subgrade conditions. This indicates that the backcalculated layer moduli obtained at pave­ment sites with unsaturated subgrade conditions based on a static interpretation method should be more accurate than those obtained at sites with saturated subgrade conditions.

Complete discussions on the accuracy of back­calculated layer moduli using a static interpreta­tion computer program (MODULUS) are presented in Chapter 5.

Page 36: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

------------··········-·~--··---------

0

~ 1:: 0 :a Q)

~ 0

E ::I E ·~

4

3.5

3

2.5

2

1.5

2 0.5

.Q ...., Ia c::: 1:: 0

:;:::; u Q)

~ 0 E ::I E ·x Ia

0

4

3.5

3

2.5

2

1.5

2 0.5

0

• Profile 1 E3 Profile 2 0 Profile 3 rll Profile 4

500 (16) 750 (36) 1,000 (63) 1,500 (142)

Vs of Subgrade, fps (E, ksi)

(a) Unsaturated subgrade conditions

• Profile 1 ~Profile 2 0 Profile 3 ~ Profile4

500 (16) 750 (36) 1,000 (63) 1,500 (142)

V5 of Subgrade, fps (E, ksi)

(b) Saturated subgrade conditions

figure 4.8 Maximum deflection ratios for FWD testing at the four pavement profiles with various subgrade stiffnesses

4.6 ESTIMATION OF DEPTH TO BEDROCK FROM THE FWD TEST

Chang et al (1992) developed a procedure for predicting the depth to bedrock based on the damped natural period of the free vibrations of the pavement system immediately after the FWD load application. Figure 4.9 illustrates the damped natural periods in the time-deflection records obtained from FWD tests with four shallow depths to bedrock. It should be noted that a much longer time interval (say 0.15 to 0.20 sec­onds) than normally recorded (0.06 seconds) must be measured to record the free vibrations.

Additional studies have been conducted herein. In these studies, various stiffnesses of the subgrade layer

26

and different subgrade saturation conditions have been examined. This work was performed to provide a more complete evaluation of the estimation of bedrock depth. Three different degrees of saturation for unsaturated subgrade conditions were simulated by using Poisson's ratio of 0.20, 0.33, and 0.40 while keeping the shear wave velocity constant. The rest of the material properties are the same as those in Table 4.1 (except for the P-wave velocity). The material properties for the case of saturated subgrade condi­tions are shown in Table 4.2.

Four different shallow depths to bedrock-S, 7.5, 10, and 20 feet (1.5, 2.3, 3.1, and 6.1 m)-were studied. These depths were selected because the resonant depth to bedrock for the FWD test was al­ways within 20 feet (6 m) of the pavement surface, as shown in Figure 4.2, unless a very stiff subgrade (V5 > 1,500 fps (458 m/s)) was encountered. The damped natural periods obtained with various Poisson's ratios, stiffnesses of subgrade, and depths to bedrock are presented in Appendix C.

4.6. f Unsaturated Subgmde Conditions

The depth to bedrock versus damped natural period of the free vibration for each pavement profile with an unsaturated subgrade with Poisson's ratio of 0.20 is shown in Figure 4.10. It is obvious that there is a linear (or nearly linear) relationship between depth to bedrock and damped natural period for each stiffness of the subgrade. It should be noted, as was noted in Chapter 3, that depth to bedrock is defined as the total depth from the top of the pavement to the top of the bedrock.

Figure 4.11 is a combined plot of the results from:

(a) the flexible pavement profiles (Profiles 1, 2, and 3), and

(b) the rigid pavement profile (Profile 4).

The relationships between depth to bedrock and damped natural period for the flexible pavements can be expressed as:

Tdl.08y u3 Db= s

5.325 (4.5)

with the shear wave velocity of the subgrade (V s) in feet per second, the damped natural period (Tct) in seconds, and the depth to bedrock (Db) in feet. For the rigid pavement, the expression becomes:

Td l.lly 1.14 Db= s

5.433 (4.6)

with Db in feet, Vs in feet per second, and Tct in seconds.

Page 37: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

-c.. ~ 2.0 -..!!! .E 1.5 '-' 1.0 c: 0 0.5 :p u Q) 0.0 ;;:: Q) 0.00 0 0.05 0.10 0.15 0.20

Time (sec)

(a) Depth to bedrock = 5 feet

-c..

·E 1.5 ~2.0~

I ~:~ ~-d,..,.; .... J ___ =----. ~ 0.00 0.05 0.1 0 0.15 0.20

Time (sec)

(b) Depth to bedrock = 7.5 feet

-c..

..!!! ·E 1.5

I

~2.0k

I ~~~-~--.---~ ~ 0.00 0.05 0.10 0.15 0.20

Time (sec)

(c) Depth to bedrock = 7 0 feet

-c.. ~

~Rl. -..!!! .E '-' c: Td/2 0 ,~ "'I :p u Q)

;;:: . . . Q) 0.00 0.05 0.10 0.15 0.20 0 Time (sec)

(d) Depth to bedrock = 20 feet

Figure 4.9 Deflection-time histories in FWD testing and damped natural periods (Td) for Profile 1 with various depths to bedrock (Vs of Subgrade = 500 fps (155 m/s) and E = 16 ksi (0.11 MNjm2))

27

Z' ~ ~ u 0 ....

"'C Q)

1:0 0 +-'

20

15

10

5 ..r:. +-' c.. Q)

0 0.00

0

g -D 20

e 15 "'C ~ 10

.8 5

£ 0 c.. Q) 0.00 0

g ~ u 20 0 15 ....

"'C Q) 10 1:0 0 5 +-'

..r:. 0 +-' c.. Q)

0

g ~ 20 u e 15

'"C ~ 1Q

',

.8 5\

0.00

[/

£ 0 fr 0.00 0

Figure 4.10

T I I I I -l o V5 = 500 fps, E = 16 ksi

• • 1: 0 D V5 = 750 fps, E = 36 ksi • V5 = 1,000 fps, E = 63 ksi - • V5 = 1,500 fps, E = 142 ksi

0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(a) Profile 7

- - " .... r I I I "I I

o V5 = 500 fps, E = 16 ksi

,1!,. 4 t p D V5 = 750 fps, E = 36 ksi • V5 = 1,000 fps, E = 63 ksi • V5 = 1,500 fps, E = 142 ksi

0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(b) Profile 2

l I I I 1 I

- ... o V5 = 500 fps, E - 19 ksi

• I D -0 D V5 = 750 fps, E = 42 ksi . • V5 = 1,000 fps, E = 75 ksi - •V~ 1,500 tps, E = 168 ksi

/

o.o2 or,64 o.o6 o.o8 0.1 o Dam1ped Natural Period (sec)

I

0.12

I (c) Profile 3

)

I I

o V5 = 500 fps, E = 16 ksi D V5 = 750 fps, E = 36 ksi • V5 = 1,000 fps, E = 63 ksi • V5 = 1,500 fps, E = 142 ksi

. -~· D.,. c

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(d) Profile 4

Depth to bedrock versus damped natural period of the pavement system for FWD testing at the four pavement profiles with various stiffnesses of unsaturated subgrade (Poisson's ratio = 0.20)

Page 38: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

~20~-,--,--,~--~~~~------~~~

~ -o 1 5 1!--t--hf-t-------.~--bi!L-f----t-----±.;fiC-t--+----l-e "0 ~ 101!--t-.~~~r-~~~~~--~~~--~

o V5 = 500 fps, E = 16 ksi 0 +-'

..c. +-' c... Q)

0

5

0

1::1 V5 = 750 fps, E = 36 ksi lf-_.,.!;Jgl!f-::.,iii'----1'----+---H • V

5 = 1,000 fps, E = 63 ksi

• V5 = 1,500 fps, E = 142 ksi

0.00 0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(a) Flexible pavements

~20~-,--~~~~~~--~~----~--~·

~ -o 1 5 H---t----1---lr-----i~+-~--+--+--,o~iF----f---+----, 0 ....

"0

~ 10~-J~~~~-t~~~~~~~~~~ o V5 = 500 fps, E = 1 6 ksi

H--JIII;II;I.,/11'0-...,..,.~--+---H 1::1 V5 = 750 fps, E = 36 ksi 0 +-'

..c. 5 +-' c... • V5 = 1,000 fps, E = 63 ksi

• V5 = 1 ,500 fps, E = 142 ksi Q)

0 0 0.00 0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(b) Rigid pavements

Figure 4. 11 Depth to bedrock versus damped natural period of the pavement system for FWD testing at: (a) flexible pave­ments and (b) rigid pavements (Poisson's ratio of the unsaturated subgrade = 0.20)

The depth to bedrock versus damped natural period of each pavement profile with an unsatur­ated subgrade with Poisson's ratio of 0.33 is shown in Figure 4.12. The data from the three flexible profiles and one rigid pavement were plotted separately and linear curve fits were per­formed with the various subgrade stiffnesses, as shown in Figure 4.13. The fitted curves can be expressed by the following equations:

Td 1.08y 1.13 Db= s

4.821 (4.7)

for the flexible pavements with Db in feet, V5 in feet per second, and Tct in seconds, and

Td l.lly 1.14 Db= s

5.045 (4.8)

for the rigid pavement, with Db in feet, V5 in feet per second, and Tct in seconds.

g -o 20 e 15 "0 ~ 10

.s 5

£ 0 c... ~ 0.00

........ ~ ..:.:. 20 u 0 15 ....

"0 Q) 10 a:J

0 5 +-'

..c. 0 +-'

- fW I I T'"' I I I o V5 - 500 fps, E= 1 6 ksi -•• a ~0 1::1 V5 = 750 fps, E = 36 ksi eV5 = 1,000fps, E = 63 ksi • V5 = 1,500 fps, E = 1 42 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(a) Profile 7

--.

- - 1-.-. Cc -c... Q)

0 0.00 0.02 0.04 0.06 0.08 0.10 0.12

g -o 20 e 15 "0 ~ 10

.s 5 ..c. '5.. 0 ~ 0.00

g

Damped Natural Period (sec)

(b) Profile 2

-..-

~- I!. 0

O.Q2 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(c) Profile 3

r~11 t-E·! 1° 11111~ c... ~ 0.00 O.Q2 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(d) Profile 4

Figure 4.12 Depth to bedrock versus natural period of the pavement system for FWD testing at the four pavement profiles with various stiffnesses of unsaturated subgrade (Poisson's ratio of subgrade = 0.33)

Page 39: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

~20r--r-.~~-r~--.mr-r-.--~*r-.~

t "0 15 tt--+--li-~'-+A-+-'21f'!'---l-+--+---f--l e "'0 ~ 1 o H---hf"1~.P.-t::7'!:..._-l==:::::b:d=k::::::b:d=L., .S •V5 =500fps,E=16ksi -:5 5 J.l-.al!MS4-:AH--+--l-~ o V5 = 750 fps, E = 36 ksi o... a V5 = 1,000 fps, E = 63 ksi QJ • V5 = 1,500 fps, E = 142 ksi 0 0

0.00 0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(a) Flexible pavements

~lor~-.-,-~-,~~~~-.-.-~~--. ...... ~

"0 15 H----+--lriY----I-:..._~+--+--::;;;o~+--+-f------1 e "'0 ~ 1 0 l+--l--.tlf---G~~-I:fli'l!q_-l----1f--+--+---11---1

.s -:5 5~~ .. ~~~---+--~1------+-~+----+-~ 0... Q)

o o~~=C===±==~~==±===~~= 0.00 0.02 0.04 0.06 0.08 0.1 0 0.12

Damped Natural Period (sec)

(b) Rigid pavements

Figure 4.13 Depth to bedrock versus damped natural period of the pavement system for FWD testing at: (a) flexible pave­ments and (b) rigid pavements (Poisson's ratio of subgrade = 0.33)

For the case of the subgrade having Poisson's ratio equal to 0.40, the linear relationship be­tween depth to bedrock and the damped natural period of each profile is shown in Figure 4.14. The combined plot of the flexible pavement and rigid pavement and curve fitting are shown in Figure 4.15. The equations are:

4.317 (4.9)

for the flexible pavement, with Db in feet, V5 in feet per second, and T d in seconds, and

Tdl.lly 1.14 Db= s

4.657 (4.10)

for the rigid pavement, with Db in feet, V5 in feet per second, and T d in seconds.

29

0 t--o 20 e 15

"'0 Ji 10

.s 5 .s:::. 0.. 0 ~ 0.00

g .::.! 20 u 0 15 ....

"'0 Q) 10 al

.s 5 .s:::. 0 ......

I• I I i I I I

- 1- - eV5 = 500fps, E= 16 ksi OV5 = 750fps, E=36 ksi

·~~ c_ c: DV5 = 1,000fps, E= 63 ksi • V5 = 1,500 fps, E = 142 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(a) Profile 1

.. I I I I I I

- • V5 = 500 fps, E = 16 ksi o V5 = 750 fps, E = 36 ksi •• q 0 D V5 = 1,000 fps, E = 63 ksi ..... • V5 = 1,500 fps, E = 142 ksi

0... Q)

0 0.00 0.02 0.04 0.06 0.08 0.10 0.12

g .::.! 20 u e 15

"'0 Ji 10

.s 5

-:5 0 g. 0.00 0

-t -o 20 e 15

"'0 Ji 10

.s 5

-:5 0 g. 0.00 0

Damped Natural Period (sec)

(b) Profile 2

- l I I -1 I I • V5 = 500 fps, E = 19 ksi - -

I e o (1 o V5 = 750 fps, E = 42 ksi DV5 = 1,000fps, E= 75 ksi • V5 = 1,500 fps, E = 168 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(c) Profile 3

- -- '1 I I "I

~· ~ D )

• V5 = 500 fps, E- 16 ksi o V5 = 750 fps, E = 36 ksi D V5 = 1 ,000 fps, E = 63 ksi • V5 = 1 ,500 fps, E = 142 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(d) Profile 4

Figure 4.14 Depth to bedrock versus natural period of the pavement system for FWD testing at the four pavement profiles with various stiffnesses of unsaturated subgrade (Poisson's ratio of subgrade = 0.40)

Finally, the equations for the flexible pave­ments with different Poisson's ratios ( u) of sub­grade can be combined into one equation. The equation thus becomes:

(4.11)

Page 40: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

with V5 in feet per second, Td in seconds, and Db in feet.

The equations for the rigid pavement with vari­ous Poisson's ratios (u) can also be combined into one equation. The equation then becomes:

Tdl.nv 1.14 Db= s

(6.21- 3.88u) (4.12)

with V5 in feet per second, Td in seconds, and Db in feet.

Equations 4.11 and 4.12 can be simplified as the linear equations shown in Table 4.3. The co­efficient of determination (r2) for these simplified equations ranged from 0.97 to 0.98. It is more convenient and easier to use the simplified equa­tions listed in Table 4.3 than the nonlinear equa­tions described above.

4.6.2 Saturated Subgrade Conditions

For saturated subgrade conditions, there are four different values for Poisson's ratios (0.495, 0.489, 0.479, and 0.451) which correspond to the four stiffnesses of the subgrade that result in the P-wave velocity of the subgrade equaling 5000 fps (1525 m/ s)(Table 4.2). Figure 4.16 shows the depth to bed­rock versus damped natural period for each profile. The combined data of the three flexible pavements and one rigid pavement are shown in Figure 4.17. The fitted equation for the flexible pavement is:

Db= 0.456V 1·03Td1.07

s (4.13)

~20rr--,-.~~-g~~~,---~~~--~ :c. ~ 15~-r-1~~-b~--~~-+--~~-+~ e -o ~ 10~~~~f-.j7~r±~~~~~~~~ .S 0 V5 = 500 fps, E = 16 ksi ..c: 5 1+-IIEII6-I...-+--+---I--II:J V5 = 750 fps, E = 36 ksi 0. • V5 = 1,000 fps, E = 63 ksi

~ 0~~~==~~~~·~~===1:,5cO:O=fp=s=,E~===14=2=ks~i 0.00 0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

Figure 4.15

(a) Flexible pavements

(b) Rigid pavements

Depth to bedrock versus damped natural period of the pavement system for FWD testing at: (a) flexible pave­ments and (b) rigid pavements (Poisson's ratio of subgrade = 0.40)

Table 4.3 Simplified equations for estimating depth to bedrock with unsaturated subgrade conditions

Correspond to

Equations Simplified Equations ?- Units Equations

4.11 Db= vs Td 0.97 Db: ft 4.1la (1t- 2.24 U) V5: fps

Td:sec

4.11 Db= Td j E 0.97 Db: ft 4.11b (8.21-5.86 u) (1+u) E: psf

Td: sec

4.12 Db= vs Td

0.98 Db: ft 4.12a

(1t • 1.44 U) V5: fps Td: sec

4.12 Db= Td j E 0.98 Db: ft 4.12b (8.21-3.75 u) (1+u) E: psf

Td: sec

Page 41: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

with V5 in feet per second, Td in seconds, and Db in feet. The fitted equation for the rigid pavement can be expressed as:

Db= 0.396V/"05TdLOS (4.14)

with V5 in feet per second, Td in seconds, and Db in feet.

Z' :::::, ..::.:: 20 u 0 15 .... "0 Q) 10 co .s 5 .!::. 0 ..... 0. Q)

0

Z' :::::, ..::.:: u 20

e 15 "0 Q) 10 co .s 5 .!::. 0 ..... 0. Q)

0

Z' :::::, ..::.:: 20 e 15

-g 10 co .s 5

0.00

0.00

t 0 Q) 0.00 0

Z' :::::, ..::.:: 20

e 15 -g 10 co .s 5

t 0 Q) 0.00 0

Figure 4.16

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(a) Profile 1

-- -I I I 1 I I 0 V

5-500fps,E-18ksi .-. t:l..,. 0

D V5 750 fps, E = 40 ksi • V5 1,000 fps, E = 70 ksi • V5 = 1,500 fps, E = 155 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(b) Profile 2

--, -I I I 1 I I I

- - - 0 V5 = 500 fps, E-21 ksi c V5 = 750 fps, E = 47 ksi

!• .... c 0 • V5 = 1,000 fps, E = 83 ksi • V5 = 1,500 fps, E = 183 ksi

0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(c) Profile 3

- -l I I .I I I I

- Ia "' 0 vs 500 fps, E = 18 ksi c V5 = 750 fps, E = 40 ksi •• ~- 0 • V5 1,ooo tps, E = 70 ksi • V5 = 1,500 fps, E = 155 ksi

0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(d) Profile 4

Depth to bedrock versus natural period of the pavement system for FWD testing at the four pavement profiles with various stiffnesses of saturated subgrade

31

0.00 0.02 0.04 0.06 0.08 0.10 0.12 Damped Natural Period (sec)

(a) Flexible pavements

~20rr--.--.-~-r9-.-~----~~-.--.-• ..... :::::, -o 15 H--+---;f-1--H4-Af--+-cJI!f--l---+---l----l---l e "0 ~ 1 0 l+--+~117-~-1-¥11--+-c--1--l---+---l---t--1

.s .!::. 51+-~~~4--+~f--4--+--t---+--+---1---1

0. Q)

o o~==~===±==~====~==~==~ 0.00 0.02 0.04 0.06 0.08 0.10 0.12

Damped Natural Period (sec)

(b) A rigid pavement

Figure 4.17 Depth to bedrock versus damped natural period of the pavement system for FWD testing at: (a) flexible pave­ments and (b) a rigid pavement (satu­rated subgrade conditions)

Equations 4.13 and 4.14 can be simplified as the linear equations listed in Table 4.4. The coef­ficient of determination for these simplified equa­tions ranged from 0.98 to 0.99.

4.7 ESTIMATION OF THE SUBGRADE STIFFNESS FROM FWD TESTS

To use the equations in Section 4.6, a good estimate of the stiffness of the subgrade is re­quired. The stiffness of the subgrade can be esti­mated by in situ seismic testing, by dynamic labo­ratory tests on undisturbed samples, or possibly by experience. However, a more convenient and accurate way to estimate subgrade stiffness was developed in this project. It was observed that one could measure the offset time (To) of the first pulse on the time-deflection records, as shown in Figure 4.18. The offset time is related to Rayleigh wave velocity of the subgrade. With the assump­tions discussed below, and knowing the distance between two measurement stations, one can de­termine the shear wave velocity.

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There are several assumptions which must be made to use the offset time method. First, the sub­grade should be able to be approximated as a uni­form material. Second, the wavelength should be long enough so that the surface, base, and subbase layers have little effect on the Rayleigh wave ve­locity. Generally, this means that the wavelength should be at least 10 times the total thickness of the surface, base, and subbase layers for untreated bases and subbases. Third, the bedrock needs to be deep enough so that it has little effect on the Rayleigh wave velocity. This condition is usually met if the bedrock depth is greater than 0.5 times the Rayleigh wavelength in the subgrade. Fourth, it is assumed that the near-field effects are so small that they can be ignored. Fifth, the first pulses of stations 5 and 7 were used to measure the offset time, because the deflections obtained at the sta­tions away from the source should better represent the properties of the subgrade. Finally, the differ­ence between the Rayleigh wave velocity and the shear wave velocity is less than 10 percent if Poisson's ratio of the material is greater than 0.2 (Richart, 1970), so it can be ignored. (Note: These assumptions frequently may not apply in normal test situations.)

Table 4.5 illustrates an example of comparisons between the estimated shear wave velocity of the subgrade and the actual shear wave velocity for Profile 1 with an unsaturated subgrade with Poisson's ratio equal to 0.20. Good estimations of the shear wave velocity of the subgrade are made in the case of the softest subgrade. However, as the stiffness of the subgrade increases, there are cases where estimations cannot be made. This happens because the first pulses in the deflection­time records were distorted and the peaks could

not be determined, as shown in Figure 4.19. This effect may result from analytical approximations and deserves future investigation.

1.5

-a. ;g_ 1.0 ~ .E ..._,

0.000 0.010 0.020 O.o30 0.040 0.050 lime (sec)

Figure 4.18 Offset time of the first pulses between station 5 and station 7 for FWD testing at Profile 1 (Vs of subgrade = 500 fps (155 m/s), E = 16 ksi (0.1 1 MN/m2), depth to bedrock = 5 feet (1.6 m))

4.8 SUMMARY

The FWD test was studied analytically using computer program UTFWD (Chang, 1991; Chang et al, 1992). Four pavement profiles, the same as those used in the study of the Dynaflect test, were studied. The stiffness of the subgrade layer was varied to simulate a typical range in pave­ment materials.

Table 4.4 Simplified equations for estimating depth to bedrock with saturated subgrade conditions

Correspond to

Equations

4.13

4.13

4.14

Simplified Equations

Db= 2~~2 Td

Db=~Td 7.0

Db=~Td 2.31

Db= .J E Td 7.28

32

r2 0.99

0.99

0.98

0.98

Units

Db:ft Vs: fps Td: sec

Db: ft E: psf Td: sec

Db:ft Vs: fps Td: sec

Db: ft E: psf Td: sec

Equations

4.13a

4.13b

4.14a

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Table 4.5 Estimated shear wave velocity of subgrade from offset time of the first pulses for FWD testing at Profile 1*

Units: V5 (fps), E (ksi) Actual V 5 of Subgrade (E of Subgrade)

500 (16) 750 (36)

Depth to Estimated Estimated Bedrock To vs Error- To Vs Error

(ft) (sec) (fps) (o/o) (sec) (fps) (o/o)

5 0.0035 571 14 na *** na na 7.5 0.0039 513 3 0.0028 714 -5 10 0.0040 500 0 0.0029 690 -8 20 0.0042 476 -5 0.0030 667 -11

Actual V5 of Subgrade (E of Subgrade)

1,000 (62) 1,500 (142)

·Depth to Estimated Estimated Bedrock To vs Error To Vs Error

(ft) (sec) (fps) (o/o) (sec) (fps) (o/o)

5 na na na na na na 7.5 na na na na na na 10 0.0020 1,000 0 na na na 20 0.0021 952 -5 0.0013 1,538 3

* Poisson's ratio of Subgrade equals 0.20. **Error= [(Estimated V5 /Actual VJ -1]* 1000!6

*** Offset time is not available because the first pulses in FWD tests are distorted.

Equations for estimating the resonant depth to bedrock were developed for both the flexible and rigid pavements. Saturated subgrade conditions did not change the trend of the resonant depth to bedrock with the stiffness of subgrade that was found under unsaturated subgrade conditions. The resonant depths to bedrock obtained with the FWD test with various subgrade stiffnesses are ap­proximately one fourth of the resonant depths to bedrock obtained with the Dynaflect test. This is because the predominate frequency in the FWD test is about 30 Hz, which is about four times the frequency of the Dynaflect test (8 Hz).

Equations for estimating the depth to bedrock based on the damped natural period of the free vibrations of the pavement system immediately after the FWD load application have been pre­sented. In these equations, effects of stiffness and degree of saturation of subgrade were taken into account.

A method for estimating the stiffness of the sub­grade by the offset time of the first pulses at two measurement stations of the deflection-time records in FWD tests has been developed. The shear wave velocity of the subgrade can be estimated by divid­ing the offset time by the distance between these two stations. At present, it seems that this approach

33

is more appropriate in those cases where the stiff­ness of the subgrade is soft to moderately stiff (V s

= 500 to 750 fps (155 to 233 m/s) or E = 16 to 36 ksi (0.11 to 0.25 MN/m2) or where the bedrock depth is 10 feet (3.1 m) or more.

-c.. :.i2 .._ ..!!:! .E ........ c 0 ; u QJ

;;:: QJ

0

60

40

20

0

0.000 0.01 0 0.020 0.030 0.040 0.050

lime (sec)

Figure 4.19 Distorted first pulses in FWD records obtained at Profile 1 with the stiffest subgrade and bedrock depth = 7.5 feet

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34

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CHAPTER 5. INFLUENCE OF DYNAMIC DEFLECTIONS ON BACKCALCULATED LAYER MODULI IN THE FWD TEST

5.1 INTRODUCTION

The computer program MODULUS (Uzan et al, 1989), which is based on static interpretation of the FWD test, was used to backcalculate layer moduli from the dynamic deflection basins ob­tained with the UTFWD program (Chang, 1991; Chang et al, 1992). The backcalculated moduli were then compared with the actual moduli used to generate the deflection basins.

The values of the moduli and the thicknesses of the pavement layers of the four pavement pro­files were used to obtain the deflection basins using UTFWD. These deflection basins were then used as input parameters along with the actual thicknesses of the pavement layers. The backcal­culated moduli from MODULUS were then deter­mined using the "Run a Full Analysis" option in MODULUS.

The main purpose of these studies was to inves­tigate the accuracy of backcalculating layer moduli from FWD measurements with a static interpretation method. The effects of the follow­ing conditions were studied:

1. depth to bedrock; 2. stiffness of the subgrade; and 3. saturated versus unsaturated subgrade condi­

tions.

The stiffnesses of the base and surface layers were not studied. Based on the results of the study with the Dynaflect presented in Chapter 3, our research indicates that the stiffness of the sub­grade and the depth to bedrock are the main fac­tors influencing the dynamic deflections.

5.2 MODEL PARAMETERS

As in the parametric study of the FWD pre­sented in Chapter 4, only the depth to bedrock and stiffness of the subgrade were varied. The stiffnesses of the other pavement layers were kept constant, such that the shear wave velocity of the CRC equaled 8500 fps (2593 m/s) (E = 5425 ksi

35

(37.4 MN/m2)), the shear wave velocity of the AC equaled 3000 fps (915 m/s) (E = 690 ksi (4.8 MN/ m 2)), and the shear wave velocity of the base equaled 1000 fps (305 m/s) (E = 67 ksi (0.46 MN/ m2)). The shear wave velocity of the subgrade layer was varied from 500 to 1500 fps (150 to 450 m/s) and the corresponding Young's modulus var­ied from 16 to 142 ksi (0.11 to 0.98 MNJm2).

To simulate an unsaturated subgrade, a Poisson's ratio of 0.33 was used. The material properties of the four pavement profiles with unsaturated subgrade conditions are given in Table 4.1. To simulate a saturated subgrade, the P­wave velocity of the subgrade was set equal to 5000 fps (1525 m/s). The shear wave velocities of the subgrades were varied from 500 to 1500 fps (150 to 450 m/s), as in the unsaturated subgrade condition. As a result, Poisson's ratio varied from 0.495 to 0.451, asS-wave velocity of subgrade var­ied from 500 to 1500 fps (150 to 450 m/s). Hence, Young's modulus for the saturated subgrade var­ied from 18 to 155 ksi (0.12 to 1.07 MN/m2). The material properties of the four pavement profiles with saturated subgrades are given in Table 4.2.

5.3 DEFLECTION BASINS

Three kinds of deflection basins were used in the backcalculation study of layer moduli with MODULUS. A schematic illustration of the rela­tive locations of the bedrock depths where these three deflection basins were taken is shown in Figure 5.1. The first basin was the dynamic de­flection basin obtained at the resonant condi­tion, as shown in Figure 5.1a. This deflection basin is denoted as the R-basin (resonant basin) and represents the case where static and dy­namic deflections exhibit the largest differences, as shown in Figure 5.2. The second basin is for the static deflection basin obtained at the same depth to bedrock as the R-basin, but with a static loading applied to the pavement. This basin, denoted as the S-basin (Static basin), rep­resents a case where one could presumably per­form a backcalculation, based on a known depth

Page 46: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

- 2.0 Ill c..

:.;;:: --. 1.5 ...!!! .E ~ 1.0 0

tl Q) 0.5

'Qj

-+- Station 1 -113- Station 2 -X- Station 3 -!1- Station 4 ""*"Station 5 -o- Station 6 -x- Station 7

Dynamic Deflections at Deep Subgrade Site

0 0.0 ~U..........L---JL...-...l.---1..---1'--...l.-.....1..---L---J 0 1 0 20 30 40 50 60 70 80 90 1 00

Depth to Bedrock (ft)

-~ .E .......... c 0 ;; u <IJ

w 0 u ;; ~

+-' V')

2.0

1.5

1.0

0.5

(a) Dynamic deflections

-+- Station 1 -113- Station 2 -x- Station 3 -!1- Station 4 ""*"StationS -o- Station 6 -x- Station 7

0.0 L-11~---1-..L........L-.L.---1..'--L-.......1----L----' 0 1 0 20 30 40 50 60 70 80 90 1 00

Depth to Bedrock (ft)

(b) Static deflections

Figure 5.1 Three kinds of deflection basins used to backcalculate layer moduli for FWD testing at Profile 7 (V5 of unsaturated subgrade = 500 fps (155 m/s) and E = 7 6 ksi (0. 7 7 MNfmZ))

to bedrock. This is an erroneous assumption be­cause the dynamics of the test still have not been taken into account. The third basin is the dynamic deflection basin obtained at each pro­file where the bedrock lies at a significant

depth. A bedrock depth of 80 feet (24 m) was selected to represent this case. As seen in Figure S.la, this case represents the condition far away from the resonant condition where static and dynamic measurements are nearly the same. This case is denoted as the N-basin (non-reso­nant basin) and represents the case where a static backcalculation scheme should involve the fewest approximations .

-+-Station 1 -fl- Station 2 -x- Station 3 -m- Station 4 -:lE- Station 5 -o- Station 6 -X- Station 7

3.0 I I

2.5 I 0 I

·.p I ~

c::: c 2.0 I 0 I Deep Subgrade Site I 1 :;::; u Q)

~~ ~ 1.5 0

1.0

0 20 40 60 80 100 Depth to Bedrock (ft)

Figure 5.2 Deflection ratio versus depth to bedrock for FWD testing at Profile 7 (V5 of unsaturated subgrade = 500 fps (1 55 m/s) and E = 7 6 ksi (0. 7 7 MN/m2))

These three deflection basins at Profile 1 with unsaturated subgrade conditions are shown in Figure 5.3. For the case of the softest subgrade conditions, there is little difference at the source between dynamic deflections obtained at the resonant condition (R-basin) and the equivalent static deflections (S-basin) as shown in Figure 5.3a. The difference between the R­basin and S-basin becomes larger as the distance from the source increases. This behavior ex­plains why the deflection ratio at the nearest measurement station is the smallest and the deflection ratio at the farthest measurement

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station is the largest in the FWD test at reso­nance, as illustrated in Figure 5.2. The deflec­tion basin obtained at the deep subgrade site (N-basin) exhibits the largest deflections because the thickest section of subgrade material is be­ing strained. However, it is interesting to note that for the N-basin the dynamic deflections are slightly less than the static deflections-a result of inertia in the pavement system.

For the stiffest subgrade condition, there is little difference between the R-basin, S-basin, and N-basin, as shown in Figure 5.3b. This indicates that deflection ratios obtained from stiff subgrade conditions are smaller than those obtained from soft subgrade conditions. This relationship is clearly seen by comparing deflection ratios shown in Appendix B.

5.4 BACKCALCULATION OF LAYER MODULI OBTAINED FROM PROGRAM MODULUS

The results of the backcalculated layer moduli for the four pavement profiles are summarized in Tables 5.1, 5.2, 5.3, and 5.4 for Profiles 1, 2, 3 and 4, respectively. The backcalculated modu­lus is denoted as Ec and the actual (assumed) modulus used to generate the deflection basin is denoted as Eo in Tables 5.1 to 5.4. The dif­ference between the backcalculated and the ac­tual modulus is represented by the ratio of back­calculated modulus to actual modulus and is denoted as Ec/Eo.

5.4.1 Profile 1

Subgrade Moduli of Profile 1

For unsaturated subgrade conditions, the back­calculated subgrade moduli obtained from the R­basins are 20 percent to 50 percent less than the actual moduli, as shown by the solid symbols in Figure 5.4a. These differences generally decrease as the stiffness of subgrade increases. This trend oc­curs because deflections increase as the stiffness of the subgrade decreases.

The errors in backcalculated subgrade moduli obtained from N-basins and S-basins are less than

37

20 percent. This result indicates that backcalculated moduli obtained from dynamic deflection basins are quite accurate for FWD measurements performed well away from the resonant bedrock depth.

For saturated subgrade conditions, there are several cases where the MODULUS program does not converge to the backcalculated layer moduli (Table 5.1b). This is a natural case in which MODULUS, a statically based analysis, cannot converge with some dynamically generated deflec­tion basins. However, with the available data in Figure 5.4b, one can see that, basically, the satu­rated subgrade condition exhibits trends similar to those exhibited in the case of the unsaturated subgrade conditions.

0.0 ....... 0.2 .~ 0.4 .s 0.6 c 0.8 0 1.0 t 1.2 ..5!::! 1.4 'Qj 1.6 Cl 1.8

2.0 ~

0

!! I • 01

1:1 R-basin • $-basin oN-basin

I

1 2 3 4 5 6 Distance from the Source (ft)

(a) 5-wave velocity of subgrade = 500 fps, E = 7 6 ksi

0.0 ....... 0.2 ~ 0.4 .E o.6 ';;' 0.8 0 1.0 t 1.2 Q) 1.4 ii 1 6 Cl .

1.8 2.0

~

0

I Ill

c R-basin • $-basin oN-basin

2 3 4 5 6

Distance from the Source (ft)

(b) 5-wave velocity of subgrade = 7 500 fps, E = 7 42 ksi

Figure 5.3 Three kinds of deflection basins for FWD testing at Profile 7 (V5 of unsaturated subgrade = 500 fps (155 m/s) and E = 7 6 ksi (0. 7 7 MN/m2))

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Table 5.1 Comparison of backcalculated layer moduli with actual moduli for FWD tests at Profile 1

(a) Unsaturated subgrade conditions

V5 of Subgrade (fps)

500 750 1,000 1,500 -Deflection Basin N* R** S*** N R s N R s N R s

Thickness of 947 59 59 947 117 Subgrade (in.) 117 947 137 137 947 227 227

AC True Eo 690 690 690 690 690 690 690 690 690 690 690 690 (ksi) CompEc 2,319 8,508 4,112 1,978 5,433 1,783 1,202 1,539 214 473 611 447

Ec/Eo 3.36 12.33 5.96 2.87 7.87 2.58 1.74 2.23 0.31 0.68 0.89 0.65 Base True Eo 67 67 67 67 67 67 67 67 67 67 67 67 (ksi) Comp Ec 68 118 75 71 93 68 71 77 71 77 77 71

Ec/Eo 1.01 1.76 1.12 1.06 1.39 1.02 1.06 1.14 1.07 1.15 1.14 1.05 Sub grade True Eo 16 16 16 36 36 36 63 63 63 142 142 142 (ksi) Comp Ec 17 9 14 35 23 34 60 52 71 119 115 149

Ec/Eo 1.06 0.53 0.88 0.97 0.65 0.95 0.95 0.82 1.13 0.84 0.81 1.05

(b) Saturated subgrade conditions

V s of Subgrade (fps)

500 750 1,000 1,500

Deflection Basin N R s N R s N R s N R i s Thickness of 947 59 59 947 117 Subgrade (in.)

AC True Eo 690 690 690 690 690 (ksi) Comp Ec - - - 2,379 7,409

Ec/Eo - - - 2.51 63.32 Base True Eo 67 67 67 67 67 (ksi) Comp Ec - - - 74 150

Ec/Eo - - - 1.10 2.24 Sub grade True Eo 18 18 18 40 40 (ksi) Comp Ec - - - 38 25

Ec/Eo - - - 0.96 0.63

* Dynamic deflection basins at deep subgrade site ** Dynamic deflection basins at resonant depth to bedrock

*** Static deflection basins at resonant depth to bedrock

117 947 137 137 947 227

690 690 690 690 690 690 1,722 1,910 - 187 606 1,387 14.71 2.02 - 1.36 0.64 6.11

67 67 67 67 67 67 69 70 - 76 76 77

1.03 1.04 - 1.13 1.13 1.14 40 70 70 70 155 155 40 64 - 72 149 130

1.02 0.91 - 1.03 0.96 0.84

Note: MODULUS program does not successfully converge at some cases so that some backcalculated moduli cannot be determined.

227

690 512

2.26 67 72

1.07 155 171 1.10

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Table 5.2 Comparison of backcalculated layer moduli with actual moduli for FWD tests at Profile 2

(a) Unsaturated subgrade conditions

V s of Subgrade (fps)

500 750 1,000 1,500

Deflection Basin N* R** S*** N R s N R s N R s Thickness of 950 62 62 950 110 110 950 140 140 950 230 230 Subgrade (in.)

AC True Eo 690 690 690 690 690 690 690 690 690 690 690 690 (ksi) Comp Ec 1,329 5,157 1,374 1,083 2,604 1,032 1,515 1,358 1,469 1,701 1,213 2,675

Ec/Eo 1.93 7.47 1.99 1.57 3.77 1.50 2.20 1.97 2.13 2.47 1.76 3.88 Base True Eo 67 67 67 67 67 67 67 67 67 67 67 67 (ksi) CompEc 281 270 359 267 445 263 181 285 173 116 173 68

Ec/Eo 4.19 4.03 5.36 3.99 6.64 3.93 2.70 4.25 2.58 1.73 2.58 1.01 Subgrade True Eo 16 16 16 36 36 36 63 63 63 142 142 142 (ksi) Comp Ec 18 9 14 36 24 34 60 so 130 113 145

Ec/Eo 1.11 0.58 0.88 1.00 0.68 0.95 0.96 0.79 0.92 0.80 1.02

(b) Saturated subgrade conditions

V s of Subgrade (fps)

500 750 1,000 1,500

Deflection Basin N R s N R s N R R s Thickness of 950 62 62 950 110 110 950 140 230 Subgrade (in.)

AC True Eo 690 690 690 690 690 690 690 690 (ksi) Comp Ec 1,105 4,506 9,545 1,039 3,676 972 1,512 1,178

Ec/Eo 1.60 6.53 13.83 1.51 5.33 1.41 2.19 1.71 Base True Eo 67 67 67 67 67 67 67 67 (ksi) CompEc 395 1,469 284 321 598 300 197 429

Ec/Eo 9.22 21.93 4.24 4.79 8.93 4.48 2.94 6.40 Subgra True Eo 18 18 18 40 40 40 70 70 (ksi) CompEc 19 9 13 38 25 37 64 51

Ec/Eo 1.07 0.51 0.73 0.96 0.63 0.94 0.92 0.73 * Dynamic deflection basins at deep subgrade site

**Dynamic defection basins at resonant depth to bedrock *** Static deflection basins at resonant depth to bedrock

39

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Table 5.3 Comparison of backcalculated layer moduli with actual moduli for FWD tests at Profile 3

(a) Unsaturated subgrade conditions

V5 of Subgrade (fps)

500 750

Deflection Basin N* R** I .,. N R s N

Thickness of 947 59 59 947 117 117 947 Subgrade (in.)

AC True Eo 715 715 715 715 715 715 715 (ksi) Comp Ec 617 366 645 617 452 596 641

Ec/Eo 0.86 0.51 0.90 0.86 0.63 0.83 0.90 Base True Eo 70 70 70 70 70 70 70 (ksi) CompEc 117 593 84 125 566 105 104

Ec/Eo 1.68 8.47 1.20 1.78 8.09 1.50 1.49 Subgrade True Eo 19 19 19 42 42 42 75 (ksi) Comp Ec 21 10 21 42 29 40 72

Ec/Eo 1.11 0.55 1.13 1.01 0.68 0.96 0.97 (b) Saturated subgrade conditions

V 5 of Subgrade (fps)

500 750

Deflection Basin N R s N R s N

Thickness of 947 59 59 117 117 947 Subgrade (in.)

AC True Eo 715 715 715 715 715 715 715 (ksi) CompEc 466 894 1,600 516 543 611 585

Ec/Eo 0.65 1.25 2.24 0.72 0.76 0.85 0.82 Base True Eo 70 70 70 70 70 70 70 (ksi) CompEc 250 895 480 193 857 99 143

Ec/Eo 3.57 12.79 6.86 2.75 12.25 1.42 2.04 Subgrade True Eo 21 21 21 47 47 47 83 (ksi) CompEc 22 9 16 46 30 47 78

Ec/Eo 1.06 0.43 0.76 0.97 0.65 1.00 0.94 * Dynamic deflection basins at deep subgrade site

**Dynamic defection basins at resonant depth to bedrock *** Static deflection basins at resonant depth to bedrock

1,000 1,500

R s N R s

137 137 947 227 227

715 715 715 715 715 522 736 647 561 752

0.73 1.03 0.91 0.79 1.05 70 70 70 70 70

253 67 87 124 63 3.62 0.95 1.25 1.76 0.89

75 75 168 168 168 55 75 157 135 174

0.74 1.00 0.93 0.80 1.04

1,000 1,500

R s N R s 137 137 947 227E

715 715 715 715 715 509 789 608 564 759

0.71 1.10 0.85 0.79 1.06 70 70 70 70 70

308 62 102 127 67 4.39 0.88 1.45 1.82 0.95

83 83 183 183

m1 61 87 169 150 0.74 1.06 0.92 0.82 1

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Table 5.4 Comparison of backcalculated layer moduli with actual moduli for FWD tests at Profile 4

(a) Unsaturated subgrade conditions

Vs of Subgrade (fps)

500 750 1,000 1,500

Deflection Basin N* R** S*** N R s N R s N R s Thickness of 932 38 38 932 62 62 932 92 92 932 182 182 Subgrade (in.)

CRC True Eo 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 (ksi) Comp Ec 8,487 7,339 4,463 6,146 6,154 4,746 5,658 4,583 5,624 6,421 5,847 5,777

Ec/Eo 1.56 1.35 0.82 1.13 1.13 0.88 1.04 0.84 1.04 1.18 1.08 1.07 AC True Eo 715 715 715 715 715 715 715 715 715 715 715 715 (ksi) Comp Ec 278 241 959 1,040 225 954 376 840 494 255 305 287

Ec/Eo 0.39 0.34 1.34 1.45 0.31 1.33 0.53 1.17 0.69 0.36 0.43 0.40 Subbase True Eo 67 67 67 67 67 67 67 67 67 67 67 67 (ksi) CompEc 83 296 83 47 225 70 125 196 81 107 165 103

Ec/Eo 1.24 4.42 1.23 0.70 3.36 1.04 1.87 2.93 1.21 1.60 2.46 1.53 Sub grade True Eo 16 16 16 36 36 36 63 63 63 142 142 142 (ksi) CompEc 27 7 13 50 23 33 75 46 68 155 122 153

Ec/Eo 1.71 0.43 0.78 1.39 0.63 0.92 1.20 0.73 1.08 1.09 0.86 1.08 (b) Saturated subgrade conditions

Vs of Subgrade (fps)

500 750 1,500

Deflection Basin N R s N R s N R s Thickness of 932 38 38 932 62 62 932 182 182 Subgrade (in.)

CRC True Eo 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 5,424 (ksi) CompEc 9,143 4,230 6,574 5,042 5,608 4,888 5,779 6,283 5,262

Ec/Eo 1.69 0.78 1.21 0.93 1.03 0.90 1.07 1.16 0.97 AC True Eo 715 715 715 715 715 715 715 715 715 (ksi) CompEc 314 2,321 605 1,639 381 1,174 587 1,728 279 962

Ec Eo 0.44 3.25 0.85 2.29 0.53 1.64 0.82 2.42 0.39 Subbase True Eo 67 67 67 67 67 67 67 67 (ksi) CompEc 94 71 20 60 338 44 264 64

1.40 1.06 0.30 0.90 5.04 0.66 2.30 0.96 Subgrad 18 18 18 40 40 40 70 70 1 (ksi) 30 6 14 54 24 45 83 55 140

1.69 0.32 0.75 1.36 0.61 1.14 1.19 0.78 0.90

* Dynamic deflection basins at deep subgrade site **Dynamic defection basins at resonant depth to bedrock

***Static deflection basins at resonant depth to bedrock

41

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w "'ia ::I 1.8 ..... u <( 1.6 0 ..... 1.4

w "C 1.2 (I)

"5 1.0

E- o.8 8 0.6

- 0.4 0

16 Young's Modulus of Subgrade (ksi)

36 63 100 142

D N-basin • R-basin 0 S-basin ___________ o __________ _

::L----c-----r::r---------~ ~-----------•----------~ ~

0 0.2 c.,_ ___ _.__ ___ ...._ ___ ......_ __ ___._.

·.;::::; 500 ~

750 1,000 1,250 1,500 S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

w Young's Modulus of Subgrade (ksi)

"'ia 18 40 70 108 155 .a 1.8 ~ 1.6 .8 1.4 w

[J N-basin • R-basin 0 S-basin

"C 12 ------------------------

"[ 1.0 ~----=-~~~-~--~~-=-~~-~----=-~~ E 0.8 0 0.6 u 0 0.4 0 0.2

~ 500 750 1,000 1,250 1,500 c:::

S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

Figure 5.4 Ratio of backcalculated subgrade moduli to actual subgrade moduli for FWD testing at Profile 1 with various subgrade stiffnesses

Base Moduli of Profile 1

For unsaturated subgrade conditions, backcalcu­lated base moduli obtained from both the S-basins and N-basins are very close to the actual moduli, as shown in Figure 5.5a. The differences are less than 15 percent, with the backcalculated moduli always larger. The backcalculated base moduli obtained from R-basins overestimate the actual moduli by 15 percent to 180 percent. This is be­cause the backcalculated subgrade moduli ob­tained at R-basins are all too low. The poorest estimation was obtained with the softest subgrade because it involves the largest motions.

For the saturated subgrade condition, there are several cases where, for unknown reasons, the MODULUS program does not successfully

42

backcalculate moduli, as shown in Table 5.1 b. According to the available data, the trends are similar to those for the unsaturated subgrade, except that the errors obtained from the R-ba­sins are even larger, as seen by comparing the solid points in Figures 5.5a and 5.5b.

Young's Modulus of Subgrade (ksi) 1 6 36 63 1 00 142

w Ia ::I 2.2 ..... u

2.0 <(

0 1.8 .....

w "C 1.6 2 ::I 1.4 c.. E 1.2 0

.

. [J N-basin • R-basin 0 S-basin

-----------------------! 5.------B----~----------·c u 1.0

0 O 0.8 - - - - - -, - - - - - - - - - - - - r - - - - -,

:;::::; 500 750 1,000 1,250 1,500 ~ S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

Young's Modulus of Subgrade (ksi) w

155 "'ia 18 40 70 108 .3 2.2 rri!.------:o • .-----.....----"T""""----rr

~ 2.0 .8 w 1.8

"C 1.6 2 5.. 1.4

[J N-basin • R-basin 0 S-basin

E 1.2 -------------------------• 8 1.0 ____ _£J ____ _B __________ ~ 0 0 0.8 ... ----- ... -----....,----- -·------

~ 500 750 1,000 1,250 1,500 S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

Figure 5.5 Ratio of backcalculated base moduli to actual base moduli for FWD testing at Profile 1 with various subgrade stiffnesses

AC Moduli of Profile 1

For the unsaturated and saturated subgrade con­ditions, the backcalculated AC moduli are at least two times larger than the actual AC moduli when the subgrade has a V5 of 1000 fps (310 m/s) (E = 63 ksi (0.43 MN/m2)) or less, as shown in Table 5.1. However, the backcalculated moduli obtained with N-basins and S-basins with the stiffest subgrade exhibit good values (differences < 15 percent).

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r

S.4.2 Profile 2

Subgrade Moduli of Profile 2

For Profile 2 with unsaturated subgrade condi­tions, the differences between backcalculated and actual subgrade moduli obtained from the N-basins (deep subgrade) and S-basins (static) are less than about 20 percent, as shown in Figure 5.6a. The backcalculated subgrade moduli obtained from the R-basins (resonant conditions) are 30 percent to 40 percent lower than the assumed actual moduli, as shown by the solid points in the figure.

Again, the saturated subgrade conditions exhibit a trend similar to that of the unsaturated subgrade conditions, as shown in Figure 5.6b. The errors in the backcalculated subgrade moduli obtained from the R-basins in the saturated subgrade conditions are about 5 percent higher than those in the un­saturated subgrade conditions.

w Young's Modulus of Subgrade (ksi) -ro 16 36 63 100 142 .a 1.8 ,.:.;::., ---.::.r---__;;;;---....;.;r=---......:....n .7t 1.6 .s1.4 w

C N-basin • R-basin 0 S-basin

"0 1.2 :i-------------------------5 1.0 ~----g----.,-----------~ ~Q8~-----------·-----------· 8 0.6. •

0 0.4 0 0.2 I:.' • .___ __ __. ___ ....~.. ________ ......

·.o:; 500 &.

7 50 1,000 1 ,250 1,500 S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

w Young's Modulus of Subgrade (ksi) 1'\'S 18 40 70 108 155 .a 1.8 ,.:.;::., ---..:.r---__;;.;---....;.;r=---.....;.;;; .7t C N-basin

• R-basin 0 S-basin

1.6 .s 1.4 w "0 1.2 ------------------------

-5 1.0 tL----g-----a----------~ ~ 0.8 p - - - - - - - - - - - i - - - - - - - - - - - •

8 0.6 It • 0 0.4 0 0.2 r:.,_ ___ .......... ___ ......._ ___ .___ __ ......a.J

~ 500 750 1,000 1,250 1,500 0:: S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

Figure 5.6 Ratio of backcalculated subgrade moduli to actual subgrade moduli for FWD testing at Profile 2 with various subgrade stiffnesses

43

Base Moduli of Profile 2

For Profile 2 with unsaturated subgrade con­ditions, the backcalculated base moduli ob­tained from all of the deflection basins are at least 2 times higher than the actual moduli, except for the stiffest subgrade case (see Figure 5.7a). For saturated subgrade conditions, the backcalculated base modulus from the R-basin with the softest subgrade condition is 25 times higher than the actual modulus. For the unsat­urated subgrade conditions, there is good agree­ment in the backcalculated layer moduli for the stiffest subgrade condition.

w Young's Modulus of Subgrade (ksi) -ro 16 36 63 100 142 ~ 25~----~----T---....;.;~---~ ...., C N-basin .S 20 • R-basin w 0 S-basin

"0 15 • ~ 5.. 10 -E 0 u 5 ~ ~ •

0 0 ········-·····-··-······-··················~··-·-·········-·-·-·-·-·········-·., 0

':;:l 1'\'S

0:: 500 750 1,000 1,250 1,500

S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

w Young's Modulus of Subgrade (ksi) -ro 1 8 40 70 1 08 1ss .a 25~---~----~T----....;.;r:::----~ .7t • .s 20 w "0 15 ~ ::I o..10t:J e E •

0 N-basin • R-basin o S-basin

8 Sp 1:1 0 ~ 0 ·········-······-·····-·-·-·-········--·0----·············-····--·-··········-~

':;:l

&. 750 1,000 1,250

S-Wave Velocity of Subgrade (fps) 1,500 500

(b) Saturated subgrade conditions

Figure 5.7 Ratio of backcalculated base moduli to actual base moduli for FWD testing at Profile 2 with various subgrade stiffnesses

AC Moduli of Profile 2

There is essentially no resolution in the backcal­culated AC moduli for both the unsaturated and saturated subgrade conditions, as shown in Table

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.-

5.2. The backcalculated AC moduli are always greater than the actual moduli. The errors in the backcalculated AC moduli are always greater than 40 percent and are generally more than 100 percent.

5.4.3 Profile 3

Subgrade Moduli of Profile 3

For unsaturated subgrade conditions, the back­calculated subgrade moduli obtained from the N­basins and S-basins are very close to the actual moduli (differences are less than 10 percent), as shown in Figure 5.8a. The backcalculated subgrade moduli obtained from the R-basins are 20 percent to 40 percent lower than the actual moduli. Satu­rated subgrade conditions exhibit similar trends, as seen by comparing Figures 5.8a and 5.8b.

LU

Iii :::l tJ 1.8 <( 1.6 0

19

Young's Modulus of Subgrade (ksi) 42 75 117

0 N-basin • R-basin

:; 1 .4 o S-basin

168

"0 1.2 Ci-- ----------------------5 1.0 ~----g-----er----------g ~ 0.8 - - - - - - ; - - - - - • - - - - - - - - - - - •

8 0.6.

0 0.4 0 0.2 c..,_ ___ _,__ ___ ~---'----_.._.

~ 500 750 1,000 1,250 1,500 c:: S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

LU Young's Modulus of Subgrade (ksi) Iii 21 45 83 128 183 .3 1.8 ,..;;;,,.;----,;.;;.__--...;;.r---~--__;-ri ~

1 .6

0 N-basin

0 -~~~ :; 1 .4 o S-basin

"0 1.2 -------------------------5 1.0 :L------r;;J-----&----------'? ~Q8 -----;-----e--- -------~ 8 0.6 t

0 0.4

0 0.2 E:..L..----'-----~---'-----£...1 ~ 500 ~

750 1,000 1,250 S-Wave Velocity of Subgrade (fps)

1,500

(b) Saturated subgrade conditions

Figure 5.8 Ratio of backcalculated subgrade moduli to actual subgrade moduli for FWD testing at Profile 3 with various subgrade stiffnesses

Base Moduli of Profile 3

For Profile 3 with unsaturated subgrade condi­tions, the backcalculated base moduli obtained from the R-basins are unrealistically high, espe­cially for the softest subgrade condition, as shown in Figure 5.9a. The differences in backcalculated base moduli obtained from the N-basins and S­basins (about 5 percent to 70 percent) are much less significant than those obtained from the R­basins (about 70 percent to 850 percent), but still quite different than the actual moduli, except for the stiffest subgrade condition. This trend results from the fact that the backcalculated subgrade moduli have been underestimated.

For saturated subgrade conditions, the backcal­culated base moduli are even higher than those obtained for the unsaturated subgrade conditions, as seen by comparing Figures 5.9a and 5.9b.

LU Young's Modulus of Subgrade (ksi) «l 19 42 75 11 7 168 :::l 14 r:;-:.r----T---,;,;;---.....;.;.;---......;,.;, <(t)

12 .9 LU 10

~ 8 ,

[ 6

E 4 0

C N-basin • R-~sin 0 S-basin

u 2 0 3-:-:: = ::~-==.:::.=::.e.::::==-==-==::=::~ 0 0 L...L-----'-----'----...._ __ --t.l ~

~ 500 750 1,000 1,250

S-Wave Velocity of Subgrade (fps) 1,500

(a) Unsaturated subgrade conditions

LU Young's Modulus of Subgrade (ksi) 21 45 83 128 183 Iii

.3 14~------T-------~-----~---~

~ 12 ~ 0 :; 10

"0 8 .l!S ... :::l 6 r-' a. E 8

500

• oN-basin • R-basin o S-basin

750 1,000 1,250

S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

1,500

Figure 5.9 Ratio of backcalculated base moduli to actual base moduli for FWD testing at Profile 3 with various subgrade stiffnesses

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AC Moduli of Profile 3

Profile 3 is the only flexible pavement pro­file which shows good resolution in backcalcu­lated AC moduli, as shown in Table S.3. For unsaturated subgrade conditions, the differ­ences between backcalculated AC moduli ob­tained from the N-basin and S-basin and actual moduli are less than IS percent. The difference in backcalculated AC moduli obtained from the R-basins vary from SO percent to 30 percent as the subgrade stiffness increases.

For the saturated subgrade condition, the errors in backcalculated AC moduli are considerably larger than those of the unsaturated subgrade condition for the softer subgrade.

5.4.4 Profile 4

Subgrade Moduli of Profile 4

For unsaturated subgrade conditions, the back­calculated subgrade moduli obtained from the N­basins overestimate the actual moduli by IO to 70 percent, as shown in Figure S.lOa. On the other hand, the backcalculated subgrade moduli obtained from the R-basins underestimate the actual moduli by IS percent to 60 percent. As expected, the back­calculated subgrade moduli obtained from the S-ba­sins have the least differences (within 20 percent).

The saturated subgrade condition exhibited a trend almost identical to that for unsaturated sub­grade conditions, as seen by comparing Figure S.lOa with Figure S.IOb.

Subbase Moduli of Profile 4

For Profile 4 with unsaturated subgrade con­ditions, the backcalculated subbase moduli ob­tained from the R-basins overestimate the ac­tual moduli by 240 percent to 440 percent, which are apparently incorrect, as shown in Figure S.lla. The errors in the backcalculated subbase moduli obtained from the N-basins and S-basins are much smaller than those obtained from the R-basins, but still vary from 20 percent to 80 percent. For saturated sub­grade conditions, as shown in Figure S.llb, the differences of backcalculated subbase moduli obtained from R-basins varied significantly (S percent to about SOO percent).

AC Base Moduli of Profile 4

Most of the backcalculated AC moduli do not show good comparisons with the actual moduli,

45

as presented in Table S.4. The. differences be­tween the backcalculated AC moduli and the actual moduli vary from IS percent to 32S per­cent, with the poorest case occurring at the soft­est subgrade condition.

CRC Moduli of Profile 4

The differences of the backcalculated CRC moduli for all deflection basins (in the case of unsaturated subgrades) are less than 20 percent, except for those obtained from the softest subgrade conditions (Table S.4). For saturated subgrade conditions, the trend is basically the same as can be seen by comparing Tables S.4a and S.4b.

Young's Modulus of Subgrade (ksi) w 16 36 63 100 142 "ia 1.8 ro-o--------..---------..... :;, 0 u 1.6

<C o1.4 o +"'

0 N-basin • R-basin o S-basin

w 1.2 ----------- -0---------- ---~ o e .$ 1.0 -----o·---------------· :;, . ~ ~:: p- - - - - -.- - - - - - ii - - - - - - - - - - - -

u '0 0.4 ' .2 0.2 r:.,_ ___ ........ ___ ,__ __ ___.,__ __ __.....

~ 500 a::. 750 1,000 1,250 S-Wave Velocity of Subgrade (fps)

1,500

(a) Unsaturated subgrade conditions

Young's Modulus of Subgrade (ksi) ~ 18 40 70 108 155 ~ 1.8

<Cti 1 .6 P 0 N-basin

• R-basin .8 1 .4 o S-basin

~ 1.2 ----- _o_---- _o_----------- 9 W 0 0 D =:; 1.0 ---------------------. 0. § 0.8 p---------- -.----- --------u 0.6 • -~ 0.4jlt ~ 0.2 b._ ___ ..a.,_ ___ ..a.,_ ___ .._ __ ---i.J

a::. 500 7 so 1,000 1,250 1,500 S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

Figure 5.10 Ratio of backcalculated subgrade moduli to actual subgrade moduli for FWD testing at Profile 4 with various subgrade stiffnesses

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Young's Modulus of Subgrade (ksi) ~ 16 36 63 100 142 3 5~~----~~------r-------~------~ ~ [] N-basin .9 4 • R-basin w 0~~~

] 3 ::I c.. E 2 • 0 u 't5 0

• • []

·.w ('1:1

c:::: 500 750 1,000 1,250 1,500

w ~ ::I .... 5 ~ .8 4 w

] 3 ....

18

S-Wave Velocity of Subgrade (fps)

(a) Unsaturated subgrade conditions

Young's Modulus of Subgrade (ksi) 40 70 108

• [] N-basin • R-basin 0 ~basin

155

::I [] • Q..2

§ ~ 0 [] ~ 1 _:-::::::e::-::-::~t:::::::::::-::::::o g p ~ ~------~------~------~------~~

('1:1 500 750 1,000 1,250 1,500 c:::: S-Wave Velocity of Subgrade (fps)

(b) Saturated subgrade conditions

Figure 5.11 Ratio of backcalculated base moduli to actual base moduli for FWD testing at Profile 4 with various subgrade stiffnesses

5.5 SUMMARY

In some cases, the R-basins and S-basins ob­tained with saturated subgrade conditions at shallow depth to bedrock might be affected by the numerical problems in UTFWD. The results

46

obtained with saturated subgrade conditions need further study.

Overall, the backcalculated subgrade moduli obtained from static deflection basins at resonant depth to bedrock (S-basins) and from dynamic deflection basins for deep subgrade profiles (N­basin), which represent nonresonant conditions, show better comparisons than those obtained with dynamic deflection basins at the resonant bedrock condition (R-basins).

The stiffness of the subgrade layer has a major effect on the accuracy of backcalculated layer moduli. The errors of the backcalculated layer moduli increase as the subgrade stiffness de­creases. This behavior also agrees with the trend of variations of maximum deflection ratios pre­sented in Section 4.5.

Profile 1, which has the thinnest surface layer, is the only profile which shows good comparisons in the backcalculated base moduli. For the other three profiles (Profiles 2, 3, and 4), the differences are generally greater than 100 percent, except for the stiffest subgrade condi­tions. For the results of the backcalculated AC moduli, Profile 3, which has the thickest surface layer in the three flexible pavements (Profiles 1, 2, and 3), shows the best comparisons. The dif­ferences are generally less than 15 percent for the backcalculated AC moduli obtained with the N-basins and S-basins. The relationship between the thickness of the surface layer and the accu­racy of the backcalculated AC and Base moduli needs further study.

Generally, the amplitudes of deflection basins (generated with 10,000-pound loading) are less than one-thousandth of an inch (mil). However, the default input format in MODULUS can only read two digits after the point (unit in mils)-pre­sumably because the FWD output provides data to only two digits after the decimal point. This might cause some reduction of resolution for backcalculated layer moduli obtained with the MODULUS program.

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CHAPTER 6. CONCLUSIONS AND RECOMMENDATIONS

6.1 CONCLUSIONS REGARDING THE DYNAFLECT TEST

Analytical simulations of the Dynaflect test were conducted using the computer program UTDYNF (Chang, 1991; Chang et al, 1992). Four typical in-service pavement profiles (three flexible pavements and one rigid pavement) were studied. The dynamic effect of the Dynaflect test was ex­pressed in terms of deflection ratios (dynamic deflections divided by static deflections).

At a given bedrock depth, the maximum value of deflection ratios is the largest for the furthest measurement station (station 5) and least for the nearest measurement station (sta­tion 1). At shallow depths to bedrock (approxi­mately 5 to 10 feet (1.55 to 3.1 m)), deflection ratios of all measurement stations are very close to 1, so the dynamic and static deflection basins are basically the same. The deflection ratio in­creases to a peak value as the depth to bedrock increases. After the peak, the deflection ratio drops rapidly back to 1. The maximum value of the deflection ratio (at station 5) ranged from 1.3 to 2.9 in these studies.

The resonant depth to bedrock (the depth to bedrock corresponding to the maximum deflection ratio) is determined predominately by the stiffness of the subgrade layer. Two sets of equations (one for the flexible pavements and one for the rigid pavement) were developed for estimating the reso­nant depth to bedrock based on the subgrade stiff­ness. For these pavements, Young's modulus of the subgrade varied from 16 to 142 ksi (0.11 to 0.98 MN/m2), and the resonant depth to bedrock ranged from 25 to 85 feet (7.8 to 26.3 m).

The amplitude of the deflection ratio is an im­portant index of the potential error generated in any static interpretation procedure of the Dyna­flect test. The stiffness of the subgrade layer has the most significant effect on the amplitude of the maximum deflection ratios. The softer the subgrade, the higher the amplitude of the maxi­mum deflection ratio. This trend indicates that

47

the error generated in a static interpretation pro­cedure of the Dynaflect test would decrease as the subgrade stiffness increases.

6.2 CONCLUSIONS REGARDING THE FWD TEST

Analytical simulations of the FWD test were conducted using the computer program UTFWD (Chang, 1991; Chang et al, 1992). Four pavement profiles, the same as those used in the study of the Dynaflect test, were studied.

As in the case of the Dynaflect test, the maxi­mum deflection ratio at a given depth to bedrock also occurs at the farthest measurement station (station 7) in the FWD test. However, the reso­nance peak exhibited in the FWD deflection ratios is much wider than that exhibited in the Dyna­flect test and decreases more slowly to 1 when compared with the sharp decrease in the deflec­tion ratio in the FWD test. The reason for these differences is that the FWD test contains a wide range in frequencies, while the Dynaflect test contains one frequency (8 Hz).

The resonant depth to bedrock obtained with the FWD test varied from 5.5 to 20 feet (1.7 to 6.2 m) when Young's modulus of the subgrade varied from 16 to 142 ksi (0.11 to 0.98 MN/m2). These resonant depths to bedrock are much shallower than those obtained with the Dynaflect test (var­ied from 25 to 85 feet (7.8 to 26.3 m)). This trend occurs because the predominate frequency in the FWD test is about 30 Hz, while the frequency used in the Dynaflect test is 8 Hz. Therefore, the resonant depths to bedrock obtained with the FWD test are approximately one fourth of those obtained with the Dynaflect test. Equations for es­timating the resonant depth to bedrock for the FWD test were developed for both the flexible and rigid pavements.

Equations are suggested for estimating the depth to bedrock based on the damped natural period of the free vibrations of the pavement sys­tem immediately after the FWD load application.

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In these equations, the stiffness of the subgrade has a major effect, while the degree of saturation of the subgrade is only marginally important. To use these equations, site engineers have to mea­sure the damped natural period in the deflection­time records of the FWD test and estimate the stiffness and Poisson's ratio of the subgrade.

A method for estimating the stiffness of the subgrade based on the offset time of the first pulses in the deflection-time recording in the FWD test has been developed. The method is best applied by using stations 5 and 7 in the FWD test. There are several assumptions that must be made when using this method. For ex­ample, the subgrade is approximated as a uni­form material, the bedrock needs to be reason­ably deep (this depends on the stiffness of the subgrade), and the difference between Rayleigh wave velocity and shear wave velocity is ne­glected. The most important advantage of this approach is that the stiffness of the subgrade can be estimated simultaneously with perfor­mance of the FWD test. The resonant depth to bedrock and the actual depth to bedrock can then be determined using the equations sug­gested in this study. Therefore, the error gener­ated by the resonant bedrock condition can be either avoided in advance or corrected during the backcalculation process.

The computer program MODULUS (Uzan et al, 1989), which is based on static interpretation of the FWD test, was used to backcalculate layer moduli from the deflection basins obtained with the UTFWD program. Generally, the backcalcu­lated layer moduli obtained from dynamic deflec­tions measured at deep subgrade sites (N-basins) and from static deflection basins at the resonant bedrock depths ($-basins) exhibit much better comparisons with the actual moduli than backcal­culated moduli obtained with dynamic deflections measured at the resonant bedrock condition (R­basins). Unfortunately, when FWD tests are per­formed at the resonant bedrock depth, dynamic deflections (not static) are measured.

At the resonant bedrock depth, the stiffness of the subgrade layer has a major effect on the ac­curacy of backcalculated layer moduli. The errors in the backcalculated layer moduli increase as the subgrade stiffness decreases. This behavior also agrees with the trend of variations in the maxi­mum deflection ratios.

Usually, backcalculated subgrade moduli ob­tained with dynamic deflection basins at the resonant depth to bedrock (R-basins) underesti­mated the actual subgrade moduli by 20 to 50 percent. This results in the backcalculated base

48

moduli being too high (generally 2 times the actual base moduli).

Profile 1, which has the thinnest surface layer, exhibits the best comparison for the backcalcu­lated base moduli (less than 20 percent of differ­ence) for theN-basins and $-basins. However, Pro­file 3, which has the thickest surface layer among these three flexible pavements, exhibits the best comparison on the backcalculated AC moduli (less than 20 percent of difference) for the N-basins and $-basins. Profile 4, which is a rigid pavement, exhibits good comparisons for the backcalculated CRC moduli. The differences are less than 20 per­cent for all these three deflection basins (N-, S­and R-basins).

The results obtained with saturated subgrade conditions need further study. Numerical prob­lems with UTFWD seemed to occur at shallow bedrock depths for saturated subgrade conditions. Changes in the mesh size may be necessary to improve calculations of the deflection basins un­der these conditions.

6.3 RECOMMENDATIONS

Dynaflect testing should be conducted with spe­cial care, since its fixed frequency (8 Hz) cannot detect resonant bedrock conditions. The errors gen­erated in backcalculated moduli using a static in­terpretation procedure can be significant if the test is performed at the resonant depth to bedrock.

A procedure for performing FWD testing is sug­gested below.

1. Estimate the Stiffness of the Subgrade The stiffness of the subgrade can be estimated by the offset time approach suggested in this study (simultaneously with the test), by in situ seismic testing (before the FWD test) or by dynamic laboratory tests on undisturbed samples (before the FWD test).

2. Estimate the Resonant Depth to Bedrock The resonant depth to bedrock can be deter­mined with the estimated subgrade stiffness (Step 1) using equations suggested in this study (Section 4.4).

3. Estimate the Actual Depth to Bedrock The actual depth to bedrock can be deter­mined based on the damped natural period of the free vibrations of the pavement sys­tem and the stiffness and Poisson's ratio of the subgrade. The stiffness of the subgrade can be determined by the offset time approach (Step 1). Site engineers have to

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estimate the saturation condition of the subgrade and an appropriate value for Poisson's ratio of the subgrade.

4. Compare the Actual Depth to Bedrock and the Estimated Resonant Depth to Bedrock If the actual depth to bedrock is more than 20 feet (6.2 m) (deeper than the estimated resonant depth to bedrock), any errors gen­erated in backcalculated moduli by a static interpretation procedure can be ignored. However, if the difference between the ac­tual depth to bedrock and the resonant depth to bedrock is less than 20 feet (6.2 m),

49

errors may be significant. In this case, the FWD test as presently performed needs to be analyzed dynamically.

The procedure just presented needs further field verifications. To measure the damped natu­ral period of the free vibrations, the record of the motions of the pavement system immedi­ately after the FWD load application should be extended to 200 milliseconds. The sampling rate in the data acquisition system of the FWD test should be less than 0.1 milliseconds, so the peak at each measurement station can be de­tected accurately.

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so

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BIBLIOGRAPHY

Chang, D. W. "Nonlinear Effects on Dynamic Response of Pavements Using the Non-Destructive Test­ing Techniques," doctoral dissertation, The University of Texas at Austin, 1991.

Chang, D. W., Kang, Y. V., Roesset, ]. M., and Stokoe, II, K. H., "Effect of Depth to Bedrock on Deflec­tion Basins Obtained with Dynaflect and FWD Tests," 1992 Annual Meeting of the Transporta­tion Research Board, Washington, D.C., 1992.

Davies, T. G., and Mamlouk, M.S. "Theoretical Response of Mutilayer Pavement Systems to Dynamic Nondestructive Testing," Transportation Research Record 1022, pp 1-7, 1985.

Heisey, S. "Determination of In Situ Shear Wave Velocity from Spectral Analysis of Surface Waves," master's thesis, The University of Texas at Austin, 1981.

Hoar, R. J. "Field Measurement of Seismic Wave Velocity and Attenuation for Dynamic Analyses," doctoral dissertation, The University of Texas at Austin, 1982.

Kang, Y. V. "Finite Width on Dynamic Deflections on Pavements," doctoral dissertation, The Univer­sity of Texas at Austin, 1990.

Kang, Y. V., Roesset ]. M., and Stokoe, II, K. H. "Effect of Loading Position on Deflection Basins Ob­tained with Dynaflect and FWD Tests," 1991 Annual Meeting of the Transportation Research Board, Washington, D.C., 1991.

Nazarian, S. "In Situ Determination of Elastic Moduli of Soil Deposits and Pavement System by Spec­tral-Analysis-of-Surface-Waves Method," doctoral dissertation, The University of Texas at Aus­tin, 1984.

Nazarian, S., and Stokoe, II, K. H. "Nondestructively Delineating Changes in Modulus Profiles of Sec­ondary Roads," Transportation Research Record 1136, pp 96-107, 1987.

Richart, F. E., Woods, R. D., and Hall, ]. R. Vibrations of Soils and Foundations. Prentice-Hall, Inc., 1970.

Roesset, ]. M., and Mamlouk, M. S. "Dynamic Interpretation of Dynaflect and Falling Weight Deflectometer Tests," Transportation Research Record 1022, pp 7-16, 1985.

Sansalone, M., and Carino, N. ]. "Detecting Delaminations in Concrete Slabs With and Without Over­lays Using the Impact-Echo Method," ACI Material Journal, 86, pp 175-84, 1990.

Uzan, ]., Lytton, R. L., and Germann, F. P. "General Procedure for Backcalculating Layer Moduli," ASTM STP 1026, American Society for Testing and Materials, pp 217-228, 1989.

51

Page 62: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3
Page 63: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

APPENDIX A. RESULTS OF ANALYTICAL SIMULATION OF THE DYNAFLECT TEST

The analytical simulation of the Dynaflect test was obtained using computer program UTDYNF (Chang, 1991; Chang et aC 1992). The motions are expressed in terms of deflection ratios as a function of depth to bedrock in this appendix. Deflection ratio is defined as the dynamic deflec­tion divided by the static deflection. Depth to bedrock is the total depth from the surface of the pavement to the top of the bedrock.

53

There are some numerical problems which caused small spikes on some of the deflection ra­tios. However, these numerical problems did not have any effect on the values of the maximum deflection ratios and the resonant depths to bed­rock. These spikes were removed from the figures in this appendix.

Page 64: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi 2.2

0 'i 2.0 ~1.8 c .:a 1.6

~ 1.4 t;:l <I) 1.2

Cl 1.0~~~~~~~~~~~~~~~~~r:R 0 10 '20 30 40 50 60 70 80 90 100 llO 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi

.:a 1.6 (;:i ~

.§ 1.4 ..... tJ ~ 1.2 <I)

Cl 1.0

~-j __ ~ ... ~ --··--1~-·----LaAL:~L .. __ i. _______ l ______ j_~_ul.~--···~--L .. ---··

~tw~tt~=t=t~~: 0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.:a 1.4 -1·--i---<-­(;:i ~ c .:a 1.2 ..... tJ

~ II)

Cl 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station I ....... Station2 ····Station 3 -- Station4

···-Station 5

-Station! ·--Station2 ····Station 3 -·Station 4

·-·- Station 5

-Station 1 "··-Station2 ····Station 3 --Station 4

·-·-Station 5

-Station I -·--Station 2 ····Station 3 --Station 4

···-Station 5

Figure A.1 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 2000 fps (E = 312 ksl) and V5 of base= 1000 fps (E = 67 ksi))

54

Page 65: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750fps, E= 36 ksi 1.8

0

~ 1.6 c .s 1.4 u ~ 1.2

o 1.o~~~;;T"i"i'T'u~~~~~~~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 1.6 ..... i$

" cl.4 0 ·--0 1.2 <U

t;:: <U 0

1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4 ..... -~ " c 0 ·= 1.2 0 <U

t;:: <U 0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -- Station2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 --·Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·-· Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ··-- Station 2 · • • • Station 3 --Station 4

·-·-Station 5

Figure A.2 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (Vs of AC = 2000 fps (E = 3 7 2 ksi) and Vs of base = 1500 fps (E = 7 52 ksi))

Page 66: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

kO~--~----~~------------------------------------------~

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 ·:: 1.6 = ~ s 1.4 ·­-<.)

~ 1.2 ~

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Subgrade = 1000 fps, E= 63 ksi 1.6

0 ·-5 - 1.4

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4 ·-.... = ~

= .E 1.2 -~ !!i: ~

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·-Station2 •••• Station 3 --Station 4

·-·-Station 5

-Station l ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·-Station2 ····Station 3 --Station 4

·-·-Station 5

-Station 1 -·Station 2 ·••• Station 3 --Station 4

·-·-Station 5

Figure A.3 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 2000 fps (E = 312 ksi) and V5 of base= 2000 fps (E = 270 ksi))

I

' t';

Page 67: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

Figure A.4

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 . 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ····-Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 --- Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 -Station2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 --· Station 2 •••• Station 3 -- Station4

·-·- Station 5

Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (Vs of AC = 3000 fps (E

= 690 ksi) and Vs of base = 1000 fps (E = 67 ksi))

57

Page 68: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

Figure A.5

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 1.8-r--~--~--~--~}A'i--~--~--~~--~--~--~--~

·~ 1.6 ~

§ 1.4 ·­.... u ~ 1.2-1-----

Q.)

0 1~~~~~~~~~~~nn~~~~~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 .... _ Station 2 ·••• Station 3 - - Station 4

·-·- Station 5

-Station 1 ·-- Station 2 ····Station 3 -- Station4

·-·-Station 5

-Station 1 .. -Station2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 ··-Station2 •••• Station 3 --Station 4

·-·-Station 5

Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 3000 fps (E = 690 ksi) and V5 of base= 1500 fps (E = 152 ksi))

58

I i

Page 69: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

{a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

{b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

.9 1.6~---------------------~-;~;~~~,~--~--------~--~--~--,

~ ~.· ~

i :: ~ll~~'~ftt=r~t~ 0 1.0 ~~··~· --~-----~---'-;; .... ~----·='·---:----·;;·-·-~---··n;·····~--··m··---~-·-~~~~~~~

0 10 20 30 40 50 60 70 80 90 100 110 120

{d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4 ·--d ~ c 0 1.2 ·-ti ~ .;:::: ~

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·····-Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ··-···Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ·---Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

Figure A.6 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 3000 fps (E

= 690 ksi) and V5 of base= 2000 fps (E = 270 ksi))

59

Page 70: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

Figure A.7

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

1.8

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

- Sta.tion 1 -Sta.tion 2 .... Station 3 -- Station4

·-·-Station 5

-Sta.tion 1 ··-·Station 2 ·••• Station 3 --Station 4

····Station 5

-Station 1 .. ,_ Station 2 •••• Station 3 - - Sta.tion 4

····Station 5

-Station 1 .... _ Station 2 ·••• Sta.tion 3 - - Station 4

···-Station 5

Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 1 (Vs of AC = 4000 fps (E = 1225 ksi) and Vs of base= 1000 fps (E = 67 ksi))

60

i' I

I L

Page 71: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi 2.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

1.6

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.52 1.4 ...... ca ~ c::

.S? 1.2 ...... C,.) 0

!;: 0 0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 """- Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 """""Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 "-···Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

Figure A.B Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (Vs of AC = 4000 fps (E

= 1225 ksi) and V5 of base= 1500 fps (E = 152 ksi))

61

),'' l

Page 72: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

---------------~~~~--

(a) Vs of Subgrade = 500 fps, E=16 ksi

.g 1.8 CIS

" 1.6 c: 0

·::: 1.4 0 Q.)

t;::: 1.2 Q.)

0 1.0

0 10 20 30 40 50 60 70 80

(b) Vs of Subgrade = 750 fps, E= 36 ksi

.g 1.6 tij c::: c:l.4 0 ·-.... 0 ~ 1.2

Q.)

0 1.0

0 10 20 30 40 50 60 70 80

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·-tij c::: 1.4 c: 0

·::: g 1.2 t;:::

Q.)

0 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4 ·-..... CIS c::: s ·::: 1.2 (.,) Q.)

t;::: Q.)

0 1.0

0 10 20 30 40 50 60 70 80 Depth to Bedrock (ft)

90 100 110

90 100 110

90 100 110

90 100 110

120

120

120

120

-Station 1 -Station2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 -Station2 •• •• Station 3 -- Station4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 -- Station4

·-·-Station 5

-Station 1 .; ..... Station 2 •••• Station 3 -- Station4

·-·-Station 5

Figure A.9 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 4000 fps (E = 1225 ksi) and Vs of base = 2000 fps (E ::::: 270 ksi))

62

l~ I

I I I

Page 73: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi u---~--:----:----:-:r--:----:---:--"':"""""---:---:---:----,

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 1.6 ·-..... Cl: ~ c: 1.4 0 ·-..... u 1.2 <!)

c <!)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·····-Station 2 ·••• Station 3 -- Station4

·-·-Station 5

-Station 1 --···Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·--··Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ·--Station 2 •••• Station 3 --Station 4

·-·-Station 5

Figure A. 7 0 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 7 (V5 of AC = 5000 fps (E

= 7 920 ksi) and V5 of base = 7 000 fps (E = 67 ksi))

63

Page 74: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

.9 1.6 ta ~ c:: 1.4 .9 -u ~ 1.2 ~

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi 1.6

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ··-·Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 - -Station 4

.•. ,;,Station 5

-Station 1 ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ,_, Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

Figure A.11 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 5000 fps (E = 1920 ksi) and V5 of base = 1500 fps (E = 152 ksi))

64

Page 75: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) V s of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ... -. Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 .... -Station 2 •••• Station 3 -- Station4

·••• Station 5

-Station 1 ... _.Station 2 ·••• Station 3 --Station 4

·-··Station 5

-Station 1 ... _Station 2 ·••• Station 3 --Station 4

····Station 5

Figure A.12 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 1 (V5 of AC = 5000 fps (E = 1920 ksi) and V5 of base = 2000 fps (E = 270 ksi))

Page 76: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

i .

. I

!

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) V s of Subgrade = 750 fps, E= 36 ksi

ol.S ·-..... Cl:l ~ 1.6 c .g 1.4 u ~ 1.2

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

Depth to Bedrock (ft)

-Station 1 ··-- Station 2 ····Station 3 ·-·Station 4 ··- ·· Station 5

-Station 1 --Station2 ····Station 3 • - . Station 4 ··-··Station 5

-Station 1 "--Station 2 ·--·Station3 • - · Station 4 ..... Station 5

-Station 1 .. -Station2 ····Station 3 • - · Station 4 ..... Station 5

Figure A.13 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 2000 fps (E

= 312 ksi) and V5 of base= 1000 fps (E = 67 ksi))

66

Page 77: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ··-·· Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-·- Station 1 ....... Station 2 ·~-- Station 3 --Station 4

·-·-Station 5

-Station 1 ·-- Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

Figure A.14 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 2000 fps (E

= 312 ksi) and V5 of base= 1500 fps (E = 152 ksi))

67

Page 78: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=l6 ksi

0 2.0 -3-·--+---i--.lo\·1-· ..... ~ 1.8

§ 1.6

·.g 1.4 0

~ 1.2

0 1.0 44~ffi14:rrn#~!;m*r;:~~~~~~~r:i:rr~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 1.8 ....,...-~-~~-""'l~~-.-~~-""'l"'"-~'""""'l'-~--:----,

~ '.. ; ·-~ 1.6 ~

§ 1.4 ·~ u ~ 1.2 0

0 1.0 fi~u{;

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 ·- 1.4 _. ~

~

= 0 1.2 ..... _. u 0

!;:;: 0

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ....... Station 2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 .. -Station2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 .. -Station2 ····Station 3 • -·Station 4 ..... Station 5

-Station 1 ·-··Station 2 ····Station 3 • - · Station 4 .••.. Station 5

Figure A.15 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 2000 fps (E

= 312 ksi) and V5 of base = 2000 fps (E = 2 70 ksi))

68

Page 79: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi 1.8-r--~--~--~--~.~~~--~--~--~--~--~~---.

0 ·.g 1.6 ~

§ 1.4 ·= u ~ 1.2 0

0 1.0

l '· .

~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

.0 ·.o ctl

1.6

~ 1.4 § ·-U1.2 0

t;: 0 Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 --"Station 2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 -Station2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 -Station2 ····Station 3 ·-·Station 4 ..... Station 5

-Station 1 ·-Station 2 ····Station 3 • - · Station 4 ..... Station 5

Figure A.16 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 2 (Vs of AC = 3000 fps (E = 690 ksi) and Vs of base = 1000 fps (E = 67 ksi))

69

Page 80: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 'i 1.6 ~

5 1.4 ·-tS ~ 1.2 -1---+--·

~ l.O~~=~~nJ#~~~~~~~~ 0 10 20 30 40 so 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi

·i l.6 --~===-==-,==·=-r::::::=.=--:;r=-=-=··1=[=/-;.~~\:;:r=-::...=71 =:::::;~=-=-=--::;,:::. =:::,;::.::.::.=-rr··=-=--=1··

~ 1.4 ' I j--/-J..:a---· . ____.,__, ____ _

J ::-~·--;.-_-:.. .... 1:._=_:-:_t=-:.f.;~( i-1- I -l +·--0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 so 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station! ··-- Station 2 ····Station 3 - ·Starion4

·-··Station 5

-Station 1 --- Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 -Station2 ····Station 3 - -Station4

·-·-Station 5

-Station 1 ·--··Station 2 •••• Station 3 --Station 4

·-·-Station 5

Figure A.17 Deflection ratio versus depth to bedrock for Dynoflect testing at Profile 2 (V5 of AC = 3000 fps (E

= 690 ksi) and V5 of bose = 1500 fps (E = 152 ksi))

Page 81: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

r -----------------~----~-~~--------~~-----

(a) Vs of Subgrade = 500 fps, E=16 ksi 2.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) V s of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Subgrade = 1000 fps. E= 63 ksi 1~~--~--~--~--~--~;-;~\~i--~--~--~--~--~--,

j V-1 I j ~ ;--t--.. ---1'···<~~--··--····,........_...,.·--+--

i .'1 I ii 1 1 1

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4

~ §1.2

~ <U

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -···Station 2 ····Station 3 • .. · Station 4 ··-·· Station 5

-Station 1 --Station2 ····Station 3 • - ·Station 4 ·····Station 5

-Station 1 -Station2 ····Station 3 ·- ·Station 4 ..... Station 5

-Station 1 -- Station 2 ····Station 3 • .. ·Station 4 •.••. Station 5

Figure A.18 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5

of AC = 3000 fps (E = 690 ksi) and V5 of base = 2000 fps (E = 270 ksi))

71

Page 82: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

--------------------~-~-

(a) Vs of Subgrade = 500 fps, E=16 ksi

2.0 0 'i 1.8 ~ = 1.6 0 '5 1.4

(I.)

~ 1.2 0

1.0 ..::w~~ri:n~~~~~~~~~~~~i=n=r=rf 0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

r: ~ }~i~R-l~r iii= = .1.2 ·---·--·;;-.t--7io-4,t···---···--·-------.. -·---·-··-· ~ 1.0 4ii,~-~1.;~?~.~~~~f:~:=~~~--~~-;-~~:'i' .. ..,.:~~.i~ .... ,. .. :J.~~~'~:.~"'··-~' ~~' ;=;:;:#1 ~~~ ~~i~~l~~

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs ofSubgrade = 1000 fps, E= 63 ksi

-Station 1 ··-·· Station 2 ····Station 3 --Station 4

·-··Station 5

-Station 1 ···- Station2 •••• Station 3 - ·Station4

.••• Station 5

-Station 1 -·- Station 2 • • • • Station 3 - -Station4

···-Station 5

Figure A.19 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 4000 fps (E = 1225 ksi) and V5 of base = 1000 fps (E = 67 ksi))

72

Page 83: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

0 W W ~ ~ ~ 00 M W (b) V s of Subgrade = 750 fps, E= 36 ksi

90 100 110 120

·~---!-!· ~·--: ---

! I I

0 w 20 30 ~ 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 ~ 50 00 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps. E= 142 ksi

0 1.4 ! '~· ! l' .: ·- ,,

'as -~ ., .:

Cl:: c: .9 1.2 -u <U = <U

0 1.0

0 10 20 30 ~ ~ 00 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 "-Starion2 ····Station 3 • - · Station 4 .,_,,Station 5

-Station 1 -Station2 ····Station 3 • - · Station 4 ·····Station 5

-Station 1 -Station2 •••· Station 3 • - · Station 4 ·····Station 5

-Station 1 ···-Station 2 ····Station 3 • - · Station 4 ..... Station 5

Figure A.20 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 4000 fps (E = 1225 ksi) and V5 of base= 1500 fps (E = 152 ksi))

73

Page 84: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

il.li!'

l

i•

·" I

I'.· 1'1

''I' 11'.1; ,,)!

l' '.1

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

i ::: ~ 1=-tllt IAA i= ~ 1.2 ____ ,_ ....... ..jt .. ,. .. ,...~.--.... --·--·•--<------.,._· ... --

~ 1~~~~~~-,~~~f~~;~,~--~~~!:¥:~~~~~~~~~~'~·~,~·-+'~~~fM~'~~~~~!~~!~;¥ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi

0 ~ j' .. ·.j ·-..... c=

" 1.4 c:: 0 ·-u1.2 Q)

~ Q)

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

1.4 i--i.---i 0

1 1 1 I ·: c=

" ~ ~ ~ c:: . I ~ f .g 1.2 ---·1·-·r--~---r--(,) Q) ~ ~ ~ ! ~ Q)

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ....... Station 2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 ·--Station 2 ····Station 3 ·-·Station 4 ..... Station 5

-Station 1 ·--Station 2 •••. Station 3 • - ·Station 4 ..... Station 5

-Station 1 ·-·- Station 2 ····Station 3 • - ·Station 4 ..... Station 5

Figure A.21 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5

of AC = 4000 fps (E

= 1225 ksi) and V5 of base= 2000 fps (E = 270 ksi))

74

Page 85: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

r: ~-r ~J~-~ =tH=H+ ~ 1.2 , _ _., __ ,_,....,.f..~.._A ... ,__ .. _ ... ___ ,__, ______ .... __ ,__ __

~ 1~~~~j~·;~:=~~~=~;~;:~··~:·~~~M\~,~~·~~?'~·~~~~~~~~~~~~~~~~~~~l~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·­... ~ ~ 1.4

§ ·-~ 1.2 ~ ~

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·-·- Station 2 ····Station 3 • - ·Station 4 .. _ .. Station 5

-Station 1 ....... Station 2 ····Station 3 ·-·Station 4 .. _ .. Station 5

-Station 1 ·- Station2 ····Station 3 • - · Station 4 .. _ .. Station 5

-Station 1 ·-· Station 2 .... Station 3 • - · Station 4 .. _ .. Station 5

""

Figure A.22 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 5000 fps (E

= 1920 ksi) and V5 of base = 1000 fps (E = 67 ksi))

75

Page 86: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

i

(a) Vs of Subgrade = 500 fps. E=16 ksi

0 10 20 30 40 so 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

: ~ ! ·g 1.6 .i.l--F~; ~- ·1--+--: -+-~ 1 ! ! /,1, \ I , ! I I I l c: 1.4 _ ___,.._.._t--t-·~ .. "'1-"'l..-...... +->--..,.___t __ -c .. --.,...__ .. ~~ .. - .....

~ :: 4~~~~.::.~:~:-".-.;~;-:~ .... ~f-.J.tt'i~n~'T:~f·r;··~i~.,.~i_~·~ ... !f;.l "'~' =n:~,~~-~-~-~~-~~~· ~~~~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

j !A ! ! J vJt j--J /··J t--g 1.2 ·-->···-;..-...;.-~-·-"'-·--·-·-,"->····---<-··-·<---------

~ 1n~~~~~·~·~::.~~~~:*~i-;;;t~=~~:: .. ~;;:: .. ·:·~~~~~-r;-'T·--T--·~;~~:,~~~l~:~~i~~~~~~~~~~~~~ 0 10 20 30 40 so 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 '"'"ti Station 2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 ohOdM Station 2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 ,._ Station2 ····Station 3 • - · Station 4 ..... Station 5

-Station 1 -Station2 ····Station 3 ·-·Station 4 ..... Station 5

Figure A.23 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 2 Ws of AC == 5000 fps (e == 1920 ksi) and Vs of base= 1500 fps (E = 152 ksi))

76

Page 87: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

~ :: =H=t~i +++-lit-as 1.2 -··-·-~--·-···~-..... ,. ~'"-· ....... _._, _____ ................... __ _

~ l.O~~~--~-!~~~~~~.~~~~:;:.;:.~~-~~~~n---~~-T .. ~I..n ... ~:~~~~~'~·~-~--~~~~~~~~~~~~~~~-~·~l~,~-~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Subgrade = 1000 fps, E= 63 ksi

0 "::I ~ 1.4

c 0 ·= (.) 1.2 d)

= d)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

1.4 0 .i ~ c

.9 1.2 ..... (.) d)

= d)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 """- S ration 2 ····Station 3 • - · Station 4 ··- .. Station 5

-Station 1 ···--Station 2 --··Station 3 • - ·Station 4 .. _ .. Station 5

-Station 1 "--Station 2 ····Station 3 • - · Station 4 ··-··Station 5

-Station 1 """""Station 2 ····Station 3 • - · Station 4 ··-··Station 5

Figure A.24 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 2 (V5 of AC = 5000 fps (E

= 1920 ksi) and V5 of base = 2000 fps (E = 270 ksi))

77

Page 88: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

1.8

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Subgrade = 1000 fps, E= 63 ksi

0 1.6

~ t: 1.4 0 ·= ~ 1.2 c;::: d)

0 1.0

-~-J--!-----~--~·-·.,·..:\.i ....... -... J ....... _-J~-··-; __ , ___ i~----i~ ......... -....

~lf~+H~+= 0 10 20 30 40 50 60 70 80 90 100 llO 120

(d) Vs of Subgrade = 1500 fps. E= 142 ksi

.5? 1.4 ... c=

c:z=: t: 0

·.:::: 1.2 ~ c;::: d)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 .. -.Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 -- Station4

·-·-Station 5

-Station! ·-·- Station 2 ··-· Station 3 -- Station4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 --Station 4

••.• Station 5

Figure A.25 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 CVs of AC = 2000 fps (E = 312 ksi) and Vs of base= 1000 fps (E = 67 ksi))

78

Page 89: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps. E=l6 ksi

0 2.0 ·g 1.8 ~ c 1.6 0 ·a 1.4 <U

~ 1.2

0 1.0 ..::w~~~~~~~~~~~n;;~~rri=r~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgi-ade = 750 fps. E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps. E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.sa 1.4 ... C':S ~ c 0

·::: 1.2 u (IJ = (IJ

0 1.0 .. 0 10 20 30 40 50 60 70 80 90 100 110 120

Depth to Bedrock (ft)

-Station 1 --··· Station 2 •••• Station 3 - -Station4

·-·-Station 5

-Station 1 ,,_, Station 2 ·••• Station 3 -- Sution4

·-··Station 5

-Station 1 ... _Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·-- Station 2 ·••• Station 3 --Station 4

·-·-Station 5

Figure A.26 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 (V5 of AC = 2000 fps (E = 312 ksi) and Vs of base= 1500 fps (E = 152 ksi))

79

1,,

Page 90: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

r

(a) Vs of Subgrade = 500 fps, E=16 ksi 2.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs ofSubgrade = 750 fps, E= 36 ksi

0 ·;::: 1.6

&a § 1.4 ·-ts ~ 1.2 (!,)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.!2 1.4 -c:l:l ~ c:

.!2 1.2 ts (!,) t;: (!,)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 IIO 120 Depth to Bedrock (ft)

-Station l -Station2 ·••• Station 3 -- Station4

····Station 5

-Station 1 --·Station 2 ·••• Station 3 -- Station4

·-·- Station 5

-Station 1 ....... Station 2 •••• Station 3 -- Station4

···-Station 5

-Station 1 ·K- Station 2 •••• Station 3 -- Station4

·-·-Station 5

Figure A.27 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 Ws of AC = 2000 fps (E = 312 ksi) and Vs of base= 2000 fps (E = 270 ksi))

80

Page 91: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(p) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 '70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 1.6~----~------~--~--~,-,~.~,~,--~--~--~----~--~~

! ,. ·~ ·­-!:a

" 1.4 .§ ~ 1.2 t;:; <I)

0 1.0 i~~Ji~llil+t= 0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 ' 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -··-Station 2 ·••• Station 3 - • Station4

····Station 5

-Station 1 --Station2 ·••• Station 3 -·Station 4

····Station 5

-Station 1 .... _ Station2 ·••• Station 3 - • Station 4

····Station 5

-Station 1 ··--· Station 2 ·••• Station 3 -- Station4

···-Station 5

Figure A.28 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 CVs of AC = 3000 fps (E = 690 ksi) and v, of base = 1000 fps (E = 67 ksi))

81

I I

Page 92: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

Depth to Bedrock (ft)

-Station 1 -Station2 ····Station 3 -- Station4

···-Station 5

-Station 1 ~-~Station 2 ·••• Station 3 -·Station 4

····Station 5

-Station 1 --Station 2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 ·-- Station 2 •••• Station 3 -- Station4

·-·-Station 5

Figure A.29 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 (V5

of AC = 3000 fps (E

= 690 ksi) and V5 of base = 1500 fps (E = 152 ksi))

82

Page 93: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

~~~-~~~~~-~~~-

(a) Vs of Subgrade = 500 fpst E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps. E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 -~ e:::: 1.4 s:: .9 ~ 1.2

1;:1 IU

Q 1.0

0 10 20 30 40 50 60 70

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.s 1.4 ..... ~

e:::: s:: .9 1.2 ..... (.) IU

1;:1 IU

Q 1.0

0 10 20 30 40 50 60 70

80

80 Depth to Bedrock (ft)

90 100 110 120

90 100 110 120

-Station 1 ....... station2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 -Station2 ····Station 3 --Station 4

·-·-Station 5

-Station l - .. Star:ion2 ····Station 3 --Station 4

·-·-Station 5

-Station! ·····-Station2 ····Station 3 --Station 4

·-·-Station 5

Figure A.30 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 (V5 of AC = 3000 fps (E = 690 ksi) and V5 of base = 2000 fps (E = 270 ksi))

83

Page 94: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = SOO fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·-Cii p::: 1.4

s::: 0 ·-t) 1.2 <U

r:+:: <U

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = lSOO fps, 142 ksi

0 1.4 -~ p::: s::: .sn.z .... (.) <U

r:+:: <U

0 1.0

0 10 20 30 40 50 60 70 80 90 100 llO 120

Depth to Bedrock (ft)

-Station 1 •H-· Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 -- Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ··--··Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 •••• Station 3 --Station 4

·-·- Station 5

Figure A.31 Deflection ·ratio versus depth to bedrock for Dynaflect testing at Profile 3 (Vs of AC = 4000 fps (E

= 1225 ksi) and Vs of base = 1000 fps (E = 67 ksi))

84

Page 95: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

.9 ~ 1.4 c: 0 ·-y1.2

!;:: 4.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 1.4 .i ~ c: .9 1.2 y !;:: 4.)

O l.O~~~~~~~~;;;~ffi 0 10 20 30 40 50 60 70 80 90 100 110 120

Depth to Bedrock (ft)

-Station 1 -·Station2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 ....... Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·- Station2 •••• Station 3 -- Station4

···-Station 5

-Station 1 ....... Station 2 ·••• Station 3 - - Station 4 ·

···-Station 5

Figure A.32 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 (V5 of AC = 4000 fps (E = 1225 ksi) and Vs of base = 1500 fps (E = 152 ksi))

85

Page 96: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 1.8 *i ~ 1.6 c: .9 1.4 -u ~ 1.2 0

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0

~ 1.4

c: 0 ·g 1.2 0 c 0

Q 1.0

0 10 20 30 40 50 60 70

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

1.4 0 ·-(ii ~ c: .9 1.2 -u

0 '+= 0

Q 1.0

0 10 20 30 40 50 60 70

80

80 Depth to Bedrock (ft)

90 100 110 120

90 100 110 120

-Station 1 --Station2 ····Station 3 -- Station4

•••• Station 5

-Station 1 ._ ... Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·-Station2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 --Station 2 •••• Station 3 -- Station4

···-Station 5

Figure A.33 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 CVs of AC = 4000 fps (E

= 1225 ksi) and Vs of base = 2000 fps (E = 270 ksi))

86

Page 97: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=l6 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

: : 4 : : : : :

'' ·~' .... * .. ~'"'" 'n~•~~~••• ·~~•• •••• •••~ •••••••·-- •'

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi 1.4

0 ·~ ~ s:::

1.2 0 ·-..... u Cl.)

!;::: Cl.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ··-· Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ····-Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 --Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 2 •••• Station 3 -- Station4

·- ·- Station 5

Figure A.34 Deflection ratio versus depth to bedrock for Dynoflect testing at Profile 3 (Vs of AC = 5000 fps (E = 1920 ksi) and Vs of bose = 1000 fps (E = 67 ksi))

87

Page 98: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

------------------···---·····-

(a) Vs of Subgrade = 500 fps, E=16 ksi

0 1.8 ·-...... ca ~ 1.6 c .9 1.4 .... 0 <1.)

t;:; 1.2 <1.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

.9 1.6 ...... ca ~ c 1.4 0 ·-...... as 1.2

t;:; <1.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 llO 120

(c) V s of Subgrade = 1000 fps, E= 63 ksi

.9 ...... 1.4 ca ~ c 0 .fi 1.2 <1.)

t;:; <1.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi 1.4-r-~-~--------~--~--~--~--~~-~~.,~\~l~--------~

• •t /! ~

, i - , : / y '~

--:··~ttl~~J=if~Etr·r·-0 10 20 30 40 50 60 70 80 90 100 110 120

Depth to Bedrock (ft)

-Station 1 -"" Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ... _Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 --Station2 .... Station 3 -- Station4

·-·-Station 5

-Station 1 ···-·· Station 2 ·••• Station 3 - -Station4

·-·-Station 5

Figure A.35 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 3 (Vs of AC = 5000 fps (E = 1920 ksi) and Vs of base= 1500 fps (E = 152 ksi))

88

I 1:':

Page 99: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E=l6 ksi

.9 1.8

. ~ 1.6 c .9 1.4 t) ~ 1.2 Q)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -· .. - Station 2 ·•• • Station 3 - - Station 4

····Station 5

-Station 1 - .. Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station I ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 -····Station 2 •• • • Station 3 -- Station4

·-·-Station 5

Figure A.36 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 3 (Vs of AC = 5000 fps (E = 1920 ksi) and Vs of base = 2000 fps (E = 270 ksi))

89

Page 100: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

- -------------------

(a) Vs of Subgrade = 500 fps, E= 16 ksi

0 2.6 ·= 2.4 ~ 2.2 c: 2.0 .9 1.8 u 1.6 ~ 1.4 ~ 1.2

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi .,

0 ·= 1.6 ~

~ § 1.4 ·-... u ~ 1.2 ~

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

.9 1.4 -~

~ c: 0 'fi 1.2 ~

t;:: ~

Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ···-·Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ····-Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ·---Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ... _.Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

Figure A.37 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 4 (V5

of AC = 2000 fps (E

= 312 ksi) and V5 of base = 1000 fps (E = 67 ksi))

90

Page 101: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi 2.8

0 2.6 ·= 2.4 ~2.2 s:: 2.0 .9 1.8 t) 1.6 ~ 1.4 v 1.2 0 1.0

0 10 20 30 40 50 60 70 80

(b) Vs ofSubgrade = 750 fps, E= 36 ksi

0 'E 1.6 ~ s 1.4 ·-... (.}

~ 1.2

8 1.0

0 10 20 30 40 50 60 70 80

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

.9 .... ~1.4 s:: 0

'B 1.2 v I;: v 0 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.9 .... d

c:c:: 1.2 s:: .9 .... (.} v

!;::

8 1.0

0 10 20 30 40 50 60 70 80 Depth to Bedrock (ft)

90 100 110

90 100 110

90 100 110

90 100 110

120

120

120

120

-Station 1 """" Station 2 ···• Station 3 - - Station 4

····Station 5

-Station 1 -- Station 2 •••• Station 3 ;. - Station 4

·-·-Station 5

-Station 1 -Station 2 .••• Station 3 - - Station 4

·- ·- Station 5

-Station 1 "'- Station 2 ·••• Station 3 - - Station 4

·-·-Station 5

Figure A.38 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5

of AC = 2000 fps (E = 312 ksi) and Vs of base= 1500 fps (E = 152 ksi))

91

Page 102: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi

2.8 .9 2.6 ~ 2.4 ~ 2.2 s::: 2.0 .g 1.8 g 1.6

tC 1.4 v 1.2 0 1.0

0 10 20 30 40 50 60 70 80

(b) Vs of Subgrade = 750 fps, E= 36 ksi 1.8

0 ·-:: 1.6 ~

su ·-...... g tC 1.2 v 0 1.0

0 10 20 30 40 50 60 70 80

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·-...... C!;f ~ 1.4 s::: 0 ·-0 1.2 ~

tC ~

Cl 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 -~

~ 1.2 s::: .9 ...... (.) ~

tC ll.)

0 1.0

0 10 20 30 40 50 60 70 80 Depth to Bedrock (ft)

90 100 110

90 100 110

90 100 110

90 100 110

120

120

120

120

-Station 1 .. _ Station2 •••• Station 3 --Station 4

·-··Station 5

-Station 1 ···-· Station 2 •••• Station 3 --Station 4

·-··Station 5

-Station 1 ·-"" Station 2 •••• Station 3 --Station 4

·-·· Station 5

-Station 1 - ... Station 2 ·••• Station 3 - - Station 4

·-·-Station 5

Figure A.39 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (Vs of AC = 2000 fps (E = 312 ksi) and Vs of base = 2000 fps (E = 270 ksi))

Page 103: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

r·· I !

(a) Vs of Subgrade = 500 fps, E= 16 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 10 20 30 40 50 60 70 80 90 100 llO 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 .i 1.4 ~ c 0 ·g 1.2 <1.)

t;:

~ 1.0 ~~~T:rrT~i"i:mrriTi::ffi:T~~Frn=i'Mffi:n~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 ·-~ 1.2 c 0

·~ t;:

<1.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -·· Station2 •••• Station 3 - • Station4

····Station 5

-Station 1 ·······Station 2 ·••• Station 3 -·Station 4

·-··Station 5

-Station 1 ··-- Station 2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 -- Station2 ····Station 3 -- Station4

·-·-Station 5

figure A.40 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (Vs of AC = 3000 fps (E

= 6 and V1 of base = 1000 fps (E = 67 ksi))

93

Page 104: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

2.8 .9 2.6 (a 2.4 ~ 2.2 c: 2.0 .9 1.8 ~ 1.6 ~ 1.4 G) 1.2 0 1.0

0 10 20 30 40 50 60 70

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 ·~ 1.6 ~

§ 1.4 ·-.... (.) G) 1.2 ~ G)

0 1.0

0 10 20 30 40 50 60 70

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

80 90 100 110 120

80 90 100 110 120

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·····-Station 2 .••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·······Station 2 .••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ·---Station 2 ·••• Station 3 - -Station 4

·-·-Station 5

-Station 1 -··-·Station 2 ·••• Station 3 --Station 4

·-·-Station 5

Figure A.41 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5

of AC = 3000 fps (E

= 690 ksi) and V5 of base= 1500 fps (E = 152 ksi))

94

~~~- --- - ~-

Page 105: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

0 10 20 30 40 so 60 70 80

(b) V s of Subgrade = 750 fps, E= 36 ksi 1.8

0 ·-= 1.6 ~ c .sa 1.4 ...... Q

~ 1.2 (I)

Q 1.0

0 10 20 30 40 50 60 70 80

(c) V s of Sub grade = 1000 fps, E= 63 ksi

0 ·~ ~ 1A c .sa gl.2 = (I)

Q 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

"'""'· 0 _,·; '. *i c::: c 1.2 .9 -Q (I) = (I)

Q 1.0

0 10 20 30 40 50 60 70 80 Depth to Bedrock (ft)

90 100 110

90 100 110

90 100 110

90 100 110

120

120

120

120

-Station 1 "-' Station 2 •••• Station 3 - - Station 4

·-·-Station 5

-Station 1 ·-·-Station 2 •••• Station 3 - - S ration 4

···-Station 5

-Station 1 ·-Station2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 ....... Station 1 . • • • Station 3 - -Station4 ···- Station 5

Figure A.42 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 <Vs of AC = 3000 fps (E = 690 ksi) and Vs of base= 2000 fps (E = 270 ksi))

95

Page 106: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi 2.8 ----~-~--~-~~---;---~--~---:---...,

0 2.6 ·~ 2.4 ~ 2.2 ::::: 2.0 .9 1.8 t) 1.6 ~ 1.4 ~ 1.2

0 1.0 ~~;:;;:;:;:;:;:;;:;:t;~;;:;::;~;;;:;::;:;:;:i;;;=;:;:;:;~=#;:~~ 0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 ·~ 1.6

" .§ 1.4 -0 ~ 1.2

Q 1.0 -1;::;~~i::riTi~~~~~~~~~~;=;J 0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

.9 ... Q2 1.2 ::::: .9 -0 ~

l+:::: ~

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 .. -Station 2 •••• Station 3 --Station 4

····Station 5

-Station 1 .. _, Station 2 •••• Station 3 -- Station4

···-Station 5

-Station 1 -Station2 .... Station3 --Station 4

·-·-Station 5

-Station 1 .. _, Station 2 •••• Station 3 --Station 4

···-Station 5

Figure A.43 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5 of AC = 4000 fps (E = 7 225 ksi) and V5 of base = 7 000 fps (E = 67 ksi))

96

Page 107: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

. il ';'·I

·i i

I

(a) Vs of Subgrade = 500 fps, E= 16 ksi 2.8

.53 2.6 ~ 2.4 ,:::: 2.2 c: 2.0

.53 1.8 ~ 1.6 c 1.4 <0 1.2

Q 1.0

0 10 20 30 40 50 60 70 80

(b) Vs of Subgrade = 750 fps, E= 36 ksi 1.8

0 ·-~ 1.6 ,:::: § 1.4 ·-..... u <0 1.2 c <0

Q 1.0

0 10 20 30 40 50 60 70 80

(c) Vs of Subgrade = 1000 fps. E= 63 ksi

.53 ..... ~

,:::: 1.4 c: 0

-~ 1.2 c <0

Q 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps. E= 142 ksi ,._ ".

,. ! \ ,. : \.

90 100 110 120

90 100 110 120

90 100 110 120

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 -·"• Station 2 •••• Station 3 -·Station 4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 - • Station 4

·-··Station 5

-Station 1 .. -Station 2 •••• Station 3 - - Station 4

·-·· Station 5

-Station 1 ···-· Station 2 ·••• Station 3 --Station 4

• • • • Station 5

Figure A.44 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5 of AC = 4000 fps (E = 1225 ksi) and V5 of base= 1500 fps (E = 152 ksi))

97

Page 108: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi

0 2.8 ·- 2.6 = 2.4 ~ 2.2 c:: 2.0 .9 1.8 ~ 1.6

t;:;: 1.4 C!Jl.2 0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi 1.8

.9 ~ 1.6 c:: .9 1.4 .... u

Cl.) 1.2 t;:;: Cl.)

0 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) Vs of Subgrade = 1000 fps, E= 63 ksi 1.6

0 ·~ ~1.4 c:: .9 .... ~1.2

t;:;:

~ 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ..... "Station 2 ····Station 3 - -Station4

• -·- Station 5

-Station 1 -·Station2 .••• Station 3 - ·Station 4

····Station 5

-Station 1 -Station 2 ····Station 3 -- Station4

·-·-Station 5

-Station 1 "-" Station 2 ·••• Station 3 -·Station 4

···-Station 5

Figure A.45 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 4 (V5 of AC = 4000 fps (E = 1225 ksi) and V5 of base = 2000 fps (E = 270 ksi))

Page 109: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi

2.8 0 2.6 ·g 2.4

t:z:: 2.2 c 2.0 .2 1.8 u 1.6 ~ 1.4 ~1.2 0 1.0

0 10 20 30 40 50 60 70

(b) Vs of Subgrade = 750 fps, E= 36 ksi

0 ·g 1.6 t:z:: § 1.4 ·-..... (,)

~ 1.2 !i: ~

0 1.0

0 10 20 30 40 50 60 70

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·-~ 1.4 c 0 ·-u 1.2 ~

!:;::;: ~

0 1.0

0 10 20 30 40 50 60 70

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 ·-~1.2 c 0 ·.:::: (,) ~

!:;::;: ~

0 1.0

80 90 100 110 120

80 90 100 110 120

80 90 100 110 120

0 10 20 30 40 50 60 70 80 90 100 110 120 ~ Depth to Bedrock (ft)

-Station 1 ···-Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ·······Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ..... "Station 2 .••• Station 3 - -Station 4

·-·-Station 5

-Station 1 ·-··· Station 2 .••• Station 3 - -Station 4

.••• Station 5

Figure A.46 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5 of AC = 5000 fps (E = 1920 ksi) and V5 of base = 1000 fps (E = 67 ksi))

99

Page 110: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi

2.8 .9 2.6 CiS 2.4 ~ 2.2 = 2.0 .9 1.8 ~ 1.6 l:l::::l.4 «.) 1.2 0 1.0

0 10 20 30 40 50 60 70 80

(b) Vs of Subgrade = 750 fps, E= 36 ksi

1.8 0 ·-CiS 16 ~·

5 1.4 ·-~ t:;::::; 1.2 «.)

0 1.0

0 10 20 30 40 50 60 70 80

(c) Vs of Subgrade = 1000 fps, E= 63 ksi

0 ·-CiS ~1.4

= 0 ·--g 1.2 l:l:::: u 0 1.0

0 10 20 30 40 50 60 70 80

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 ·-CiS ~ 1.2 = 0 ·--(..) «.)

l:l:::: 41.)

0 1.0

0 10 20 30 40 50 60 70 80 Depth to Bedrock (ft)

90 100 110

90 100 110

90 100 110

90 100 110

120

120

120

120

-Station 1 -Station2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 "-·· Station 2 •••• Station 3 - - Station 4

····Station 5

-Station 1 -- Station 2 •••• Station 3 - - Station 4

·-·-Station 5

-Station 1 ··-" Station 2 ·••• Station 3 - - Station 4

·-·-Station 5

Figure A.47 Deflection ratio versus depth to bedrock for Dynaflect testing at Profile 4 (V5

of AC = 5000 fps (E

= 1920 ksi) and V5 of base = 15 00 fps (E = 152 ksi))

100

Page 111: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps, E= 16 ksi

0 2.8 -lil······-,···i-·······+··~-t---···t····--·1··········1···-·····]··········t·-··+--···1··········]··········· ~ t.~ ·:::r-:=r=:::::::L=J=:::r::::::::r:::::::::c:::····c~::::J:::::::::

2.2 ~-t-•-•"••t--•••-i••••n•-·+•••••••••t--•--•••+u-.-•ninn•nn•i-·-i--•u•~• .g i:~ .. ·:L.:: ... .L.- ; _____ ::J:::::-.::r:::::::r:::::::c::::::I::::::r:::: 16 : : : : : : : ; : a:s · ·- ·y---r--·-r······-r··--·-r·-··-··r······-T-····r········r····-···

~+:: 1.4 , ··-- ···--,--·-·,-·r·--r····-·r····-·r·-··1··········1········-.,., 1.2 ···r-- ··-··'!'····-·-·!··-·-:---·-··1--~···-~!-·--:---·····

Q 1.0 ; : __ ; _ __:_ : ........ ...i-....... l---·-'-·----1---···-

0 10 20 30 40 50 60 70 80 90 100 110 120

(b) Vs of Subgrade = 750 fps, E= 36 ksi

:I~~l=+::~~~r~~f ... :::··l~~:~r:::~:~~:=:: ~ ~ ~ ~ ~ l ~

........... ~--i·----i ............. l,. .............. .._~.~-···--i .............. -J .............. _ .. ..

~ ~ 1 I 1 1 l I

0 10 20 30 40 50 60 70 80 90 100 110 120

(c) V s of Sub grade = 1000 fps, E= 63 ksi 1.6

0 ·-~ ~ 1.4 c 0 ..... ..... g 1.2

!+:: .,., Q 1.0

0 10 20 30 40 50 60 70 80 90 100 110 120

(d) Vs of Subgrade = 1500 fps, E= 142 ksi

0 10 20 30 40 50 60 70 80 90 100 110 120 Depth to Bedrock (ft)

-Station 1 ·······Station 2 •••• Station 3 --Station 4

·-·-Station 5

-Station 1 -Station2 •••• Station 3 -- Station4

·-·-Station 5

-Station 1 ....... Station 2 ·••• Station 3 --Station 4

·-·-Station 5

-Station 1 ···-Station 2 •••• Station 3 -- Station4

·-·- Station 5

Figure A.48 Deflection ratio versus depth to bedrock for Dynaf/ect testing at Profile 4 (V5 of AC = 5000 fps (E = 1920 ksi) and V5 of base = 2000 fps (E = 270 ksi))

101

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102

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APPENDIX B. RESULTS OF ANALYTICAL SIMULATION OF THE FWD TEST

The analytical simulations of the FWD test were obtained using computer program UTFWD (Chang, 1991). The motions are expressed in terms of deflection ratios as a function of depth to bedrock, a format similar to that used for the Dynaflect test in Appendix A.

There are some numerical problems with the deflection ratios obtained from shallow bedrock depths (less than 10 feet (3.1 m)). These problems caused the first pulses in the deflection-time records to be distorted, so that the maximum de­flections were incorrect as discussed in Section 4.7.

However, for unsaturated subgrade conditions, numerical problems did not have any effect on the values of the maximum deflection ratios and the resonant depths to bedrock. They had no effect because numerical problems always occurred at shallower bedrock depths than the resonant depths obtained with unsaturated subgrade conditions, as

103

shown in Figure B.l. The maximum deflection ra­tios and the resonant depths to bedrock can be determined without difficulties, as shown in Fig­ures B.2 to B.S (the data generated by numerical problems were removed from these figures).

For saturated subgrade conditions, the numeri­cal problems tend to occur at greater depths than those for the unsaturated subgrade conditions, as shown in Figure B.6. Generally, the measurement stations away from the source (stations 5, 6, and 7) exhibit the poorest results. Therefore, the reso­nant depths to bedrock were determined from the bedrock depths corresponding to the maximum deflection ratios of the first three measurement stations (stations 1, 2, and 3). The values of the maximum deflection ratios of the farthest station (station 7) were estimated based on the trends of the deflection ratios of the stations which were not affected by the numerical problems.

Page 114: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

2.s -l.L..-=.J----~.r.....;___._~_.....__ ______ -, Numerical Problems at Shallow Depths to Bedrock

0 1 0 20 30 40 so 60 70 80 90 Depth to Bedrock ( ft)

-+- Station 1 -m- Station 2 -x- Station 3 ~ Station4 ....,._Station 5 -0- Station 6 -x- Station 7

Figure B. 7 Numerical problems with UTFWD program at shallow depths to bedrock for unsaturated subgrade

conditions (Profile 7 with V5 of subgrade = 7 000 fps (E = 63 ksi))

Numerical Problems at Shallow

~ 25 -H~·t··~·----+'--D~e_p __ ths~ro __ B_~~-k~--~--~~··i 6 ·-~ 2.0~·--~~~-~~-----~·~···--·--~---l···--~·---·-~····-~ 0

o w w ~ ~ ~ ro m w w Depth to Bedrock (ft)

-+- Station 1 -f:B- Station2 -x- Station3 ~Station4 ....,._StationS -0- Station 6 -x- Station 7

Figure 8.2 Numerical problems with UTFWD program at shallow depths to bedrock for saturated subgrade

conditions (Profile 7 with Vs of subgrade = 1000 fps (E = 63 ksi))

Page 115: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps (E= 16 k.si) 3.0 -r;:~::::::;.:==;==:::;::::=::::;==::::;==::;:::::=::;::::=::;::::::::==.,

0 10 20 30 40 so 70 80 90

(b) V s of Subgrade = 750 fps JE= 36 ksi) 3.0 - ~·· ........... :···-·-·-···! ....... --.... ~·-··-·······"!"·"'"'"-'" t,........ -·······--··-¥·--"-""'"00

"'t'00'""•••···· .. -·.

0 . . . : . i i i i i

~~~~-u.ml§ 0

o.s _ L·-··-··J··-·····-···L ............ L_ .......... l ..... --..l··-····--·l········-··-l ......... -. .1 ........... _.! I I I I I I I I I I 0 10 20 30 40 so 60 70 80 90

(c) V s of Sub grade = 1000 fps (E= 63 k.si) 3.0

0 "i 2.S ~ c 2.0 0

"E t.s 4)

l:i:::: 4) 1.0 0 o.s

0 10 20 30 40 50 60 70 80 90

(d) Vs of Subgrade = 1500 fps (E= 142 k.si)

-+-Swi.on 1 -s-Swi.on2 -x-Swi.on3 ..._S£a.tion4 -~E-Swi.on5 -a- Swi.on6 -z-Swi.on 7

-+-Station 1 -s-Swion 2 ""*- Station 3 ..._Station4 -11- SEa.tion S -&- SEa.tion 6 -z- S~a.tion 7

-+-Swi.on 1 -s-Swi.on2 ""*- Swi.on 3 -B-Swi.on4 -11-Swi.onS -&- Swi.on6 -x-Swi.on7

-+-Swion 1 -a- Station 2 -x- SEa.tion 3 ...... si:Ui.on4 -11-StationS -a- Swi.on6 -z- S~a.tion 7

Figure 8.3 Deflection ratio versus depth to bedrock for FWD tests at Profile 1 with unsaturated subgrade conditions

105

Page 116: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps (&:: 16 ksi)

Q l :· l l l ; : : I I : I I I : o.s - J..-.l.------l·-·--··-L----.i.··--·····-~·--·.......l····---·L ............. L.--·····1

I 0

I 10

I 20

I 30

I 40

l 50

(b) Vs of Subgrade = 750 fps (E= 36 ksi)

I 60

(c) Vs of Subgrade = 1000 fps (E= 63 ksi)

I 70

I 80

I 90

o 3'0 -r;::=:::::::;:==;==;:::::::=:;==:;r=·===~;::· =-::::....=-:;:j =··-=---:::::::;:. i =-=·-=;'11 "i 2.5 .._ ___ , ____ , ___ _..._,., ...... ____ ~----l-·-··--..i...-.-i ....... - ... l

~ ! l l ! ! ! 1 1 ! !

i ~ r-~ .. ~.:r~.--J.-··;-.F.J.J 0 o.s L_ i ..l.-.. J. ___ J_ .. ___ _.l _____ .....l ______ L ....... J. ___ J

0 10 20 40 50 60 70 80 90

(d) Vs of Subgrade = 1500 fps (E= 142 ksi)

~ ~ = F--i -t-·-·--·1---··-t·--+··-·---·1-- : ·--+-···--·1 c 2.0- ---.. -·--·-·-·<-----·--·----.. ·----·--·-<-- -·: .9 i i l i [ j j i l i

j :~ -r-fll 'II I' iiI' Ill' II if.i I' .u r.;;~ 0.5-..!........ : - '· : ............ ,!.___ : ••• :.. .. : .............. :

I I I I I I I 1 I I o 10 m ~ 40 ~ 60 w w ~

Depth to bedrock (ft)

-+- Station 1 -s-Station2 ...x- Station 3 ..... station4 ...._StationS -e- Station6 -x- Station 7

-+- Station 1 -s-Station2 ...x- Station 3 ..... station4 ...._StationS -e- Station 6 -x- Station 7

-+- Station 1 -s-Station2 ...x- Station 3 -e-Station4 ...._StationS -e-Station6 -x- Station 7

-+-Station 1 -m-Station2 ...x- Station 3 -e-Station4 -11-Station 5 -e- Station 6 -x- Station 7

Figure 8.4 Deflection ratio versus depth to bedrock for FWD tests at Profile 2 with unsaturated subgrade conditions

Page 117: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fp:~ (E= 19 ksi)

0 10 20 30 40 50 60 70 80 w

(b) Vs of Subgrade = 750 fps (E= 42 ksi)

0.5 - --····· - ... ,. - ... .;. .. -.. .. ....... -......... ·--····- ···.:--·-·-·.;.----··-: I I I I I I I I I I o ro 20 ~ 40 50 60 w w w

(c) Vs Qf Subgrade = 1000 fps (E= 75 ksi) 3.0

0 ·~ 2.5 ~ = 2.0 0 ·~ 1.5 ti=:

<!..) 1.0 Cl

0.5

0

~

•••• ~ -..... I

10 20 30 40 50 60

(d) Vs ofSubgrade = 1500 fps (E= 168 ksi)

70 80 90

0 3.o r, --.:. --1,----··--_,.· --···;,··--_,.-- ·.,.-······-·-.--...,

~ ~ ~ ·~ 2.5 .L............l---i·-·-··L--l··-·········i---·'··---.i.-.--...;.·-···--·1 ~ ! ! l ! -! l ! ! ! ! c 2.0 <----- .., _____ _.. __ , _ _,_,._,__ ·-:

j :~ i ·- fi1fmfuifiiifii-FFF1 0.5 ~·--·-~--... ~ .. --...;.. ___ _.;. ........ _ ...... _. ---·: .. ---·--· --·-·-~·

0 10 20 30 40 50 60 Depth to bedrock (ft)

70 80 90

-+- Station 1 -m- Station 2 ->G- Station 3 -e-Station4 ....... stationS -a- Station 6 -:z:- Station 7

-+- Station 1 -m- Station 2 -x- Station 3 -e-Station4 ....,_StationS -a- Station 6 -:z:- Station 7

-+- Station 1 -m- Station 2 -x- Station 3 ..... station4 ....,_StationS -a- Station 6 -z- Station 7

-+- Station 1 -m- Station 2 -x- Station 3 ..._Station4 ....... stationS -a- Station 6 -z:- Station 7

Figure 8.5 Deflection ratio versus depth to bedrock for FWD tests at Profile 3 with unsaturated subgrade conditions

107

Page 118: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps (E= 16 ksi) 2 .. 0 - ;-····-~.............. ·~· ......... ~---- ···-r-· " r····- -·- .. ,... .._ ....... ,..-.... u .... ~--.

0 ; : : ; l : . ; i ;

; ::~~;i~!~t~tl~i~ ~ 0.8 - ' ' ---... 1 I I I i1 • .................. ' ...... ; ................ "-·-· ···-'·· ..... : o L. . .... .L .......... ..! ................ L........ ~--~ .. !.:!.! .. ~ ~ .. ~.!.!.! ... !.l~-~-~ .. ! .. ~ .. ~-~-'

: : : : : : : : : : I 0

I 10

I 20

I 30

I 40

I 50

(b) Vs of Subgrade = 750 fps (E= 36 ksi)

I 60

I 70

I 80

I 90

2.0 - r. -··---··~=. ....... ·-,! ......... .,.. ·-·"v _ .. _,..... ....---.--.. -.,.......... ·····:·---.............. : 0 : ' . . ; l ; i : : ·a r--·---r .. - .................. r·--·-·· .. 1···-·----1----···---E·--·---·-··~-····-~-·-··r········ .. -·-r· ............ _ ....... ~ ~ 1.6 - +--···-·...f--··-····1-········-+·········-...f·····-·····f···-··--··+·--····+-······..f-······-·-·i

·~ 1.2 -~=-1t6;t:=:t==···t:::::=+:=:===~=:::::::t::::::::::::1:::::::::::::j ~ • t••••••~ •• i ....... : unm••+-• •••!••moo ••+ •••u : ••n•••••l

~ 0.8 - ~ ~ ..... +--- ·j --~-~ ·~.!.~ .. !..!.!.~.! .. !I! .. !I! .. ;.J. . .l.l:.~:l.:l.:l.; 0

fl t·-•-••••f•--•--•-t.,,.,...,,.,.,.,._.~•t•••"""'"'"''"""'"'"f•••••••w•••-·f'""'"'"'"'"'"""'"'"""'"~'""--"~••••••f••••n•~...,~·~•~n~~·•u•«n•o;•"1 I 0

I 10

I 20

I 30

I 40

I 50

I 60

(c) Vs of Subgrade = 1000 fps (E= 63 ksi)

I 70

I 80

I 90

2.0 - . -:-·· -····-:: . . ·--.,-·-···- . ..,. ............ ....,

j::~~m~ 0 0.8 ~r:=r~==l==~r.::=t=l==l==r-:::::r.:::=~

I I I I I I I I I I 0 10 20 30 40 50 60 70 80 90

(d) Vs of Subgrade = 1500 fps (E= 142 ksi)

0 ·-ta ~ ~~~+----~-----~-·--+·--····~·-·-·--·4--··-·~---··-~··········-<•······--···l

·i 1.2-+----t-~............. ...... .., ~ 0.8-H-----~--~---~--~----+-·--~----···~··--·····-~~-·····--~~

0 .10 I I I

30 40 50 60 Depth to bedrock (ft)

70 80

l I

90

......j- Station 1 -e- Station 2 ~Station3 _...Station4 _... Station 5 -&- Station 6 -x- Station 7

......j- Station 1 -e- Station 2 -x- Station 3 ..... station4 _..StationS -&- Station 6 -x- Station 7

......j- Station 1 -e- Station 2 -*" Station 3 ..... station4 _... Station 5 -&- Station 6 ~Station?

......j- Station 1 -e- Station 2 ~Station3 ..... station4 _... Station 5 -&- Station 6 -z- Station 7

Figure 8.6 Deflection ratio versus depth to bedrock for FWD tests at Profile 4 with unsaturated subgrode conditions

108

Page 119: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

(a) Vs of Subgrade = 500 fps (E= 18 ksi)

o 1.0-t--- . liiiiiiiiiMIIItllllli·;·· i•••••••••••-•t•••••-••••••.i•-•••••-••••L•••••••••••••l••••••••••••••tu••••••••••••~••••••••••••••l.••••••••••••••t•••••••••••••.; I T T I I I I I I T 0 10 20 30 40 50 60 70 80 90

(b) Vs of Subgrade = 750 fps(E= 40 ksi)

·! ::~R=ft=T=+=l=P=~~ j:~E~~~~~~~

1. .................. l .......... _ ........ i .................. i ... _ ............ l .................. ~ .................. i .................. i .............. .t ................ ; I I I I I I I l I I 0 10 20 30 40 50 60 70 80 90

(c) V s of Sub grade = 1000 fps (E= 70 ksi) 4·0 - • ·· ·-·-r··--··-··-r··-··-· ·T ··-·····r·····-···-1-············r············r·············l

l:~~~fm~ ~ 1.0 _ r-- saslnnri-.fiilflillM.-.' t··· -·····t·····-·······:····-········f-···········t···········:··:··············j··············t·············t··············j 0 10 20 30 40 50 60 70 80 90

(d) Vs of Subgrade = 1500 fps (E= 155 ksi) 4.o - : -· ·: ······-··:· ··--····:-· T... --r-···-·····r-···-······T·········-··l

·: '~-t±=F._Lt-t-=:=i=1~Ej ~ ~::1--Jmim~~ii.t.~

l,.,.,.,.,.,.,.,.,.,. .. ,..i_.,,..,,.,.,. ___ f_,.,.,._,..,.,,._,.i •••• n•••••••i•-••••-••••j••••••••••••••i••••••'"•'"•••••l•••••••••••••l••••••••••••••~ I 0

I 10

I 20

I I I I 30 40 50 60 Depth to bedrock (ft)

I 70

I 80

I 90

-+-Station 1 -s- Station 2 -x- Station 3 -B- Station 4 -i1-Station5 -a- Station 6 -z- Station 7

-+-Station 1 -s- Station 2 -x- Station 3 -B- Station 4 -II- Station 5 -a- Station 6 -z- Station 7

-+- Station 1 -s- Station 2 ->e- Station 3 -B- Station 4 -il-Station5 -a- Station 6 -z- Station 7

-+- Station 1 -s- Station 2 ->e- Station 3 -B- Station 4 -il-Station5 -a- Station 6 -:r- Station 7

Figure 8.7 Deflection ratio versus depth to bedrock for FWD tests at Profile 1 with saturated subgrade conditions

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i i

(a) Vs of Subgrade = 500 fps (E= 18 ksi) Y~•••-•••••-•t•••--••••-·••••·-••••••••y•

•••••••u••••r••••••••••••••,

: : : ! : :

0 1.0- t····- · ··, . . ···111111111. Ill t I II • I I •.• ~-••••••n•••••l••••••••-•••••i••u••••••••••t••••••••••••••~••••••-•••••••~••••••••••••••l•••u••u•••••~•••••••••••••U~•u•••••••••••~

I 0

I 10

I 20

I 30

I 40

I 50

I 60

I 70

I 80

I 90

(b) Vs of Subgrade = 750 fps(E= 40 ksi) 4.0 ~·····-···-·r• .. ••••••••••-r·--·····--•,•••••••·-··-y-'"•·-···•·•t•••••·-··-··•·••••••••••••·~·••••••••••••••r••••••·

·••·•·•.

~~~~ .9 ~ 3.0 c 0 ·5 2.o

(1.) t;::

(1.)

0 1.0 : : : : : : : : : : Y.••••••••n••uJ.••••••••n••••i•••••••n•••••i••••••••••••••*•••••-•••-•••}o•••••••••••••i••••••••••••••'•••••••••••••••i-••••••••••••••:

0 10 20 30 40 50 60 70 80 90

(c) Vs of Subgrade = 1000 fps (E= 70 ksi)

4.0 •r---·--.,.··---·--·,····-···-·-r·----... , .. _ .......... ~-·····-··.··---···••••if••••··•••••··•r•••••••·•·••••· . 0 ·-~ 3.0 c 0 ·5 2.o

(1.)

'= (1.) 0 1.0

. t ............... ~ .................. l. ..................... i ............ --[ .. _ ....... __ .. L ................... l ....... __ .... _._t __ ................... ~ .................. J

~mt~w.~t~ ~ ~ ~ ~ ~ ~ ~ ~ ~ l •:!'••••••••••••••,••••••••••••••-!--•u••••••••••~••••••••••••••

,••••••••••••••':••••••••••••••"!•••••u•o•oo•••~•••••••••u•••:•u.,.•••••••••-\'

0 10 20 30 40 50 60 70 80 90

(d) Vs of Subgrade = 1500 fps (E= 155 ksi)

4.0 - . . . . . .,.... -· : ··-·-·····-:·············:··············;

:J ::~m==-~i-~fi~ ~ 1.0 ~ t:==::rii i' Ill 'llll1IIl1Iili1 .. 1lilifi .. lii

l ................ l .................. L ................. i ................... l ................ l ..................... L ................ i ................... l .................... l

I 0

I 10

I 20

I I I I 30 40 50 60 Depth to bedrock (ft)

I 70

I 80

I 90

-+- Station 1 -&-Station2 -x- Station 3 ..,._ Station 4 -11- Station 5 -G- Station 6 -x- Station 7

-+- Station 1 -&-Station2 -x- Station 3 ..,._ Station 4 -11- Station 5 -G- Station 6 -x- Station 7

-+- Station 1 -&-Station2 -x- Station 3 ..,._Station 4 -11- Station 5 -G- Station 6 -x- Station 7

-+-Station 1 -&-Station2 -x- Station 3 ..,._ Station 4 -11- Station 5 -G- Station 6 -x- Station 7

Figure 8.8 Deflection ratio versus depth to bedrock for FWD tests at Profile 2 with saturated subgrade

conditions

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(a) Vs of Subgrade = 500 fps. (E= 21 ksi)

0 .i ..... 3.0 c: 0 ·5 2.o ~

<1.)

0 1.0

0 10 20 30 40 50 60 70 80 90

(b) Vs of Subgrade = 750 fps (E= 47 ksi) 4.0 - ....... --·-- .. ~- . ., ......... ~ .. .

·~ 3n . :-::--t=+=i=i=-~t=t=:=::j

1 ~;~ ~..~m~~:r~~h~h-~~~:1 J .. .,.,.,.,.,.,.,.,. l.,. .__ J,.,.,..,,._,,.,.,..,,..,,..j,.,..,,.,.,.~,.,.,.,.,.,.,.l .. u.•••••••••J•n*"'**"",."""i"'""'-"""'~" .. ,.nlu•••••••un•~•U••••••••••J I I I I I I I I I I 0 w 20 30 40 ~ 60 w w ~

(c) Vs of Subgrade = 1000 fps (E= 83 ksi)

.!::~t~fE§~j~~ J:~t~=-·~·~ t··-··--.. t ............ t·--- -;-···········: ............ 1 .............. :-·············t··--···· .. ·t··············l

0 w 20 30 40 ~ 60 w w ~

I 0

I 10

I I I I 30 40 50 60 Depth to bedrock (ft)

-+- Station 1 -e- Station 2 -** Station 3 -II-Station4 -11- Station 5 .....a- Station 6 -x- Station 7

-+- Station 1 -a- Station 2 -x- Station 3 -11- Station4 -11- Station 5 .....a- Station 6 -x- Station 7

-+- Station 1 -e- Station 2 -** Station 3 -II-Station4 ""*"StationS .....a- Station 6 -x- Station 7

-+- Station 1 -e- Station 2 -** Station 3 -11- Station4 -II-Station5 .....a- Station 6 -x- Station 7

Figure 8.9 Deflection ratio versus depth to bedrock for FWD tests at Profile 3 with saturated subgrade conditions

111

Page 122: Chia-Ray Seng, Kenneth H. Stokoe, II, and Jose M. Roesset · ft3 a cub~c feet 0.0328 meters cubed m3 ---=1 § temperature add 32) temperature yd cub1c yards 0.0765 meters cubed m3

,II

(a) Vs of Subgrade = 500 fps (E= 18 ksi) 2,0 - ~··- ·-•n••;"'" --•"'"!'"""""'""''""' ;-····- ;'" ............ uf'" ·- ........ ·--···•••••-••,..•h••••uu~ .. . . . . . : : .

I :::W.~E!-Et.~Ef.~l~~ .!) 0.8- +----t --:-···· .ll'IIE I I 1 ............... i .............. .:.-........ '······ .. ··-··1 ~ ; ; ; ; : : ··~············ ~-----..... -... r-·-·-~-·-·-r·-.... -~ ......................... 1 .................... 1 ........................ ~-·--~ .. -.......... 1 .................... 1 ........................ ~

I I I I I I I I I 1 o ro w ~ ~ ~ ro w w oo

(b) y s of Subgrade = 750 fps (E= 40 ksi)

-~ ~~~ r-±~~~l~=EE::E:=t~::=t3

j::~~~~1~ : : : : : : : a : :

1 1 I I I I I I I I o ro w ~ ~ ~ oo w w oo

(c) V s of Subgrade = 1000 fps (E= 70 ksi) 2.0

:

..lii...OL

=•• • 1 ; ;

I I I 0 10 w ~ ~ 50 ro 70 80 90

(d) Vs of Subgrade = 1500 fps(E= 155 ksi) 2.0 - . . ......... T ........ . . ·· ····-:···---·~-······- . ···

-~ 1.6 : t~=:±:=~==:l:::::=::f::::===::t::=:=::=:±:====f=::::::::J:::==:j::==:::::::! -~ 1.2~ !=iiitiliittiilin~t·;;li;i~ ~ o.

8 - ~=t=--==~~=:=~t.~~=t~~:::==t=:====~=:::::::f:::::::f:=::::::j

I 0

I 10

I 20

I I I I 30 ~ so ro Depth to bedrock (ft)

I 70

I 80

I 90

-+- Station 1 -e- Station 2 -x- Station 3 -B-Station4 -11-StationS -a- Station 6 -x- Station 7

-+- Station 1 -a- Station 2 -x- Station 3 -B- Station4 -II- StationS -a- Station 6 -x- Station 7

-+- Station 1 -e- Station 2 -x- Station 3 -B-Station4 -II-Station5 -a- Station 6 -x- Station 7

-+- Station 1 -e- Station 2 -x- Station 3 -B-Station4 -11-StationS -a- Station 6 -x- Station 7

Figure 8.10 Deflection ratio versus depth to bedrock for FWD tests at Profile 4 with saturated subgrade conditions

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APPENDIX C. DEFLECTION-TIME RECORDS IN THE FWD TEST

Shear Wave Approx. Depth Dampted Naturated Period (sec)

Velocity of Young's to Profile I Profile 2 Profile 3 Profile 4

Sub grade Modulus Bedrock (FM 137) (FM195) (Route 1) (llilO) (fps) (ksi) (ft)

500 14 5 0.0300 0.0300 0.0300 0.0365

500 14 7.5 0.0435 0.0425 0.0425 0.0490

500 14 10 0.0560 0.0550 0.0550 0.0615

500 14 20 0.1170 0.1080 0.1090 0.1200

750 32 5 0.0190 0.0200 0.0190 0.0240

750 32 7.5 0.0290 0.0290 0.0280 0.0320

750 32 10 0.0370 0.0038 0.0380 0.0410

750 32 20 0.0700 0.0710 0.0690 0.0715

1000 57 5 0.0165 0.0150 0.0150 0.0170

1000 57 7.5 0.0215 0.0200 0.0215 0.0240

1000 57 10 0.0270 0.0280 0.0270 0.0310

1000 57 20 0.0525 0.0525 0.0530 0.0535

1500 128 5 0.0100 0.0110 0.0085 0.0120

1500 128 7.5 0.0145 0.0145 0.0150 0.0160

1500 128 10 0.0180 0.0175 0.0185 .0.0190 1500 128 20 0.0350 0.0350 0.0350 0.0385

Table C.1 Damped natural period in the deflection-time histories for FWD testing at the four pavement profiles, with Poisson's ratio of unsaturated subgrade equal to 0.20

113

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Shear Wave Approx. Depth Dampted Naturated Period (sec)

Velocity of Young's to Profile 1 Profile 2 Profile 3 Profile 4

Sub grade Modulus Bedrock (FM 137) (FMI95) (Route I) (lli10) (fps) (ksi) (ft)

500 16 5 0.0275 0.0280 0.0260 0.0310 liqli 500 16 7.5 0.0360 0.0380 0.0375 0.0425 i !il!

ill'

I 500 16 10 0.0480 0.0500 0.0490 0.0540

500 16 20 0.0940 0.0910 0.0980 0.1050

750 36 5 0.0175 0.0175 0.0160 0.0210

750 36 7.5 0.0250 0.0350 0.0250 0.0290

750 36 10 0.0325 0.0340 0.0320 0.0360

750 36 20 0.0620 0.0620 0.0620 0.0700

1000 63 5 0.0140 0.0135 0.0135 0.0130

1000 63 7.5 0.0175 0.0190 0.0190 0.0220

1000 63 10 0.0235 0.0240 0.0245 0.0260 i i

1000 63 20 0.0450 0.0480 0.0475 0.0500

1500 142 5 0.0090 0.0095 0.0090 0.0100

1500 142 7.5 0.0120 0.0125 0.0120 0.0160

I' I'

1500 142 10 0.0160 0.0170 0.0160 0.0180 1500 142 20 0.0290 0.0300 0.0305 0.0320

I' il' .

Table C.2 Damped natural period in the deflection-time histories for FWD testing at the four pavement II I

profiles, with Poisson's ratio of unsaturated subgrade equal to 0.33

114

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Shear Wave Approx. Depth Dampted Naturated Period (sec) Velocity of Young's to Profile 1 Profile 2 Profile 3 Profile 4 Sub grade Modulus Bedrock (FM 137) (FMI95) (Roule 1) (fillO)

(Cps) (ksi) (ft)

500 17 5 0.0265 0.0265 0.0250 0.0290 500 17 7.5 0.0385 0.0380 0.0380 0.0405 500 17 10 0.0480 0.0490 0.0510 0.0500 500 17 20 0.0880 0.0850 0.0970 0.0975 750 37 5 0.0165 0.0160 0.0160 0.0190 750 37 7.5 0.0235 0.0260 0.0240 0.0270 750 37 10 0.0310 0.0320 0.0310 0.0355 750 37 20 0.0540 0.0640 0.0610 0.0670 1000 66 5 0.0120 0.0125 0.0130 0.0155 1000 66 7.5 0.0175 0.0175 0.0175 0.0205 1000 66 10 0.0225 0.0225 0.0240 0.0260 1000 66 20 0.0420 0.0435 0.0415 0.0520 1500 150 5 0.0085 0.0090 0.0080 0.0105 1500 150 7.5 0.0110 0.0110 0.0110 0.0120 1500 150 10 0.0130 0.0130 0.0140 0.0165 1500 150 20 0.0280 0.0285 0.0280 0.0330

Table C.3 Damped natural period in the deflection-time histories for FWD testing at the four pavement profiles, with Poisson's ratio of unsaturated subgrade equal to 0.40

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--------------~~--~~

Shear Wave Approx. Depth Dampted Naturated Period (sec)

Velocity of Young's to Profile 1 Profile 2 Profile 3 Profile 4

Sub grade Modulus Bedrock (FM 137) (FMI95) (Route 1) (lli10) (fps) (ksi) (ft)

500 18 5 0.0225 0.0240 0.0225 0.0250

500 18 7.5 0.0350 0.0350 0.0350 0.0350

500 18 10 0.0425 0.0445 0.0450 0.0450

500 18 20 0.0875 0.0880 0.0875 0.0875

750 40 5 0.0150 0.0175 0.0150 0.0175

750 40 7.5 0.0225 0.0215 0.0250 0.0250

750 40 10 0.0325 0.0295 0.0300 0.0300

750 40 20 0.0550 0.0585 0.0575 0.0575

1000 70 5 0.0125 0.0120 0.0125 0.0150

1000 70 7.5 0.0175 0.0175 0.0175 0.0175

1000 70 10 0.0225 0.0220 0.0225 0.0250

1000 70 20 0.0425 0.0440 0.0425 0.0450

1500 155 5 0.0075 0.0100 0.0075 0.0075

1500 155 7.5 0.0125 0.0125 0.0125 0.0125

1500 155 10 0.0150 0.0150 0.0150 0.0150 1500 155 20 0.0300 0.0300 0.0275 0.0325

Table C.4 Damped natural period in the deflection-time histories for FWD testing at the four pavement profiles with saturated subgrade conditions

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