geotechnical assessment and design · 2019-08-19 · geotechnical assessment and design bear flat...
TRANSCRIPT
Prepared for:
R.F. Binnie & Associates Ltd.
101 - 1577 7th Avenue, Prince George, BC, V2L 3P5
August 14, 2019
GEOTECHNICAL ASSESSMENT AND
DESIGN
Bear Flat Cache Creek Segment (East)
Highway 29, British Columbia
Project # KX05280503
‘Wood’ is a trading name for John Wood Group PLC and its subsidiaries
GEOTECHNICAL ASSESSMENT AND DESIGN
Bear Flat Cache Creek Segment (East)
Highway 29, British Columbia
Project # KX05280503
Prepared for: R.F. Binnie & Associates Ltd.
101 - 1577 7th Avenue, Prince George, BC, V2L 3P5
Prepared by: Wood Environment & Infrastructure Solutions,
a Division of Wood Canada Limited
3456 Opie Crescent Prince George, BC V2N 2P9
August 14, 2019
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Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Table of Contents
Table of Contents
INTRODUCTION ................................................................................................................................................................... 1
SCOPE ....................................................................................................................................................................................... 1
GENERAL PROJECT DESCRIPTION ................................................................................................................................ 2
BACKGROUND ...................................................................................................................................................................... 3
4.1 GEOLOGY ............................................................................................................................................................... 3
SITE CONDITIONS AND DISCUSSION ......................................................................................................................... 4
5.1 SUBSURFACE GEOLOGICAL CONDITIONS – HIGHWAY 29 REALIGNMENT ................................ 4
5.2 SHALE BEDROCK ................................................................................................................................................. 5
5.3 ACID ROCK DRAINAGE AND METAL LEACHING POTENTIAL ........................................................... 6
5.4 EXISTING HIGHWAY 29 ASPHALT THICKNESS ........................................................................................ 6
5.5 GROUNDWATER CONDITIONS ..................................................................................................................... 7
GEOTECHNICAL DESIGN CONSIDERATIONS & RECOMMENDATIONS ........................................................ 9
6.1 STRIPPING .............................................................................................................................................................. 9
6.2 SUBGRADE PREPARATION .............................................................................................................................. 9
6.3 TEMPORARY EXCAVATIONS .........................................................................................................................10
6.4 EMBANKMENT FILL CONSTRUCTION .......................................................................................................10
6.4.1 Embankment Fill East of Cache Creek (Station 407+450 to 408+880) .......................11
6.5 CUT SLOPES .........................................................................................................................................................15
6.6 GEOTEXTILE AND BIAXIAL GEOGRID SPECIFICATIONS .....................................................................16
6.7 PAVEMENT STRUCTURE .................................................................................................................................16
6.8 WASTE DISPOSAL .............................................................................................................................................17
6.9 INSTRUMENTATION ........................................................................................................................................18
6.9.1 New Instrumentation & Monitoring .........................................................................................18
6.9.2 Protection of Existing Instrumentation ....................................................................................19
6.10 DETAILED GEOTECHNICAL RECOMMENDATIONS BY STATION SECTION ................................19
CLOSURE ...............................................................................................................................................................................21
REFERENCES .........................................................................................................................................................................22
List of Appendices
APPENDIX A FIGURES
APPENDIX B SLOPE STABILITY ANALYSIS (SLOPE/W)
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Table of Contents
List of Tables
Table 5-1: Encountered Bedrock .................................................................................................................................................... 5
Table 5-2: Measured Asphalt Core Thickness ........................................................................................................................... 6
Table 5-3: Summary of Groundwater Monitoring ................................................................................................................... 8
Table 6-1: Summary of Subsurface Conditions (Sta. 407+450 to 408+880) ............................................................. 12
Table 6-2: Geotechnical Material Properties for Limit Equilibrium Slope Stability Analyses............................... 13
Table 6-3: Summary of Limit Equilibrium Slope Stability Analyses for 3H:1V Embankment Fill Slopes ......... 14
Table 6-4: Non-Woven Geotextile Specifications ................................................................................................................. 16
Table 6-5: Biaxial Polypropylene Geogrid Specifications .................................................................................................. 16
Table 6-6: Recommended Minimum Pavement Structure Thickness ........................................................................... 16
Table 6-7: Detailed Geotechnical Recommendations by Station Section .................................................................. 20
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Page 1
INTRODUCTION As part of BC Hydro’s proposed Site C Clean Energy Project, portions of the existing Highway 29
alignment between Hudson’s Hope and Charlie Lake, BC, will be flooded during normal reservoir
operation. Before filling of the reservoir, the affected portions of the highway will be relocated away from
the reservoir area. In support of the project, Wood Environment & Infrastructure Solutions a Division of
Wood Canada Limited (Wood), formerly Amec Foster Wheeler, was retained by R.F. Binnie & Associates
Ltd. (Binnie) to provide geotechnical engineering services in support of proposed realignment for an
approximately 4.9 km long segment of Highway 29. The general location is shown in Figure 1, and a plan
of the proposed realignment is provided on two map sheets in Figure 2. This report has been prepared
specifically in relation to the approximately 1.8 km long easternmost portion of the alignment located on
the east side of the Cache Creek valley and proposed new bridge crossing.
Granular borrow investigations carried out in the vicinity of the Bear Flat Cache Creek realignment are
described in separate reporting. Additional background geotechnical information is provided in our
previous report: Preliminary Geotechnical Assessment, Proposed Bear Flat Segment, Highway 29 Definition
Design, Site C Clean Energy Project dated 5 March 2012. Results of geotechnical subsurface investigations
carried out to date are provided in our report: Geotechnical Data Report, Bear Flat Cache Creek Segment,
dated 14 August 2019. Amec Foster Wheeler also produced a Geotechnical Assessment and Design
Report: Geotechnical Assessment and Design, Highway No. 29, Bear Flat-Cache Creek, dated 21 July 2017,
for a previous L4000-Line alignment which has since been superseded.
This report includes a description of the scope of services, methodology, a discussion of geotechnical
engineering analysis and geotechnical recommendations developed to support the detailed design for
the proposed highway alignment on the east side of Cache Creek. The detailed design (analysis and
reporting) of the bridge structure, abutments/end fills and portion of the alignment to the west of Cache
Creek are reported separately.
SCOPE The general scope of Wood’s geotechnical field assessment for the Bear Flat Cache Creek realignment
segment was as described in Work Order 5 Release 3 Highway 29 Contract Completion for the Cache Creek
West (CCW) segment and the Detail and Functional Design of a new alignment called the Cache Creek East
(CCE) segment, and pursuant to the Sub-Consultant Agreement between Binnie and Wood, dated 1 April
2018.
The geotechnical assessment included the following activities:
Attendance at project team meetings;
Review of relevant project background data;
Preparation of a site-specific health and safety plan for the field work;
Field reconnaissance to identify locations and access routes for the geotechnical investigation;
Development of multiple geotechnical site investigation plans and budgets for various phases of field
investigation;
Preparation of various site access plans and permit support information;
Procurement and coordination of subcontractor equipment and support services for the geotechnical
investigation work including utility location, tree fallers, Level 3 medical support with emergency
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Page 2
transport vehicle, an excavator contractor, traffic control, multiple drill rigs, as well as cone
penetration testing and downhole geophysical testing subcontractors;
Coordination of the access preparation and geotechnical investigation work with concurrent activities
by others, including property considerations, surveyors, archaeology and environmental studies;
Supervision of several phases of geotechnical field investigation, including logging of ground
conditions, retention of soil samples from test pits, and retention of soil and rock core samples from
boreholes;
Supervision of the installation of groundwater instrumentation (vibrating wire piezometers) at select
locations, and follow-up monitoring;
Coordination and review of in-situ seismic piezo-cone (sCPTu) and downhole geophysics data
procurement;
Laboratory testing on selected soil and rock samples;
Geotechnical analysis to develop appropriate design recommendations, including the following
analyses:
Limit equilibrium slope stability analyses (using Slope/W) for current conditions, at maximum
normal reservoir level (MNRL), and after emergency drawdown,
Settlement due to embankment loading.
Provision of interim geotechnical data reports and draft recommendations as required; and
Compilation of this report.
GENERAL PROJECT DESCRIPTION The proposed 4.9 km long Bear Flat Cache Creek realignment segment is referenced as L4000O43 (Binnie
draft geometric design drawings dated 24 June 2019). The subject L4000O43 Line begins near Station
404+200 (eastern terminus of what is referred to as the Cache Creek West segment of the new Highway
29 alignment) and runs north of and approximately parallel to the existing Highway 29 alignment. The
new alignment will consist of two paved lanes. A major bridge structure is planned over Cache Creek
between approximately Sta. 406+744 to Sta. 407+334. The new highway alignment then merges with the
existing highway at approximately Station 409+144.
This report provides a discussion and preliminary geotechnical recommendations prepared by Wood for
the functional design of the approximately 1.8 km section of the proposed Bear Flat Cache Creek segment
on the east side of Cache Creek (i.e. from Sta. 407+334 to 409+144). Generally, the new highway
alignment is located north of the future Site C reservoir shoreline, along an upper fluvial terrace level
within the Peace River valley.
Figure 1 depicts the general location of the project segment. Figure 2 presents a detailed plan view of the
new highway alignment on an orthophoto underlay. Figure 3 (sheets 1 to 4) depicts a profile view along
the new highway alignment centreline.
For more detailed descriptions of the background topographic, geology and terrain conditions along the
project segment, the reader is referred to our definition design phase reporting (Amec Foster Wheeler, 5
March 2012). Results of geotechnical subsurface investigations carried out to date are provided in our
report: Geotechnical Data Report, Bear Flat Cache Creek Segment, dated 14 August 2019.
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Bear Flat Cache Creek Segment (East)
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BACKGROUND
4.1 GEOLOGY
Within the study region the bedrock geology consists of Cretaceous marine sedimentary rock sequences
overlain by a series of glacial and fluvial Quaternary sediments (Hartman and Clague, 2008). The bedrock
units present include flakey and fissile shales and siltstone ascribed to the Shaftsbury Formation (part of
the Fort St. John Group), overlain by Dunvegan Formation sandstones and conglomerates (Hartman and
Clague, 2008 and Bidwell, 1999). Gates Formation sandstone (also part of the Fort St. John group) can be
found underlying the Shaftesbury Formation (Thurber, 1978). The bedding inclination of the bedrock has
been reported as near horizontal (Klohn Crippen Berger and SNC-Lavalin, 2003) in the vicinity of the
project segment, but may exhibit local undulation and variations.
The Dunvegan sandstone outcrops in upper elevation slopes within the Peace River Valley, within a
previously identified landslide feature (see Figure 2, Cache Creek Landslide). The contact between the
sandstone and the underlying shale is estimated to be near 670 m elevation (Thurber, 1978). The
Shaftesbury shale typically is well bedded with thin, weak layers, some of which include bentonitic clays
from ash fall deposits that exhibit high plasticity and have low shear strength (Bidwell, 1999). Stability
issues in the shale have developed from weak cementation, valley rebound due to stress relief and
movement along pre-sheared or weak layers parallel to bedding.
Within the Bear Flat Cache Creek project segment, shale bedrock outcrops are apparent along both the
Peace River and the Cache Creek valley sidewall slopes between the base of the valley at about 430 m
elevation up to about 465 m elevation. Shale is assumed to underlie the terrace on which the alignment
will be constructed at shallow depth, and underlie the upper terrace at depths of 3 to 16 m.
The Gates Formation can consist of sandstone, shale and silty shale. It does not outcrop within the Bear
Flat project segment and is anticipated to underlie the valley bottom at an unknown depth.
The Quaternary-age sediments of the Peace River region are well exposed in the study area. Several
research papers (Matthews, 1978; Hartman and Clague, 2008) identify and describe a series of
predecessor valleys of the Peace River and its tributaries. In general, four paleovalleys have been identified
within the proposed Site C reservoir area. The paleovalleys are sometimes wider, but generally shallower
than the modern valley. The valleys are infilled with a sediment sequence that can be listed by decreasing
age as follows: pre-glacial fluvial deposits overlying the bedrock; advance phase fine-grained
glaciolacustrine soils (Glacial Lake Mathews); glacial tills of the last glaciation, late-glacial fine-grained
glaciolacustrine deposits (Glacial Lake Peace) and post-glacial deposits including fluvial sand, gravel and
silt and landslide debris.
In the Bear Flat Cache Creek project segment, a predecessor of the modern Halfway River tributary
drainage meets the ancient Peace River valley. As a result, the Peace Valley sidewall slopes within the
project area west of Cache Creek are underlain by colluvium derived from glacial sediments. East of Cache
Creek valley, the slopes are primarily underlain by similar colluvium, but shale bedrock outcrops in existing
highway cuts on the lower reaches of Cache Creek Hill.
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Bear Flat Cache Creek Segment (East)
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SITE CONDITIONS AND DISCUSSION
5.1 SUBSURFACE GEOLOGICAL CONDITIONS – HIGHWAY 29
REALIGNMENT
Sta. 407+334 to 407+450: This section comprises the eastern approach to the planned new bridge
across the Cache Creek valley. Embankment sections up to 3.5 m high would be constructed on the
relatively level surface of a fluvial terrace. The subsurface conditions are anticipated to consist of up to 0.2
m of topsoil and 1.9 to 2.4 m high plastic clay and silt overlying 7.8 m to 9.6 m of compact to very dense
fluvial sand and gravel. Shale bedrock occurs under the sand and gravel, anticipated to be at an elevation
of approximately 462.6 m to 463.9 m along the alignment centerline.
Sta. 407+450 to 408+880: This section of the alignment comprises a significant embankment, ranging
up to 12 m in height, to be constructed adjacent to the existing Highway 29 alignment across terrain that
dips gently towards the south. Between approximately Sta. 407+900 and 408+340 the lower portions of
the highway embankment would be within the Site C reservoir. The south-sloping terrain appears to
represent a subdued colluvial fan consisting of fine-grained soils (likely derived from the adjacent Peace
River valley slopes to the north and east). The colluvial fan appears to overlie a remnant fluvial terrace
feature comprised of eroded shale bedrock, fluvial overbank and/or lacustrine soil deposits. Topsoil under
the embankment footprint is expected to range in thickness from 0.3 m to 0.5 m. Beneath the topsoil, the
foundation conditions for the embankment are expected to consist predominantly of firm to very stiff,
intermediate plasticity silty clay soils ranging in depth from 3 m to 10.7 m below ground surface. The silty
clay deposit thickness appeared to increase towards the north and east. Moisture contents were typically
at or below the plastic limit. The upper 4 m of silty clay appears to be over-consolidated, while at depth
the silty clay appeared to be normally to slightly over-consolidated. Weathered shale and/or shale
bedrock underlies the embankment area at variable depths (ranging from 3 m to greater than 25 m below
surface, at elevations between about 453 m and 466 m depending on location). Generally, the underlying
bedrock profile appeared to dip towards the south and west. In addition to the fine-grained soil and shale
bedrock, some isolated or discontinuous deposits of sand and gravel were noted to occur, typically
directly overlying the shale bedrock. Groundwater appears to be perched on some areas of bedrock and
may also be perched in the more permeable granular soil seams that directly overlie lower elevation
sections of the shale bedrock surface. Of note, at three locations north of Sta. 408+700 (drilling
encountered several meters of variably intact and/or distorted/broken shale within a sequence of
unconsolidated silt and clay soils. Within this section, between 3.1 and 7.9 m of the intervening shale
deposit was encountered at depths ranging from 8.2 m to 10.7 m below ground surface. It is postulated
that these shale deposits represent buried colluvium derived from the adjacent slope of the Peace River
valley, and possibly even distal portions of the landslide run-out debris from the adjacent historic Cache
Creek Slide area.
Sta. 408+880 to 409+143.892: Represents a transitional side slope fill area (up to 15 m in height) from
the low lying, gently sloping colluvial fan terrain described above, onto the existing Highway 29 fill
alignment along the lower reaches of the north slope of the Peace River valley, an area that is referred to
as Cache Creek Hill. Topsoil in the order of 0.3m in thickness is anticipated to occur on the native ground
and portions of the existing highway fill slope, although it may be deeper in some locations, particularly
along ditch bottoms. Foundation conditions for the new highway embankment are expected to consist of
a relatively thick sequence (up to at least 8.8 m) of low to medium plastic, stiff to very stiff silty clay and/or
highway embankment composed of similar material. Moisture contents for this fine-grained soil are
anticipated to be at or below the plastic limit. Intact shale bedrock is expected to be relatively deep, at
depths ranging from 13.1 to 14.5 m below ground surface (approximate elev. 498.9 m to 507 m),
depending on location. However, at two drill locations (BH16-A-034 and BH16-A-035) old landslide debris
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Page 5
or colluvium was noted at depths of 7.9 m and 8.8 m under the existing highway alignment. Significant
groundwater was not encountered in this area. However, there may be local pockets of groundwater
seepage on side slope areas not specifically investigated.
5.2 SHALE BEDROCK
In general, where bedrock was encountered during the investigation, it consisted of shale attributed to the
Shaftesbury Formation (part of the Fort. St. John Group). The Shaftesbury shale typically is well bedded
with thin, weak layers, some of which may include bentonitic clays from ash fall deposits that exhibit high
plasticity and have low shear strength. Stability issues in the shale have developed from weak
cementation, valley rebound due to stress relief and movement along pre-sheared or weak layers parallel
to bedding (Amec Foster Wheeler, 5 March 2012). Although it is not expected that shale bedrock will be
encountered by the proposed new highway alignment earthworks east of Cache Creek, the shale bedrock
locations and elevations encountered by drilling relative to the L4000O43-Line (Station and Offsets) are
summarized in Table 5.1, below.
In general, at the interface between the overburden and shale bedrock, the shale was weak, highly
weathered and in many instances resembled residual clay soil. Based on previous experience in the area,
portions of the Shaftesbury shale can be highly sensitive to moisture changes when exposed/disturbed
and can rapidly decompose to a clay-like soil. The shale bedrock is generally not considered suitable for
highway embankment fill construction without special consideration (low slope angles, careful placement,
encapsulation to prevent moisture driven decomposition, etc.).
Table 5-1: Encountered Bedrock
ID Station Offset
(m)
Bedrock Depth
(m)
Bedrock Elevation
(m)
BH18-A-073 407+331 -12 9.9 463.4
BH18-A-077 407+393 -8 10.2 463.9
BH18-A-017 407+435 40 9.7 463.6
BH18-A-051 407+540 -16 11.7 462.6
BH18-A-078 407+677 2 10.2 461.9
BH18-A-020 407+803 3 4.9 463.4
TH16-A-055 407+896 -22 3.6 460.8
BH16-A-026 407+996 -43 4.2 458.8
TH16-A-056 408+002 -2 3 458.9
BH16-A-027 408+129 -4 4.5 455.3
BH16-A-029 408+258 -36 5.7 458.6
BH16-A-028 408+261 92 7 453.4
BH16-A-030 408+377 39 5.8 458.6
BH16-A-031 408+500 53 9 462.6
BH16-A-032 408+505 -21 7.5 466.3
BH16-A-033 408+617 42 15.9 466.2
TH16-A-061 408+859 16 7.3 498.8
BH16-A-035 408+944.1 9.5 7.9 504.6
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Bear Flat Cache Creek Segment (East)
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5.3 ACID ROCK DRAINAGE AND METAL LEACHING POTENTIAL
In general, shale bedrock is anticipated to be below the limits of planned earthworks for the design
alignment. To assess the shale’s potential for acid rock drainage (ARD) and metal leaching (ML), two core
samples were selected from two drill holes completed near the western bridge abutment area (BH16-A-
015, at an approximate depth 7.6 m / elevation of 462 m and DH11-51, at approximate depth of 7.1 m /
elevation of 461.9 m). The samples were crushed and sent to SGS Canada Inc. (SGS) in Burnaby, BC for
acid-base accounting (ABA) analysis and multi-element analyses, and to SGS in Lakefield, Ontario for
quantitative X-ray diffraction by Rietveld Refinement. The laboratory results can be found in the
Geotechnical Data Report.
ABA results indicated that the pH values of the samples were 6.82 and 7.8 for BH16-A-015 and DH11-51,
respectively, with the total concentrations of sulphur at 0.52% and 0.48%. The acid potential (AP) values
(based on the sulphide content) were 11.3 and 12.2 tonnes CaCO3 per 1000 tonnes of material, and the
modified Sobek Neutralization Potential (NP) values were 3.4 and 32.7 tonnes CaCO3 per 1000 tonnes of
material respectively.
The neutralization potential ratio (NPR) is a measure of the proportion of NP to AP (NPR = NP/AP). The
NPR value for BH16-A-015 was 0.3, while for DH11-51 it was 2.68. Based on the NPR criteria outlined in
the guidance document Technical Circular Letter T-04/13 (MoTI, 15 September 2013), the sample from
BH16-A-15 was classified as having a high potential to produce ARD. The sample from DH11-15 was
classified as non-acid generating with low potential to produce ARD. While both samples contained pyrite
(1.2 to 1.3%), only DH11-51 had appreciable carbonate (calcite, siderite) which would provide offsetting
neutralization potential. This high variation between the two samples found in relatively close proximity
and at similar elevations suggests that the ARD & ML potential will most likely be highly variable and
dependent on local mineralogy within each shale layer. Accordingly, it will be onerous and likely
impractical to screen and separate non-acid generating layers from shale that is or has the potential to be
acid generating. Consequently, it is conservatively considered that all the shale bedrock, if encountered,
should be considered as potentially acid generating, and where excavated should be disposed of in an
environmentally appropriate manner. Should significant surface exposures of shale remain after
excavation, they could likely be appropriately treated by backfill cover as needed.
5.4 EXISTING HIGHWAY 29 ASPHALT THICKNESS
The results of the pavement drilling program along the existing pavement surface of Highway 29 are
provided inTable 5-2. Figure 2 depicts the coring locations.
Table 5-2: Measured Asphalt Core Thickness
Hole ID Thickness
(mm) Hole ID
Thickness
(mm)
PV16-A-016 165 PV16-A-025 85
PV16-A-017 180 PV16-A-026 55
PV16-A-018 210 PV16-B-027 70
PV16-A-019 135 PV16-A-028 50
PV16-B-020 155 PV16-B-029 70
PV16-A-021 185 PV16-A-030 55
PV16-A-022 180 PV16-A-031 60
PV16-A-023 215 PV16-A-032 70
PV16-A-024 140 - -
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5.5 GROUNDWATER CONDITIONS
Vibrating wire piezometers were installed to provide information on the long-term groundwater conditions
at the site. The details of the vibrating wire piezometers, along with maximum and minimum piezometric
levels in 2017 and 2018 are provided in Table 5-3. Further details on the instrumentation installation can
be found in the Geotechnical Data Report (Wood August 2019).
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Table 5-3: Summary of Groundwater Monitoring
Hole ID Station Offset Piezometer
No.
Elevation
Ground/Tip
(m)
Maximum
Measured
Piezometric
Level in 2016
Minimum
Measured
Piezometric
Level in 2016
Measured
Piezometric
Level in 2018
Measured
Piezometric
Level in 2019
BH16-A-025 407+412 269R
BH025A 461.3/436.3 439.9 445.5 445.5 445.5
BH025B 464.3/412.8 431.0 437.4 433.1 432.9
BH16-A-026 407+996 43L BH026 463.0 460.1 460.1 460.1 460.1
BH16-A-028 408+261 93R BH028 460.4/453.7 453.7 453.3 454.0 454.7
BH16-A-031 408+500 53R BH031B 471.6/467.3 469.6 468.5 468.8, 468.9 469.0
BH031A 471.6/462.8 470.7 470.5 470.7, 470.8 470.5
BH16-A-033 408+617 42R BH033A 482.1/473.6 475.9 475.8 476.7 476.5
BH033B 482.1/466.8 472.1 472.0 472.4 472.2
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GEOTECHNICAL DESIGN CONSIDERATIONS &
RECOMMENDATIONS Based on the office and field investigations to date, there does not appear to be any significant
geohazards or geotechnical conditions that would preclude the construction of the L4000O43 alignment
as proposed. Section 6.1 through Section 0 provide geotechnical recommendations that are generally
applicable for the design and construction of the new highway alignment. A summary of
recommendations specific to various station ranges is provided in Section 6.10. Recommendations are
based on specific base mapping data provided to Wood on 9 Jan 2018 and design alignment L4000O43
provided on 24 June 2019 by Binnie. The following recommendations also reference the Ministry of
Transportation and Infrastructure’s 2016 version of the Standard Specifications for Highway Construction
(SS2016), which will be used for the project construction.
6.1 STRIPPING
For design, unless indicated otherwise, a minimum average stripping depth of 300 mm should be
assumed at the base of the proposed fills. Additional areas (e.g. existing ditches, colluvial slopes and wet
areas) will require deeper stripping and/or sub-excavation of soft, wet, weakened and organic soils that
are unsuitable for fill foundations. All stripped foundation subgrades should be reviewed prior to fill
placement by a geotechnical engineer or their representative to confirm that underlying soft, wet,
weakened and organic soils have been appropriately removed and that conditions are as anticipated in
this report. Some additional details regarding stripping and/or sub-excavation specific to various project
station ranges are provided in Section 6.10, below.
6.2 SUBGRADE PREPARATION
For the purposes of fill construction, the following subgrade preparation procedure is recommended:
Remove all unsuitable materials such as loose fill, organic materials, stripping, and softened soils
from the subgrade surface. Location-specific guidance for additional sub-excavation (in excess of
stripping) of subgrade soils is provided in Section 6.10 below. A geotechnical engineer should
review all prepared subgrade prior to placement of fill (and/or geotextile separators, where
applicable) to confirm that unsuitable soils have been adequately removed.
Crown the subgrade to promote drainage by providing a minimum cross fall of 2% as soon as
possible following exposure of the subgrade soils. This will help minimize softening of the fine-
grained subgrade materials due to infiltration of surface water from precipitation events that occur
following exposure of the subgrade.
Minimize disturbance of the subgrade by limiting vehicle and construction traffic over the prepared
subgrade surface. If the subgrade surface is disturbed and becomes softened, removal of softened
soils and replacement with suitable fill will be required.
Deposits of unsuitable subgrade soils that are too deep to be practically removed will require
additional subgrade improvements as directed by a geotechnical engineer at the time of
construction. Subgrade improvements may consist of (but are not limited to) use of geotextile
separator(s), biaxial geogrid layer(s), granular backfills and/or other methods.
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6.3 TEMPORARY EXCAVATIONS
Temporary excavations greater than 1.2 m in depth, where worker entry is required should be constructed
in accordance with the current Part 20.78 through 20.95 of the Occupational Health and Safety Regulation
as per WorkSafeBC. The construction contractor, however, is ultimately responsible for the safety of
temporary excavation slopes. Should excavations encounter groundwater, flatter slopes than those
recommended by WorkSafeBC could be required. Excavations greater than 1.2 m in depth with steeper
slopes and those subject to seepage or sloughing should not be entered unless they are shored, braced
or sloped as approved by the contractor’s geotechnical engineer.
6.4 EMBANKMENT FILL CONSTRUCTION
For the majority of the alignment, new embankment fills are estimated to be greater than 5 m high.
Maximum fill slopes of 3H:1V are recommended. This maximum slope recommendation of 3H:1V is also
based on the embankment being constructed on a properly prepared subgrade approved by a
geotechnical engineer, and the fill consisting primarily of clean granular fill for its upper and lower
portions. Note that a stabilization berm is required for higher fill areas between Sta. 407+450 to 408+880.
See Section 6.4.1 for more details.
The following general recommendations are provided for fill construction.
All fill foundation preparation, fill placement and fill compaction operations should be observed by
qualified geotechnical engineering field personnel to confirm that the construction is in accordance
with the recommendations in this report and SS 2016.
Existing organic materials, loose fill and/or otherwise unsuitable soils should be removed from under
the footprint of any new fills and from the outside face of the existing fill slopes prior to placing the
new fill.
Fill materials should consist of inorganic granular soil with moisture contents near (±1%) of the
optimum moisture content (as determined by laboratory moisture-density testing) such that they are
conducive to good compaction. In general, the following two granular fill types are recommended for
indicated uses:
Clean Granular Fill (CGF) – to be used for all embankment/berm fills constructed below an elevation of
466 m, the lower or back 1 m of fills placed on or against groundwater seepage zones..
♦ Material is to be free of organics and other detritus and has less than 5 % passing the
0.075 mm sieve.
♦ Maximum particle size as large as 300 mm can be used, provided that adequate lift thickness
and compaction is achieved before placement of the next lift. The contractor must
demonstrate via test strips and test excavations that they have the equipment, methodology
and are achieving compaction nominally equivalent to 95 % (Standard Proctor Maximum Dry
Density as per the current version of ASTM D 698), with no observable segregation or
deflection and no rutting greater than 10 mm under construction traffic loading.
Type D Granular Fill (Type D) – to be used for all other fill locations, where internal drainage is not
required as described above.
♦ Material gradation shall meet SS 2016 Section 201.44 and consist of predominately granular
material with a maximum 300 mm particle size that contains a maximum of 20% fines
(material passing the 0.075 mm sieve), and is free of organics and other detritus material.
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
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Fills that will overlie seepage zones from existing fill or natural slopes will require field review by a
geotechnical engineer. These areas should be treated on a case by case basis and may need to be
treated by placement of a granular drainage blanket from the base of the excavation to a minimum of
2.0 m above the seepage area. Figure 5 Sheet 2 provides a typical construction detail for construction
of granular drainage blankets.
Fills underlain by groundwater seepage zones should be founded on a minimum 0.5 m thickness (as
measured above the high-water level or original ground surface, as determined by the geotechnical
engineer) of clean granular fill. A layer of non-woven geotextile (as defined in Section 6.6) should be
placed on the prepared subgrade before placement of granular drainage fill. Geotextile should also be
placed over granular drainage fill where finer-grained fill (i.e. having greater than 5% fines) will be
placed over the cleaner drainage fill.
Drainage from under an embankment area should be directed to an exposed face of a ditch or a sub-
drain system but should not be directed over the face of potentially unstable or erodible slopes
without additional armouring and/or riprap.
At the transition sections between the new highway embankment and existing embankment, positive
subsurface drainage away from the existing highway embankment is to be maintained. Fills placed
near an existing granular fill (e.g. SGSB) should be free-draining granular material and extend a
minimum 100 mm in elevation below the bottom of adjacent existing granular fill so as to not block
internal drainage.
6.4.1 Embankment Fill East of Cache Creek (Station 407+450 to 408+880)
An embankment fill up to 12m in height is proposed for this section. Based on completed sub-surface
investigations in this area, the fill foundation materials are anticipated to consist of firm to very stiff,
intermediate plasticity silty clay soils. Laboratory analysis indicated that predominantly the upper 4 m is
considered over-consolidated, while the fine-grained material at depth was normally to slightly over-
consolidated. Cone (sCPTu) penetration testing yielded similar findings. The silty clay presents limitations
in terms of slope stability and possibly settlement for embankment construction. Shale bedrock underlies
the silty clay soil deposit at depths ranging from 3 m to 15.9 m, depending on location. The upper contact
of the shale is weathered and appears to have deteriorated to a residual clay-like soil. The lightly
weathered to fresh bedrock below appeared stronger but may have weak seams of bedding planes which
may also present limitations for embankment slope stability depending on depth and height of
embankment at any one location. See Table 6-1 for a summary of subsurface conditions.
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Table 6-1: Summary of Subsurface Conditions (Sta. 407+450 to 408+880)
Hole ID/
Sta
tio
n
Ele
vati
on
To
pso
il
Silt/Clay Sand/Gravel
Residual
Soil/Highly
Weathered
Shale
Lightly
Weathered to
Fresh Shale
and/or
Sandstone
BH18-A-051 407+540 474.3 0.2 0.2-2.1 (CH) 2.1-11.7 (SP-SM) 11.7->13.6 -
BH18-A-078 407+677 472.1 0.2 0.2-1.8 (ML) 1.8-10.2 (SP) 10.2->10.3 -
BH18-A-020 407+803 468.3 0.2 0.2-1.8 (CL) 1.8-4.9 (GP-GM) 4.9->6.1 -
TH16-A-055 407+896 464.4 0.3 0.3-3.1 (CL-CH) 3.1-3.6 3.6->5.2
BH16-A-026 407+996 463.0 0.3 0.3-3.2 (CH) 3.2-4.2 (SP-SM) 4.2-8.6 >8.6
TH16-A-056 408+002 461.9 0.2 0.2-3.0 (CH) - 3.0->4.6 -
BH16-A-027 408+129 459.8 0.3 0.3-1.1 (CL)
1.5-4.5 (CL) 1.1-1.5 (SM2) 4.5-6.1 >6.1
BH16-A-029 408+258 464.3 - 1.3 (CL)
1.3-5.7 (CH) - 5.7-7.4 >7.4
BH16-A-028 408+261 460.4 - 0.8-6.2 (CL-CH) 0.8 (GP)
6.3-7.0 (SP-SM) 7.0-7.5> -
TH16-A-057/ 408+382 466.7 0.5 0.5-3.0 (CL) - >3.0 -
BH16-A-030 408+377 464.4 0.2 0.2-5.8 (CL-CH) - 5.8-10.6 >10.6
BH16-A-032 408+505 473.8 0.3 0.3-6.7 (CL-CH) 6.7-7.5 (GP) 7.5-10.8 >10.8
BH16-A-031 408+500 471.6 0.2 0.2-9.0 (CL-CH) - 9.0-11.3 >11.3
TH16-A-058/ 408+625 482.0 0.3 0.3->5.2 (CL-CH) - - -
BH16-A-033 408+617 482.1 0.2
0.2-8.2 (CL-CH)
8.2-11.3 (BX*1)
11.3-12.5 (CL-CH)
12.5-15.9 (SM1) 15.9->19.8 -
TH16-A-060 408+741 492.4 0.3 0.3-6.7 (CL-CH) - - -
BH16-A-034 408+741 493.4 0.3
0.3-10.7 (CL-CH)
10.7-18.6 (BX*1)
18.6-24.5 (CL-CH)
24.5->24.8 (SM2) - -
TH16-A-059 408+859 494.9 0.2 0.2->5.2 (CL-CH) - - -
*1 – Landslide Debris
Note: Soil classifications based on the MOTI Soil Classification System.
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To assess the suitability of the proposed alignment and possibly required stability improvement measures,
limit equilibrium slope stability analyses were undertaken at four locations along the proposed
embankment section using the proprietary computer program Slope/W by GeoSlope International Inc.
The Morgenstern half-slice function was used to resolve interslice forces. The geometry of the slope and
the stratigraphy was based on available survey and embankment geometry provided by Binnie and
subsurface information obtained during the geotechnical field investigation. Potentially weak horizontal
shale layers were included in the stability models for the sections analyzed. A summary of the parameters
used in the stability analysis is provided in Table 6-2.
Table 6-2: Geotechnical Material Properties for Limit Equilibrium Slope Stability Analyses
Soil Type
Unit
Weight
(kN/m3)
Limit Equilibrium
Shear Strength
Model
Cohesion
(kPa)
Angle of
Internal
Friction (°)
Tau/Sigma
Ratio
Minimum
Strength
(kPa)
Embankment
Sand and Gravel
Fill
21 Mohr-Coulomb 0 36 - -
Clay/Silt 19 Mohr-Coulomb 0 22 - -
S=f(overburden) - - 0.22 35
Sand and Gravel 21 Mohr-Coulomb 0 37 - -
Weathered
Shale 24.5 Mohr-Coulomb 0 30 - -
Lightly
Weathered to
Fresh Shale
24.5 Anisotropic
Strength 50
45 (vertical)
35
(horizontal)
- -
RipRap 22 Mohr-Coulomb - 43 - -
Where the failure of a slope would affect highway operation (i.e. a potential failure envelope encroaches
the paved surface, a failure causes lane closures, or failure might necessitate excessive maintenance),
minimum factors of safety under static loading conditions in accordance with Table 6.2b of the BC
MoTI (British Columbia Ministry of Transportation and Infrastructure) Supplement to CHBDC (Canadian
Highway Bridge Design Code) S6-14 were applied. The minimum required factor of safety for global long-
term slope stability for a typical consequence slope with a typical degree of understanding is 1.54,
assuming a reservoir at maximum normal reservoir level (elev. 461. 8 m). The minimum required factor of
safety for global short-term slope stability for a typical consequence slope with a typical degree of
understanding is 1.34, assuming a reservoir at maximum normal reservoir level (elev. 461. 8 m). The
minimum required factor of safety for the emergency drawdown scenario for the reservoir is 1.24. The
geotechnical design criteria for the rapid drawdown scenario used in the stability analyses were as follows;
elevation 461.8 m to 452.5 m at approximately 4.5 m per day, then to 444 m at 2.5 m per day.
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Table 6-3: Summary of Limit Equilibrium Slope Stability Analyses for 3H:1V Embankment Fill Slopes
Station Design Case Required
FOS
No Berm
FOS
Berm
FOS
Minimum Berm
Dimensions
407+910 Normal
Operating Level
Effective Stress 1.54 1.59*1
N/A N/A
Undrained 1.33 1.63*1
Stage 2
Emergency
Drawdown
Effective Stress 1.24 1.59*1
Undrained 1.62*1
408+050 Normal
Operating Level
Effective Stress 1.54 1.44 1.57
6.0 m wide
3.6 m high
Undrained 1.33 1.45 1.61
Stage 2
Emergency
Drawdown
Effective Stress 1.24 1.08 1.24
Undrained 1.24 1.38
408+120 Normal
Operating Level
Effective Stress 1.54 1.40 1.55
9.25 m wide
2.6 m high
Undrained 1.33 1.37 1.44
Stage 2
Emergency
Drawdown
Effective Stress 1.24 1.08 1.25
Undrained 1.18 1.37
408+200 Normal
Operating Level
Effective Stress 1.54 1.39 1.54
8.75 m wide
2.8 m high
Undrained 1.33 1.29 1.43
Stage 2
Emergency
Drawdown
Effective Stress 1.24 1.16 1.33
Undrained 1.16 1.28
1. Modify ditch design so that an open ditch (if required) is eliminated or located a minimum 15 m away from the right fill toe. An alternative
approach would be to install a swale/culvert rather than an excavation that compromises stability. A ditch at the left fill toe is not required for
geotechnical purposes, but if still needed should not be excavated at the toe of the fill.
To achieve target FoS in relation to possible rapid drawdown scenarios, where portions of the
embankment and/or its stability berm will be inundated by the reservoir there will be a requirement to
construct the embankment from free draining granular fill. In addition, maintenance of adequate slope
stability is also predicated upon preservation of the existing ground profile beyond the toes of the
proposed highway embankment. On the reservoir side of the embankment, there is a need to protect not
only the toe of the embankment where it will encroach on the reservoir but also protect some of the
intervening original ground that although it will not be inundated will still be subject to attrition by
longer-term shoreline erosion. It is anticipated that placement of the required stability berm and riprap
armouring of the embankment would address the majority of this potential issue.
Given the depth and thickness of the underlying clay and the height of the planned embankment,
consolidation settlement of the foundation soils is anticipated to occur. To estimate the anticipated
settlement, one-dimensional consolidation theory was used, with established parameters based on
laboratory consolidation testing, and sCPTu in-situ testing data. The worst-case estimate for a 16.8 m
embankment resulted in a maximum total settlement in the order of 200 mm, which would be expected
to be largely complete within 12 to 18 months of embankment completion. The analysis uses the
assumption that consolidation would not start until the end of embankment construction. Given the time
required to construct an embankment of this size, it is likely that consolidation would be complete
somewhat earlier. Analyses based on the sCPTu data suggested that the maximum total settlement would
be somewhat less, at 150 mm for a 16.8 m embankment.
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Based on the investigation and analyses performed to date, the following specific recommendations are
provided for embankment construction at this location:
The embankment and stability berm footprint should be stripped of organic topsoil and any other
unsuitable (soft or wet) foundation soils and shaped to promote drainage.
The stripped and prepared subgrade should be reviewed and approved by a geotechnical engineer
before further construction. The geotechnical engineer will give direction as to required
improvements if any.
The approved subgrade should be protected from disturbance by construction equipment.
A non-woven geotextile (Class 2, as defined in Section 6.7, below), should be placed on the approved
subgrade before fill placement.
Embankment fill should be constructed at slopes no steeper than 3H:1V.
Between Sta. 407+920 and 408+620, a stability berm (approximately 2 m in height and 9.25 m wide,
with a maximum fill slope of no steeper than 3H:1V) should be constructed along the southern (right)
toe of the embankment.
The embankment fill height should not exceed the constructed height of the adjacent stability berm
by more than 1.0 m until after the stability berm has been completed to final design elevation.
Temporary internal fill placement slopes and ramp slopes shall not exceed 3 m in height if they are
constructed at slopes steeper than 3H:1V.
All portions of embankment and stability berm below elevation 466 m shall consist of clean granular
fill (CGF as defined in Section 6.4, above), having less than 5 % fines (passing 0.075 mm sieve). The
remaining fill material should have no more than 20 % fines (Type D as defined in Section 6.4 above).
For monitoring of stability and settlement, a program of geotechnical instrumentation is
recommended for the most critical portions of the embankment. The recommended instrumentation
program and protocol is provided in Section 6.9.1.
See Figure 5 (sheet 1) for typical section.
6.5 CUT SLOPES
Some shallow cuts up to 2 m and relatively minor ditch cuts of up to 2 m will be required for the currently
proposed alignment. The required cuts are expected to encounter mainly glaciofluvial and alluvial soils
(BCMoTI Type D excavation) that are generally anticipated to be unsuitable for use in the construction of
new highway embankments. For detailed design, the following recommendations are provided:
Unless otherwise specified in Section 6.10, use a maximum cut slope angle of 3H:1V.
Cuts that encounter seepage require field review by a geotechnical engineer and may need to be
protected from piping erosion by the placement of a granular drainage blanket on the face of the
slope from the base of the ditch to a minimum of 2 m above the seepage zone.
Fine-grained cut materials within the project alignment are unsuitable for re-use and should be
considered waste.
Cut areas should be hydro-seeded with an appropriate vegetation seed mix as soon as possible
after soil disturbance is complete.
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6.6 GEOTEXTILE AND BIAXIAL GEOGRID SPECIFICATIONS Where non-woven geotextiles are required, the recommended specifications listed in Table 6-4, below
should be used.
Table 6-4: Non-Woven Geotextile Specifications
2. Elongation > 50%, as per ASTM D4632
3. Based on minimum average roll values (as per ASTM C 4759) in the weaker principal direction
4. Based on maximum average roll values
Where geogrid is required for local subgrade improvement during construction, the recommended
specifications for a biaxial polypropylene geogrid are provided in Table 6-5, below.
Table 6-5: Biaxial Polypropylene Geogrid Specifications
Property Test Method Value
Tensile Strength @ 5% Strain, Machine Direction1 ASTM D 6637 ≥ 11.8 kN/m
Tensile Strength @ 5% Strain, Cross Machine Direction1 ASTM D 6637 ≥ 18.8 kN/m
Maximum Aperture Size 50 mm
Minimum Aperture Size 15 mm
Flexural Stiffness1 ASTM D 7748 ≥ 700 g-cm
Roll Width 4.0 +/- 0.1 m 1. Based on minimum average roll values (as per ASTM C4759).
6.7 PAVEMENT STRUCTURE
The recommended pavement structure is dependent on the nature of the soil subgrade that will be
encountered (in cuts) or constructed (fills). Table 6-6 provides a recommended pavement structure for the
new highway alignment, for two different subgrade conditions (Type A for well-drained granular
subgrades, Type B for poorly drained and/or fine-grained subgrades).
Table 6-6: Recommended Minimum Pavement Structure Thickness
Property Test Method Class 1 Class 2
Material Type Non-Woven1 Non-Woven1
Grab Tensile Strength2 ASTM D 4632 ≥ 900 N ≥ 700 N
Sewn Seam Strength2 ASTM D 4632 ≥ 810 ≥ 630 N
Tear Strength2 ASTM D 4533 ≥ 350 ≥ 250 N
Puncture Strength2 ASTM D 6241 ≥ 1925 ≥ 1375 N
Permittivity ASTM D4491 ≥ 0.2 sec-1 ≥ 0.1 sec-1
Apparent Opening Size3 ASTM D 4751 < 0.43 mm < 0.22 mm
Recommended Application + 50 kg class riprap
drainage layers
subgrade separation
- 50 kg class riprap
Subgrade Type Pavement
Structure Asphalt (AP)
Crushed Base
Course SGSB
Well Drained Granular Soils (sand
and gravel <10% fines) A 125 mm 300 mm 300 mm
Poorly Drained or Fine-Grained
Soils (>10% fines) B 125 mm 300 mm 600 mm
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It is currently anticipated that the recommended Type B structure would be used for the entire alignment
segment. However, in cases where subgrade fill soils meet the gradation for SGSB, the thinner Type A
structure can be substituted. Additionally, where new pavement structures will abut existing pavement
structures, the new SGSB thickness should match or exceed that of the existing structure to not hinder
drainage.
6.8 WASTE DISPOSAL
The following procedures are recommended for general siting and placing waste from unsuitable or
surplus soil materials generated by the project. Specific disposal scenarios different from below should be
assessed on a case by case basis by a geotechnical engineer.
Waste materials should only be placed on slopes with a gradient of 10° (approx. 5.7H:1V) or less
and should not be placed in the vicinity of the crests of other slopes where they could have a de-
stabilizing influence.
Do not site waste areas within or near environmentally sensitive locations such as riparian zones,
seepage zones, or where the waste will cause ponding of water or redirection of drainage patterns
(including ditches).
Waste materials should be placed with a maximum slope of 3H:1V, and to a maximum height of
3 m. Place the waste in maximum 1 m thick lifts and level with tracked equipment, as required.
Do not site waste piles adjacent to existing and proposed road fills, where practicable. Waste piles
placed adjacent to road fills are often encountered during future road widening and upgrading
projects, frequently leading to costly removal (and schedule delays) during construction.
Waste piles placed adjacent to road fills should not block drainage from existing fills and should be
kept at least 1 m below existing or proposed road pavement structure subgrade and/or any other
granular fills that are likely to transmit drainage.
Contour the waste material to promote surface drainage. To maintain positive drainage from the
fill surface while allowing for long-term settlement of the loosely placed fill, use a minimum 10%
cross fall slopes to crown the waste material.
Use appropriate short-term measures to control off-site transport of fines in runoff (such as silt
fencing). Maintain the short-term controls until effective long-term measures (such as vegetation
cover) are established.
Subject to relevant environmental and land use requirements, disposal of surplus excavation material
(waste) is not anticipated to be a geotechnical concern, especially if deposited on fluvial terrace areas and/or
below the reservoir inundation level. Surplus material should not be disposed along the Cache Creek valley
slope crest, the main Peace River Valley sidewall slope located above and to the north of the proposed
alignment and/or along the crests of the slopes down to the Peace River, as these areas may be unstable.
Also, waste material should not be disposed of against the downstream (right side) toes of embankments
and stability berms where internal drainage of the embankment under static and rapid-drawdown reservoir
conditions is required.
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6.9 INSTRUMENTATION
6.9.1 New Instrumentation & Monitoring
To facilitate monitoring of stability and settlement of the fill area between Sta.407+450 and 408+880, a
program of instrument installation and monitoring during construction is recommended. Prior to fill
construction, and once the fill subgrade has been prepared, a series of vibrating wire piezometers (VWP)
paired with settlement plates (SP) fitted with steel riser survey pipe is recommended for the following five
locations:
SP/VWP 19-01 Sta. 408+000 offset 5 m Right (VWP at 5 m depth)
SP/VWP 19-02 Sta. 408+120 offset 5 m Right (VWP at 5 m depth)
SP/VWP 19-03 Sta. 408+260 offset 5 m Right (VWP at 5 m depth)
SP/VWP 19-04 Sta. 408+380 offset 5 m Right (VWP at 5 m depth)
SP/VWP 19-05 Sta. 408+500 offset 7 m Right (VWP at 5 m depth)
The vibrating wire piezometers should be installed by drilling through the prepared subgrade depths of
approximately 5 m and then fully grouting in the piezometers. After three days (to allow grout set-up and
piezometer stabilization), the settlement plates should be placed on the prepared subgrade on or near
the locations of the vibrating wire piezometers. The cables from the piezometers should be threaded up
through the steel riser pipes. The initial elevations of the settlement plates (and piezometer tips) should
then be determined by field survey. Fill can then proceed, with successive surveys, and additional lengths
of riser pipes added as required.
When the stability berm has been constructed to its design elevations, fill placement should be
temporarily suspended, and slope inclinometer (SI) casings should be installed by drilling and grouting
through the top of the stability berm to 15 m deep at the following four locations at or near the rear of
the berm:
SI 19-01 Sta. 408+000 offset 30 m Right (SI to 15 m depth)
SI 19-02 Sta. 408+120 offset 35 m Right (SI to 15 m depth)
SI 19-03 Sta. 408+260 offset 35 m Right (SI to 15 m depth)
SI 19-04 Sta. 408+380 offset 40 m Right (SI to 15 m depth)
Fill placement should not resume until at least three days after the slope inclinometer casings have been
installed and initial surveys conducted.
A geotechnical engineer should coordinate and review the monitoring program. After initial
measurements, the frequency of successive measurements and requirements are for adjustments to the
construction operations (if any) will be determined by the geotechnical engineer based on fill placement
rates and results from the monitoring. As a preliminary guide, it is considered that fill placement would be
suspended for a period of at least one week after placement of each successive 3.0 vertical meters of fill
above the completed elevation of the adjacent stability berm to allow the analysis of monitoring results.
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6.9.2 Protection of Existing Instrumentation
Geotechnical instrumentation in the form of piezometers (vibrating wire and standpipes) and plastic (PVC)
site investigation casings have been installed during this and previous phases of site investigation. Some
of these locations should be preserved for additional monitoring during construction and post-
construction. The instrument locations to be preserved for future use include:
BH16-A-026 – Station 408+000 offset 45 m Left (VWP)
BH16-A-028 – Station 408+260 offset 90 m Right (VWP)
BH16-A-031 – Station 408+500 offset 52 m Right (VWP)
BH16-A-033 – Station 408+620 offset 45 m Right (VWP)
6.10 DETAILED GEOTECHNICAL RECOMMENDATIONS BY STATION
SECTION
A summary of geotechnical conditions encountered, and station specific recommendations are provided
in Table 6-7 on the following pages.
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Table 6-7: Detailed Geotechnical Recommendations by Station Section
Station Range Reference Geometric
Design Configuration
Representative
Geotechnical
Investigation
Anticipated Subsurface Conditions Geotechnical Recommendations
From To
407+334 407+500
Fill up to 5 m high
3H:1V Fill Slopes and up to
3 m ditch cuts 3H:1V BH18-A-019, BH18-A-078
Upper 0.2 m: Topsoil.
Below Topsoil: 1.1 to 1.9m of high plasticity SILT and CLAY.
Below Silt and Clay: approx. 6 m of SAND and GRAVEL over SHALE BEDROCK.
Bedrock at elev. 461.9 m to 463.0 m.
Groundwater not encountered during drilling.
Stripping Typically 2.1 m, maybe locally deeper. Subgrade to be
reviewed and approved by a geotechnical engineer.
Max Fill Slopes 3H:1V. Use granular fill.
407+500 407+700
Scatch grade/ Cuts up to
2 m
3H:1V Cut Slope
BH18-A-051
Upper 0.2 m: Topsoil
Below Topsoil: 2.0 m of high plasticity CLAY.
Below Clay: 9.6 m of GRAVEL and SAND over SHALE BEDROCK.
Bedrock ay elev. 462.6 m.
Groundwater encountered at Elev. 463.6 m.
Stripping Typically 2.1 m, maybe locally deeper.
Subgrade to be reviewed and approved by a geotechnical
engineer.
Max Cut Slopes 3H:1V.
407+450 408+880 Fill up to 12 m in height
3H:1V Fill Slopes
TH16-A-054 to TH16-A-062
BH16-A-026 to BH16-A-034
CPT16-A-003 to CPT16-A-
005
Upper 0.2 m: Topsoil.
Below Topsoil: 2.5 to 10.4 m of SILT and CLAY, with minor sand and gravel, increasing thickness to east.
Below Silt and Clay: SHALE BEDROCK (irregular profile, encountered between elev. 453.4 m and 466.3
m).
NOTE - north of approx. Stn. 408+617 buried landslide COLLUVIUM (several meters of weathered shale
within a thick silt and clay sequence) appears to have been encountered (8.2 - 11.3 m depth in BH16-A-
033, and 10.7 - 18.6 m depth in BH16-A-034) between elevations ranging between 471 and 483 m.
Groundwater encountered at some locations (approx. elev. 459.4 m in BH16-A-026; 467.7 m in BH16-A-
031; 464.7 m in BH16-A-032; 482.9 m in BH16-A-034; 463.9 m in TH16-A-057).
Stripping: Typically, 0.3 m, may be locally deeper.
Subgrade to be reviewed and approved by a geotechnical
engineer.
Approved subgrade to be covered with a non-woven geotextile.
Max Fill Slopes 3H:1V. Use granular fill.
Requires a granular stability berm on right side between Stn.
407+920 and 408+620.
Requires riprap protection on right side between Stn. 407+895 and
408+345.
Requires geotechnical instrumentation and monitoring.
SEE REPORT SECTION 6.9.1 FOR MORE DETAIL
408+880 409+143.892
Side slope transition
onto existing Highway 29
fill
Fill up to 10 m in height
on left (Side slope)
3H:1V Fill Slopes
TP16-A-061 to TP16-A-064
BH16-A-035 to BH16-A-036
Upper 0.3 m at the toe of existing fill: Topsoil
Below Topsoil adjacent to toe of existing fill: 7 to 8 m of SILT and CLAY over SHALE BEDROCK
Under Highway 29: up to 8.8 m of CLAY, FILL over fine-grained COLLUVIUM and SHALE BEDROCK.
NOTE - Buried landslide COLLUVIUM (several meters of weathered shale within a silt and clay
sequence) appears to have been encountered (8.8 - 13.1 m depth in BH16-A-035, and 7.9 - 12.8 m
depth in BH16-A-036) between elevations ranging between 505 and 512 m.
Bedrock elevation variable, encountered from elev. 498.8 to 504.6 m.
Groundwater encountered near elev. 494 m, in BH16-A-036.
Stripping: Typically, 0.3 m, 0.5 m on face of existing highway fill.
Max. Fill Slopes 3H:1V, use granular fill.
Requires side slope terracing on face of existing fill, potential for
additional sub-excavation to remove weak/wet pockets.
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503 | 8/14/2019 Page 22
REFERENCES Amec Foster Wheeler. (5 March 2012). Preliminary Geotechnical Assessment Proposed Bear Flat Segment
Highway 29 Definition Design.
Amec Foster Wheeler. (19 January 2017). Gravel Investigation – Lower Cache Creek Gravel Borrow
Prospect Highway 29: Bear Flat – Cache Creek.
Amec Foster Wheeler. (27 January 2017, revised 20 April 2018). Gravel Resource Assessment Peaceview Pit
Prospect Highway 29 Bear Flat to Cache Creek.
Amec Foster Wheeler. (21 July 2017). Geotechnical Assessment and Design Highway No. 29 Bear Flat –
Cache Creek.
Bidwell, A.K., May 1999, “The Engineering Geology of the Fort St. John Area”, Master of Engineering
Report, University of Alberta.
Hartman, G.M.D. and Clague, J.J., 25 June 2008, “Quaternary Stratigraphy and Glacial History of the Peace
River Valley, Northeast British Columbia”, Canadian Journal of Earth Science, Volume 45, pages 549-564.
Klohn Crippen Berger and SNC-Lavalin Inc., January 2003, “Peace Cascade Development, Prefeasibility for
a Cascade of Low Consequence Structures as an Alternative to Site C”, Technical Report.
Wood Environment and Infrastructure Solutions. (14 Aug 2019). Highway 29, Bear Flat Cache Creek
Segment, Geotechnical Data Report.
DesignAlignment
Hwy 29Peaceview PitProspect
Lower Cache CreekGravel Borrow Prospect
Ha l f
w a y R ive
r
C a c h e C r e e k
P e a c e R i v e r
C h a r l i eL a k e
Notes:1. L4000O43 centreline alignment provided by R.F. Binnie & Associates CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June 2019.2. Bing Maps Road - © 2018 Microsoft Corporation © 2018 HERE.
LegendL4000O43 Centreline Alignment
!(
!(
!(
!(
!(
_̂
VancouverKamloops
ChetwyndFort St John
PrinceGeorge
ProjectLocation
This drawing was originally produced in colour.
CLIENT:
\\Prg-fs1\cad\Internal\KX052805-GIS\4CacheCreek\CCE-AlignGeotechInvest-DetDes-Fig1-SiteLocationPlan.mxd
SCALE:
PROJECTION:
DATUM:
CHK'D BY:
DWN BY: TITLE:
PROJECT:REV NO.:
PROJECT NO.:
DATE:
HIGHWAY NO. 29BEAR FLAT CACHE CREEKUTM Zone 10
NAD 83
KS
BB SITE LOCATION PLANGEOTECHNICAL INVESTIGATION
A
FIGURE 1
KX05280503
AUGUST 2019
$
1:200,000
0 4 8 12 162km
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
WoodEnvironment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
BC HYDRO c/o R.F. BINNIE &ASSOCIATES LTD.
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
a Division of Wood Canada Limited (Wood)Wood Environment & Infrastructure Solutions
407+000
407+500
408+000
408+500
409+000
!A
!A
!A
!A!A
!A
!A
!A
!A
")
")
")
")
")
")
")
")
")
!A
!A
!A
!A
!A
!A
!A
!A!A
!A
!A!A
#*
#*
#*
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
!A
(See Note 1)
Highway 29
Ca c h e
Cr e
ek
BH17-A-001
DH-33
92-01
92-02
92-0392-04 92-05
92-06
92-07
92-08
PV16-025
PV16-028
PV16-029
PV16-031
PV16-030
PV16-026
PV16-032
PV16-027
BH18-A-014
BH18-A-017
BH18-A-019
BH18-A-020
BH18-A-043
BH18-A-046
BH18-A-051
BH18-A-073BH18-A-077
BH18-A-078
BH16-A-025
BH16-A-026
BH16-A-027
BH16-A-028
BH16-A-029
BH16-A-030BH16-A-031
BH16-A-032BH16-A-033
BH16-A-034
BH16-A-035BH16-A-036
TH16-A-051
TH16-A-052
TH16-A-053
TH16-A-054
TH16-A-055
TH16-A-056
TH16-A-057
TH16-A-058
TH16-A-059
TH16-A-060
TH16-A-061
TH16-A-062
TH16-A-063
TH16-A-064
BH17-A-002
BH17-A-003
CPT16-A-003
CPT16-A-004
CPT16-A-005
PROJECTION:
DATUM:
CHK'D BY:
DWN BY:
This drawing was originally produced in colour.
CLIENT: DATE:
KX05280503
AUGUST 2019
A
SITE PLAN WITH ORTHOPHOTOGEOTECHNICAL INVESTIGATION
HIGHWAY NO. 29BEAR FLAT CACHE CREEK
FIGURE 2
TITLE:
PROJECT:
UTM Zone 10
NAD 83
KS
BBPROJECT NO.:
REV NO.:
1:5,000\\Prg-fs1\cad\Internal\KX052805-GIS\4CacheCreek\CCE-AlignGeotechInvest-DetDes-Fig2-SitePlan-Ortho.mxd
SCALE:
0 130 260 390 52065m
Notes:1. Survey by WSP.2. Hole location provided by handheld GPS.3. L4000O43 centreline alignment and slope stake lines provided by R.F. Binnie & Associates CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June 2019.4. Maximum Normal Reservoir Level (461.8 m) downloaded from BC Hydro SharePoint 11 April 2018.5. Orthophoto imagery provided by BC Hydro 9 January 2018.
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.Legend!A 2018 Borehole Location !A 2016/2017 Borehole Location
#* 2016 CPT Location
") 2016 Pavement Core Location
!A Historical Drillhole LocationL4000O43 Centreline AlignmentL4000O43 Slope Stake LineMaximum Normal Reservoir Level (461.8 m)
$
407+200 407+300 407+400 407+500 407+600 407+700
430
440
450
460
470
430
440
450
460
470
420 420
407+150 407+250 407+350 407+450 407+550 407+650
Elevation (m
)
Station (m)
Elevation (m
)
407+100407+050
410 410
480 480
C a c h e C r e e k
Cross Section
Station 407+330
See Figure 4 Sheet 1
TSCL
GP
BREND
Water Level5/18/2018
0.31.6
9.710.8
183244485028223338352126
RRRR
19151111
11212
39
256
m
BH18-A-017N WW TS
CH
SP-SM
BREND
Water Level5/19/2018
0.2
2.1
11.7
13.6
1624817533353468
56
33
R
R
R
2017111211
2
2
6
6
13
23 65
m
BH18-A-051N WW PL LL
TSCH
GM1
GP
BR
END
Water Level4/28/2018
0.2
2
5.8
9.9
60.9
153178364738
53
33
33R
28232124
3
3
59
26 63
0.91 / 1.630.23 / 0.72
0.30 / 0.91
0.24 / 0.60
0.30 / 0.77
N/A / N/A
0.21 / 0.89
0.22 / 0.28
0.05 / 1.55
0.14 / 0.90
0.17 / 1.21
0.10 / 0.31
0.13 / 0.63
0.15 / 0.96
0.20 / 0.50
0.06 / 1.32
0.18 / 1.87
0.19 / 1.25
0.08 / 2.33
1.80 / 2.00
1.66 / 2.42
0.91 / 2.24
1.33 / 3.14
0.15 / 1.04
0.20 / 1.52
0.25 / 1.30
0.16 / 1.82
0.23 / 0.65
0.08 / 1.21
0.41 / 1.80
0.08 / 1.72
0.23 / 2.07
0.15 / 2.09
0.48 / 1.83
m
BH18-A-073N WW PL LL Is50Is50
Dia/Axial CH
GP-GM
BR
END
Water Level9/19/2018
2.4
10.2
27.3
172131512626
53
52
25
R
292116144
3
4
3
10
25 63
0.15 / 0.10
0.12 / 0.52
0.09 / 0.23
0.26 / 0.18
0.10 / 0.03
0.11 / 0.68
0.77 / 1.34
0.07 / 0.76
0.18 / 0.56
0.15 / 0.62
0.14 / 0.80
m
BH18-A-077N WW PL LL Is50Is50
Dia/Axial
TSML
SP
BR
0.2
1.8
10.210.3
85
38454749
37
47
R
R
25344332
4
3
6
8
m
BH18-A-078N WW
END
(MPa)(MPa)
N/A
PROJECTION:
N/A
DATUM:
PROFILE
STATION 407+050 TO 407+700
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
Legend
L4000O43P3 Centerline Alignment Profile
Existing Ground Profile at Centreline
FIGURE 3
SHEET NO. 1 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
0m 25 50 75 100
H 1 : 2000
V 1 : 400
0m 5 10 15 20
Notes:
1. SPT N values and associated laboratory testing data provided with the Sticklogs may not be
presented at representative elevations. Please refer to Geotechnical Data Report (July 2019)
Appendix B – Investigation Logs for additional details.
2. L4000O43P3 centreline alignment profile and existing ground profile provided by R.F. Binnie &
Associates Ltd. CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June
2019.
407+800 407+900 408+000 408+100 408+200 408+300
460
470
480
460
470
480
450 450
407+850 407+950 408+050 408+150 408+250
440 440
Elevation (m
)
Station (m)
Elevation (m
)
407+700 407+750 408+350
TSCL
GP-GM
BREND
Water Level5/17/2018
0.2
1.8
4.96.1
11226759
61RRR
102RR
2420112
10
10
m
BH18-A-020N WW
Water Level9/28/2016
0.3
3.24.2
19.7
TS
CH
SP-SM
BR
15
3
2222253530208
23 57
m
BH16-A-026N WW PL LL
0.31.11.5
4.5
13.6
TSCL
CL
BR
18
55
128189106
20 38
m
BH16-A-027N WW PL LL
1.3
5.7
30.2
CL
CH
BR
1215
21
232428
20
29
39
57
m
BH16-A-029WW PL LL
0.3
3.13.65.2
TS
CL-CH
BR
15
12
44
2020222519187
129
m
TH16-A-055N WW
END
END
END
END
SM2
SM2
Cross Section
Station 408+260
See Figure 4 Sheet 2
0.10 / 0.656.37 / 0.16
0.70 / 0.84
4.37 / 0.27
0.03 / 0.39
Is50Is50Dia/Axial
(MPa)
0.19 / 0.12
0.10 / 0.94
0.18 / 0.22
0.06 / 0.28
Is50Is50Dia/Axial
(MPa)
0.18 / 0.50
0.03 / 0.29
0.08 / 0.47
0.04 / 0.55
0.19 / 0.59
0.44 / 0.94
0.13 / 0.42
0.12 / 0.54
0.12 / 0.23
0.05 / 0.26
1.38 / 3.10
0.12 / 0.74
0.11 / 0.38
0.20 / 0.72
Is50Is50Dia/Axial
(MPa)
N/A
PROJECTION:
N/A
DATUM:
PROFILE
STATION 407+700 TO 408+350
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 3
SHEET NO. 2 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
0m 25 50 75 100
H 1 : 2000
V 1 : 400
0m 5 10 15 20
Legend
L4000O43P3 Centerline Alignment Profile
Existing Ground Profile at Centreline
Notes:
1. SPT N values and associated laboratory testing data provided with the Sticklogs may not be
presented at representative elevations. Please refer to Geotechnical Data Report (July 2019)
Appendix B – Investigation Logs for additional details.
2. L4000O43P3 centreline alignment profile and existing ground profile provided by R.F. Binnie &
Associates Ltd. CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June
2019.
408+400 408+500 408+600 408+700 408+800
490
500
510
520
490
500
510
520
480 480
408+450 408+550 408+650 408+750
470 470
Elevation (m
)
Station (m)
Elevation (m
)
408+350 408+850 408+900 408+950 409+000
460 460
Water Level5/17/2016
0.3
6.77.5
19.6
TS
CL-CH
GP
BR
15191816
17
17
30
110R
13131513161412181821202224147
27
18
57
41
m
BH16-A-032N WW PL LL
Water Level5/15/2016
0.3
10.7
18.6
24.524.8
TS
CL-CH
BX
CL-CH
SM2
17151529
12
15
14
13
14
8
15
15
21
26
21
810127
10668
131413181419161416201921222218
21
20
18
23
23242724
24
19
21
21
20
49
41
34
38
35
m
BH16-A-034N WW PL LL
Water Level5/13/2016
0.10.5
8.8
13.114.5
30.6
APSP
CL
BX
CL
BR
108
10
11
11
11
12
9
21
18
16
24
182015
15
17
19
21
20
22
27
27
20
2020
18
19
20
2321
36
35
39
3939
m
BH16-A-035N WW PL LL
Water Level4/30/2016
0.5
3
5.2
TS
CL
BR
10
9
6
222325304019
m
TH16-A-057N WW
0.3
5.2
TS
CL-CH16
15
9
10149
111513
24 45
m
TH16-A-058N WW PL LL
0.3
5.5
TS
CL
6
21
914
10101014
m
TH16-A-063N WW
END
END
END
END
END
ENDTS
CL
0.3
5.2 9
12
10
14
m
TH16-A-062N WW
Cross Section
Station 408+380
See Figure 4 Sheet 3
Cross Section
Station 408+500
See Figure 4 Sheet 4
0.23 / 0.56
0.15 / 0.52
0.08 / 0.71
0.77 / 0.93
0.33 / 0.54
Is50Is50Dia/Axial
(MPa)
N/A
PROJECTION:
N/A
DATUM:
PROFILE
STATION 408+350 TO 409+000
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 3
SHEET NO. 3 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
0m 25 50 75 100
H 1 : 2000
V 1 : 400
0m 5 10 15 20
Legend
L4000O43P3 Centerline Alignment Profile
Existing Ground Profile at Centreline
Notes:
1. SPT N values and associated laboratory testing data provided with the Sticklogs may not be
presented at representative elevations. Please refer to Geotechnical Data Report (July 2019)
Appendix B – Investigation Logs for additional details.
2. L4000O43P3 centreline alignment profile and existing ground profile provided by R.F. Binnie &
Associates Ltd. CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June
2019.
409+000
510
520
530
510
520
530
409+050
Elevation (m
)
Station (m)
Elevation (m
)
409+100 409+150 409+200 409+250 409+300 409+350 409+400 409+450 409+500 409+550 409+600 409+650
540 540
Highway 29
0.3
4.9
TS
CL21
20
9
141113121814
m
TH16-A-064N WW
END
N/A
PROJECTION:
N/A
DATUM:
PROFILE
STATION 409+000 TO 409+650
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 3
SHEET NO. 4 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
0m 25 50 75 100
H 1 : 2000
V 1 : 400
0m 5 10 15 20
Legend
L4000O43P3 Centerline Alignment Profile
Existing Ground Profile at Centreline
Notes:
1. SPT N values and associated laboratory testing data provided with the Sticklogs may not be
presented at representative elevations. Please refer to Geotechnical Data Report (July 2019)
Appendix B – Investigation Logs for additional details.
2. L4000O43P3 centreline alignment profile and existing ground profile provided by R.F. Binnie &
Associates Ltd. CAD file '20190624 - Alignment and Toes for Wood.dwg', received 24 June
2019.
-60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70-70
Elevation (m
)
460
440
420
-80
Elevation (m
)
460
440
420
480 480
TS
GP
BR
0.4
8.2
61.1 END
47412748R474854R
2222112
13
N/A / N/AN/A / N/A
0.23 / 0.280.18 / 0.380.36 / 1.110.25 / 1.740.51 / 2.380.14 / 0.790.23 / 0.450.55 / 0.870.25 / 0.630.08 / 0.550.10 / 0.620.09 / 0.830.17 / 1.060.19 / 1.420.08 / 0.920.27 / 0.840.28 / 0.830.13 / 0.610.50 / 0.851.11 / N/AN/A / N/A
0.42 / 1.05N/A / N/A
0.36 / 0.480.05 / 1.200.13 / 2.130.21 / 2.400.04 / 2.040.45 / 2.010.27 / 2.080.47 / 2.420.20 / 2.270.41 / 2.100.16 / 2.25
m
BH18-A-014N WW Is50Is50
Dia/AxialTS CL
GP
BR
0.22.4
10.8
50.3 END
Water Level5/21/2018
193173321025R48
50R90R
1715101022434
107
0.30 / 0.570.32 / 0.720.33 / 0.450.19 / 0.280.07 / 0.790.65 / 1.380.56 / 1.590.41 / 0.620.04 / 1.480.16 / 0.290.19 / 0.430.11 / 0.300.21 / 1.050.13 / 0.070.28 / 1.030.16 / 0.290.12 / 1.010.33 / 1.220.14 / 0.820.26 / 2.240.95 / 2.860.36 / 0.751.19 / 1.620.04 / 0.880.08 / 1.010.09 / 1.44
m
BH18-A-043N WW Is50Is50
Dia/Axial TS CL
GP
BR
0.22.1
10.2
61 END
Water Level5/24/2018
23295027674134
100R21R
1815113242588
0.15 / 0.630.07 / 0.480.15 / 0.770.07 / 0.930.01 / 0.350.12 / 0.340.14 / 1.010.19 / 0.150.18 / 0.280.10 / 0.390.01 / 0.310.10 / 0.850.10 / 0.340.09 / 1.110.24 / 1.960.02 / 1.280.16 / 0.870.25 / 1.170.15 / 1.511.78 / 0.880.94 / 2.130.70 / 0.840.22 / 0.540.01 / 0.270.18 / 0.900.16 / 0.810.17 / 1.300.20 / 0.410.01 / 0.960.27 / 0.950.29 / 0.890.21 / 1.380.35 / 1.34
m
BH18-A-046N WW Is50Is50
Dia/Axial TS CHGM1
GP
BR
0.22
5.8
9.9
60.9 END
Water Level4/28/2018
153178364738533333R
282321243359
26 63
0.91 / 1.630.23 / 0.720.30 / 0.910.24 / 0.600.30 / 0.77N/A / N/A
0.21 / 0.890.22 / 0.280.05 / 1.550.14 / 0.900.17 / 1.210.10 / 0.310.13 / 0.630.15 / 0.960.20 / 0.500.06 / 1.320.18 / 1.870.19 / 1.250.08 / 2.331.80 / 2.001.66 / 2.420.91 / 2.241.33 / 3.140.15 / 1.040.20 / 1.520.25 / 1.300.16 / 1.820.23 / 0.650.08 / 1.210.41 / 1.800.08 / 1.720.23 / 2.070.15 / 2.090.48 / 1.83
m
BH18-A-073N WW PL LL Is50Is50
Dia/Axial
Offset (m)
(MPa) (MPa) (MPa)(MPa)
℄L4000O43
407+330
N/A
PROJECTION:
N/A
DATUM:
CROSS SECTION
STATION 407+330
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
Legend
Existing Ground Profile at Centreline
FIGURE 4
SHEET NO. 1 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
100m 5 2015
H 1 : 500
V 1 : 1000
200m 10 4030
Notes:
1. Existing ground (main) provided by R.F. Binnie & Associates Ltd. CAD file
'CCE-L4000O41p2-XS_WOOD.dwg', received 21 November 2018.
2. Additional existing ground (approximate) processed from LIDAR (UTM) provided by
BC Hydro 9 January 2018.
℄
440
480
Elevation (m
)
460
440
480
Elevation (m
)
460
-60 -40 -20 0 20 40 60-80
Offset (m)
-100-120 80 100 120
CPT16-A-004
Avg qt(kPa) Avg fs
(kPa)100005000 250 500
5
Refusal
GP
CL-CH
SP-SMBR
0.8
6.37
10.7
71015171714131130
2524282324281524810
2626
23
4452
58
0.06 / 0.681.8 / 1.65
m
BH16-A-028N WW PL LL Is50Is50
Dia/Axial
CL
CH
BR
1.3
5.7
30.2
121521232428
20
29
39
57
0.18 / 0.500.03 / 0.290.08 / 0.470.04 / 0.550.19 / 0.590.44 / 0.940.13 / 0.420.12 / 0.540.12 / 0.230.05 / 0.261.38 / 3.10
0.12 / 0.740.11 / 0.380.20 / 0.72
m
BH16-A-029WW PL LL Is50Is50
Dia/Axial
END
END
L4000O43
408+260
(MPa)
(MPa)
N/A
PROJECTION:
N/A
DATUM:
CROSS SECTION
STATION 408+260
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
1:750
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 4
SHEET NO. 2 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
Legend
Typical Cross Section Based on L4000O43 Centerline Alignment
Existing Ground Profile at Centreline
Notes:
1. Typical cross section based on L4000O43 centerline alignment and existing ground
profile at centreline provided by R.F. Binnie & Associates Ltd. CAD file '20190624 -
L4000O43 Cross Sections.dwg', received 24 June 2019.
2. Additional existing ground profile at centreline (approximate) processed from LIDAR
provided by BC Hydro 9 January 2018.
1 : 750
5 1510 20 25 300m
440
480
-60 -40 -20 0 20 40 60-80
Offset (m)
80
℄L4000O43
460
Elevation (m
)
TSCL
BR
0.5
3
5.2Water Level
4/30/2016
10
9
6
222325304019
m
TH16-A-057N WW
END
TS
CL-CH
BR
0.2
5.8
15.1
182224252931196
18
26
28
62
0.06 / 0.110.09 / 0.570.14 / 0.460.33 / 0.51
m
BH16-A-030N WW PL LL Is50Is50
Dia/Axial
440
480
460
Elevation (m
)
408+380
(MPa)
N/A
PROJECTION:
N/A
DATUM:
CROSS SECTION
STATION 408+380
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
1:600
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 4
SHEET NO. 3 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
Legend
Typical Cross Section Based on L4000O43 Centerline Alignment
Existing Ground Profile at Centreline
24181260m
1 : 600
Notes:
1. Typical cross section based on L4000O43 centerline alignment and existing ground
profile at centreline provided by R.F. Binnie & Associates Ltd. CAD file '20190624 -
L4000O43 Cross Sections.dwg', received 24 June 2019.
2. Additional existing ground profile at centreline (approximate) processed from LIDAR
provided by BC Hydro 9 January 2018.
460
-60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70
Offset (m)
80
℄L4000O43
Elevation (m
)
450
470
460
Elevation (m
)
450
470
480 480
Avg qt(kPa) Avg fs
(kPa)100005000 250 500
Refusal
5
CPT16-A-005(See Note 1)
TS
CL-CH
BR
0.2
9
19.3
161486
8
6
23
R
131214122227242426222125283027143116151012
21
21
21
45
44
47
0.03 / 0.500.21 / 0.440.28 / 1.240.25 / 0.970.29 / 0.92
m
BH16-A-031N WW PL LL Is50Is50
Dia/Axial
TS
CL-CH
GP
BR
0.3
6.77.5
19.6
Water Level5/17/2016
15191816
17
1730
110R
13131513161412181821202224147
27
18
57
41
0.23 / 0.560.15 / 0.520.08 / 0.710.77 / 0.930.33 / 0.54
m
BH16-A-032N WW PL LL Is50Is50
Dia/Axial
END
END
408+500
(MPa)
(MPa)
N/A
PROJECTION:
N/A
DATUM:
CROSS SECTION
STATION 408+500
GEOTECHNICAL INVESTIGATION
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
1:500
BB
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 4
SHEET NO. 4 of 4
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
Legend
Typical Cross Section Based on L4000O43 Centerline Alignment
Existing Ground Profile at Centreline
100m 5
1 : 500
2015
Notes:
1. Hole location provided by ConeTec.
2. Typical cross section based on L4000O43 centerline alignment and existing ground profile at
centreline provided by R.F. Binnie & Associates Ltd. CAD file '20190624 - L4000O43 Cross
Sections.dwg', received 24 June 2019.
3. Additional (approximate) existing ground profile at centreline processed from LIDAR provided
by BC Hydro 9 January 2018.
PROPERTY TEST METHOD CLASS 2
Material Type
Non-Woven ¹Grab Tensile Strength ²
ASTM D 4632> 700N
Sewn Seam Strength ²
ASTM D 4632> 630N
Tear Strength ²
ASTM D 4533> 250N
Puncture Strength ²
ASTM D 6241> 1375N
Permittivity
ASTM D 4491> 0.1 sec ¹
Apparent Opening Size ³
ASTM D 4751 < 0.22mm
Recommend Application
Drainage layers subgrade
separation -50 kg class riprap
Pavement Structure
3H:1V
El. 466m
Type D Granular Fill
(<20% fines)
Settlement Plate
New VWP
(To be installed prior
to fill placement)
Clean Granular Fill (<5% fines)
3H:1V
El. 466m
Original Ground
Stripping
300mm (min)
subgrade to be
approved by
Geotechnical
Engineer
Non-woven
geotextile
(Class 2)
New SI Casing
(To be installed after
the completion of the
stability berm)
20H:1VRiprap
Stability Berm
min 2m, max 4m thick
3H:1V
Highway Embankment
(See Note 1)
SGSB (minimum 600 mm)
Note 1: Until the Stability Berm is constructed to the final design height, Highway Embankment fill height is not to exceed 1.0 m above the Stability Berm height.
Recommended Geotextile Specifications
N/A
PROJECTION:
N/A
DATUM:
TYPICAL SECTION BETWEEN
STATION 407+920 TO STATION 408+620
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB/NW
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 5
SHEET NO. 1 of 2
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
Sieve Size
(mm)
Percent Passing
by Weight (%)
150 100
75 50 - 100
50 30 - 100
19 20 - 100
4.75 10 - 60
1.18 6 - 32
0.300 3 - 15
0.075 0 - 5
PROPERTY TEST METHOD CLASS 2
Material Type
Non-Woven ¹Grab Tensile Strength ²
ASTM D 4632> 700N
Sewn Seam Strength ²
ASTM D 4632> 630N
Tear Strength ²
ASTM D 4533> 250N
Puncture Strength ²
ASTM D 6241> 1375N
Permittivity
ASTM D 4491> 0.1 sec ¹
Apparent Opening Size ³
ASTM D 4751 < 0.22mm
Recommend Application
Drainage layers subgrade
separation -50 kg class riprap
2.0m (min)
Seepage
Zone
Place parallel to
prepared cut slope
Top of cut
Non-woven geotextile
(Class 2)
2.0m (min)
Top of seepage zone
1m (min)
Seepage
Zone
Place parallel to
prepared slope
Perforated PVC drain (if required)
Top of fill
Drainage Blanket
Non-woven geotextile
(Class 2)
Top of seepage zone
Prepared existing fill
slope or subgrate
Designed fill
1m (min)
Maintain design ditch
Existing
Cut Slope
See Note 6
Drainage Blanket
N/A
PROJECTION:
N/A
DATUM:
TYPICAL SECTIONS
GRANULAR DRAINAGE BLANKET DETAILS
PROJECT:
TITLE:
REV. NO.:
PROJECT NO.:
KX05280503
A
CLIENT:
DWN BY:
CHK'D BY:
AUGUST 2019
DATE:
SCALE:
KS
AS NOTED
BB/NW
HIGHWAY NO. 29
BEAR FLAT CACHE CREEK
This drawing was originally produced in colour.
FIGURE 5
SHEET NO. 2 of 2
Wood Environment & Infrastructure Solutions
a Division of Wood Canada Limited (Wood)
3456 Opie CrescentPrince George, BC, CANADA V2N 2P9Tel. (250) 564-3243 Fax (250) 562-7045
BC HYDRO c/o R.F. BINNIE & ASSOCIATES LTD.
Notes:
1. Seepage zones are to be reviewed by a Geotechnical Engineer or their representative at
the time of construction prior to covering with geotextile and drainage blanket.
2. Free-draining drainage blanket is to be a minimum of 1.0m thick or as required by the
Geotechnical Engineer.
3. Drainage blanket should be keyed into cut slopes to accommodate ditch width.
4. The drainage blanket is for control of seepage and potential internal erosion only and
should not be designed to be used as a buttress for additional toe support.
5. Extend drainage blanket laterally and horizontally a minimum 2.0m beyond seepage zone.
6. A geotextile between drainage blanket and general embankment fill (placed adjacent and
downslope of the drainage blanket) may be omitted if the general embankment fill contains
<5% fines (material passing the 0.075mm sieve size).
TYPICAL GRANULAR DRAINAGE BLANKET DETAIL
FOR FILL SLOPE
TYPICAL GRANULAR DRAINAGE BLANKET DETAIL
FOR CUT SLOPE
Recommended Geotextile Specifications
Notes:
Drainage Blanket Gradation
1.593
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 407+910.gszName: 4. Sta. 407+910_(Maximum Normal Reservoir Level_Effective Stress) (No Ditch)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.632
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 407+910.gszName: 5. Sta. 407+910_(Maximum Normal Reservoir Level_Undrained) (No Ditch)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.587
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 407+910.gszName: 6a. Sta. 407+910_(Rapid Drawdown) No ditch (Effective Stress)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.618
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 407+910.gszName: 6b. Sta. 407+910_(Rapid Drawdown) No ditch. (Undrained)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.435
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 7. Sta. 408+050_Full Supply Level_No Berm
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.451
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 8. Sta. 408+050_Full Supply Level_Undrained_No Berm
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
Tau/Sigma
Ratio
Minimum
Strength
(kPa)
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.082
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 9a. Sta. 408+050_Rapid Drawdown_No Berm (Effective Stress)
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.237
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 9b. Sta. 408+050_Rapid Drawdown_No Berm (Undrained)
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
Tau/Sigma
Ratio
Minimum
Strength
(kPa)
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.571
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 4. Sta. 408+050_Full Supply Level_Berm Resize
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.611
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 5. Sta. 408+050_Full Supply Level_Berm Resize_Undrained
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
Tau/Sigma
Ratio
Minimum
Strength
(kPa)
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.242
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 6a. Sta. 408+050_Rapid Drawdown_Fully Specified_Berm Resize (Effective Stress)
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.383
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/7/2019Last Edited By: Sinclair, KimFile Name: 408+050..gszName: 6b. Sta. 408+050_Rapid Drawdown_Fully Specified_Berm Resize (Undrained)
Color Name Model Unit
Weight
(kN/m³)
Cohesion'
(kPa)
Phi'
(°)
Phi-B
(°)
Piezometric
Line
Tau/Sigma
Ratio
Minimum
Strength
(kPa)
C-Horizontal
(kPa)
C-Vertical
(kPa)
Phi-Horizontal
(°)
Phi-Vertical
(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.401
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 7. Sta. 408+120_Full Supply Level_No Berm
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.365
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 8. Sta. 408+120_Undrained_No Berm
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.079
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 9a. Sta. 408+120_Rapid Drawdown_No Berm (Effective Stress)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.178
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 9b. Sta. 408+120_Rapid Drawdown_No Berm (Undrained)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.552
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 4. Sta. 408+120_Full Supply Level_Berm Resize
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.443
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 5. Sta. 408+120_Undrained
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.248
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 6a. Sta. 408+120_Rapid Drawdown_Berm Resize (Effective Stress)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Effective Stress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.372
-50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200420
430
440
450
460
470
480
KX05280503.7
Highway 29. Bear Flat Cache Creek Segment
Date: 5/7/2019
Last Edited By: Sinclair, Kim
File Name: 408+120.gsz
Name: 6b. Sta. 408+120_Rapid Drawdown_Berm Resize (Undrained)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.385
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 7. Sta. 408+200_Full Supply Level_No Berm
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.285
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 8. Sta. 408+200_Full Supply Level_Undrained_No Berm
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.162
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 9a. Sta. 408+200_Rapid Drawdown_No Berm (Effective Stress)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.163
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 9b. Sta. 408+200_Rapid Drawdown_No Berm (Undrained)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.544
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 4 Sta. 408+200_Full Supply Level_Berm Re-size
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.425
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 5. Sta. 408+200_Full Supply Level_Undrained_Berm Re-size
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.331
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 6a. Sta. 408+200_Rapid Drawdown_Berm Re-size (Effective Stress)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi' (°)
Phi-B(°)
PiezometricLine
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (EffectiveStress)_High Plastic
Mohr-Coulomb 19 0 22 0 1
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
1.279
-80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90 100445
450
455
460
465
470
475
445
450
455
460
465
470
475
KX05280503.7Highway 29. Bear Flat Cache Creek SegmentDate: 5/8/2019Last Edited By: Sinclair, KimFile Name: 408+200..gszName: 6b. Sta. 408+200_Rapid Drawdown_Berm Re-size (Undrained)
Color Name Model Unit Weight (kN/m³)
Cohesion'(kPa)
Phi'(°)
Phi-B(°)
PiezometricLine
Tau/SigmaRatio
MinimumStrength (kPa)
C-Horizontal(kPa)
C-Vertical(kPa)
Phi-Horizontal(°)
Phi-Vertical(°)
1. Fill Mohr-Coulomb 21 0 36 0 1
2. Clay/Silt (Undrained)_High Plastic
S=f(overburden) 19 1 0.22 35
3. Weathered Bedrock
Mohr-Coulomb 24.5 0 30 0 1
4. Shale Bedrock Anisotropic Strength 24.5 0 1 50 50 35 45
Geotechnical Assessment and Design
Bear Flat Cache Creek Segment (East)
Project # KX05280503| August 14, 2019
‘Wood’ is a trading name for John Wood Group PLC and its subsidiaries
Limitations
1. The work performed in the preparation of this report and the conclusions presented are subject
to the following:
a. The Standard Terms and Conditions which form a part of our Professional Services
Contract;
b. The Scope of Services;
c. Time and Budgetary limitations as described in our Contract; and
d. The Limitations stated herein.
2. No other warranties or representations, either expressed or implied, are made as to the
professional services provided under the terms of our Contract, or the conclusions presented.
3. The conclusions presented in this report were based, in part, on visual observations of the Site
and attendant structures. Our conclusions cannot and are not extended to include those portions
of the Site or structures, which are not reasonably available, in Wood’s opinion, for direct
observation.
4. Where testing was performed, it was carried out in accordance with the terms of our contract
providing for testing. Other substances, or different quantities of substances testing for, may be
present on-site and may be revealed by different or other testing not provided for in our contract.
5. The utilization of Wood’s services during the implementation of any remedial measures will allow
Wood to observe compliance with the conclusions and recommendations contained in the report.
Wood’s involvement will also allow for changes to be made as necessary to suit field conditions as
they are encountered.
6. This report is for the sole use of the party to whom it is addressed unless expressly stated
otherwise in the report or contract. Any use which any third party makes of the report, in whole or
the part, or any reliance thereon or decisions made based on any information or conclusions in
the report is the sole responsibility of such third party. Wood accepts no responsibility whatsoever
for damages or loss of any nature or kind suffered by any such third party as a result of actions
taken or not taken or decisions made in reliance on the report or anything set out therein.
7. This report is not to be given over to any third party for any purpose whatsoever without the
written permission of Wood.
8. Provided that the report is still reliable, and less than 12 months old, Wood will issue a third-party
reliance letter to parties that the client identifies in writing, upon payment of the then current fee
for such letters. All third parties relying on Wood’s report, by such reliance agree to be bound by
our proposal and Wood’s standard reliance letter. Wood’s standard reliance letter indicates that in
no event shall Wood be liable for any damages, howsoever arising, relating to third-party reliance
on Wood’s report. No reliance by any party is permitted without such agreement.