soil constitutive models in rocscience tools · with more soil-specific constitutive models now...

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Abstract The library of material models in RS 2 has been expanding, with more soil-specific constitutive models now included in the package. On top of the built-in constitutive models, RS 2 has the ability to extend its material model library by using a DLL file that includes user-defined material models. The default DLL file in RS 2 includes the “Hardening Soil” and “Hardening Soil with Small Strain Stiffness” models of PLAXIS, and the “ChSoil,” “CySoil” and “Double- Yield” models of FLAC. This article will demonstrate some applications of such models. In this article the “Softening Hardening” and the “Hardening Soil” models in RS 2 will be used in the simulation of a deep excavation in Berlin, Germany (Nikolinakou et. al., 2011). The “Hardening Soil” model and the “Softening Hardening” model Three key aspects of the mechanical behaviour of soils are: the plastic deformation or yielding starts at the early stages of loading; the stiffness is proportional to the level of confinement; and, the volumetric behaviour exhibited consists of compaction followed by a possible dilation under shear loading. Considering these three features, the material models used in the following simulations utilize three respective formulations: a continuous yielding and hardening behaviour; a nonlinear elastic behaviour in which the Young’s modulus is related to the level of stress; and, an appropriate flow rule that can capture compaction and dilation of the volumetric behaviour of soils. The “Hardening Soil” and the “Softening Hardening” models will be used to simulate the behaviour of Berlin sand in the following sections. Site Characteristics The deep excavation studied is in the M1 pit from the VZB tunneling project in Berlin. The pit was excavated underwater to a depth of 20 metres, and supported by a diaphragm wall. Soil constitutive models in Rocscience tools 1 Figure 1 - M1 pit deep excavation location (Nikolinakou M. A., Whittle, Savidis, & Schran, 2011) The site soil (Berlin sand) is characterized as saturated glacier deposits from three different deposition periods. The vertical soil profile consists of one fill layer (3-4 m thick) overlying three layers of sandy tills, including S0 (6 m thick with 1 m thick organic soil), S1 (10 m thick), and S2 (below the depth of 22 m) (Nikolinakou et. al., 2011).

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AbstractThe library of material models in RS2 has been expanding, with more soil-specific constitutive models now included in the package. On top of the built-in constitutive models, RS2 has the ability to extend its material model library by using a DLL file that includes user-defined material models. The default DLL file in RS2 includes the “Hardening Soil” and “Hardening Soil with Small Strain Stiffness” models of PLAXIS, and the “ChSoil,” “CySoil” and “Double-Yield” models of FLAC. This article will demonstrate some applications of such models. In this article the “Softening Hardening” and the “Hardening Soil” models in RS2 will be used in the simulation of a deep excavation in Berlin, Germany (Nikolinakou et. al., 2011).

The “Hardening Soil” model and the “Softening Hardening” modelThree key aspects of the mechanical behaviour of soils are: the plastic deformation or yielding starts at the early

stages of loading; the stiffness is proportional to the level of confinement; and, the volumetric behaviour exhibited consists of compaction followed by a possible dilation under shear loading. Considering these three features, the material models used in the following simulations utilize three respective formulations: a continuous yielding and hardening behaviour; a nonlinear elastic behaviour in which the Young’s modulus is related to the level of stress; and, an appropriate flow rule that can capture compaction and dilation of the volumetric behaviour of soils. The “Hardening Soil” and the “Softening Hardening” models will be used to simulate the behaviour of Berlin sand in the following sections.

Site CharacteristicsThe deep excavation studied is in the M1 pit from the VZB tunneling project in Berlin. The pit was excavated underwater to a depth of 20 metres, and supported by a diaphragm wall.

Soil constitutive models in Rocscience tools

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Figure 1 - M1 pit deep excavation location (Nikolinakou M. A., Whittle, Savidis, & Schran, 2011)

The site soil (Berlin sand) is characterized as saturated glacier deposits from three different deposition periods. The vertical soil profile consists of one fill layer (3-4 m thick) overlying three layers of sandy tills, including S0 (6 m thick with 1 m thick organic soil), S1 (10 m thick), and S2 (below the depth of 22 m) (Nikolinakou et. al., 2011).

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Model Setup in RS2

This RS2 model includes three primary layers of sand depositions, ignoring secondary fill and organic soil. The material properties of the three layers of sands are presented in Tables 1 and 2 for the “Hardening Soil” and “Softening Hardening” models, respectively.

A 1.5 m thick diaphragm wall extends to 28.7 metres below the ground soil, and it is supported by a row of pre-tensioned tiebacks. The water table is at a depth of 2 m, and ponded water pressure is used to model underwater excavation.

Figure 2 - Initial Stage

Table 1. Hardening Soil model parameters for Berlin sands

Figure 3 - Final Stage Excavation

The elastic behaviour of the “Softening Hardening” model is set to match the same elastic behaviour of the “Hardening Soil” model by using its E50 properties. The strength characteristics, including friction angle, cohesion, and tensile strength, are also the same for the two models. The hardening parameter of the “Softening Hardening” model is set so that the two material models predict very similar behaviour for Berlin sands in drained and undrained triaxial test simulations as shown in Figures 4 and 5 for Sand I. The major difference between the two models is that the “Hardening Soil” model has a cap yield surface in its formulations at a cost of having more material parameters as listed in Table 3.

CHARACTERISTICS SAND I SAND II SAND III

(kPa) 100 100 100

(MPa) 40 105 100

(Ma) 120 315 300

(MPa) 40 105 100

0.5 0.5 0.5

Poisson’s Ratio 0.25 .25 0.25

.43 .38 .38

(degrees) 35 39 39

(degrees) 5 8 8

(kPa) 1.0 1.0 1.0

Failure Ratio 0.9 0.9 0.9

Tensile Strength (kPa)

0 0 0

Results and DiscussionsThe horizontal displacement of the diaphragm wall was measured after both the bolt installation and the final stage of excavation. The following compares the simulations from the RS2 “Hardening Soil” model, RS2 “Softening Hardening” model, the PLAXIS “Hardening Soil” model reported by Nikolinakou et. al. 2011, and the observed behaviour.

In the first case, after installing the bolt (Figure 6), the PLAXIS and RS2 models are identical for the case of the “Hardening Soil” model but both give lower bound estimation compared to the observed behaviour. The “Softening Hardening” model predicts more accurate results at this stage.

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Table 2. Softening Hardening model parameters for Berlin sands

Table 3. Number of model parameters for Hardening Soil model and Softening Hardening model

CHARACTERISTICS SAND I SAND II SAND III

(kPa) 100 100 100

(MPa) 40 105 100

0.5 0.5 0.5

Poisson’s Ratio 0.25 0.25 0.25

(degrees) 35 39 39

zero dilation angle 30.75 32.45 32

(kPa) 1.0 1.0 1.0

Hardening Parameter 0.0004 0.00025 0.0001

Tensile strength (kPa) 0 0 0

CONSTITUTIVE MODEL NUMBER OF PARAMETERS

Hardening Soil with Small Strain Stiffness 14

Hardening Soil 12

Softening Hardening with Nonlinear Elasticity 9

Softening Hardening with Linear Elasticity 7

Figure 4 – Comparison of simulation results using Softening Hardening and Hardening Soil models; Drained triaxial compression test starting at confinement of 50 kPa

In the second case, after the final excavation (Figure 7), the PLAXIS and RS2 models are identical for the case of the “Hardening Soil” model and they both predict more accurate results than the previous case (Figure 6). The prediction by the “Softening Hardening” model is also reasonable. All models predict higher values of displacement at the bottom of the wall, but again the predicted results are in close agreement with the observed behaviour.

ConclusionThis article serves as an effective example of finite element simulations in soils using RS2. The focus was to select constitutive models that best represented the behaviour of the soils in the Berlin sand case and carry out a finite element simulation that provided accurate predictions. Through modeling the deep excavation in Berlin sand, the “Softening Hardening” and “Hardening Soil” models were shown to provide reliable predictions for the behaviour of sands.

ReferencesNikolinakou, M. A., Whittle, A. J., Savidis, S., & Schran, U. (2011). Prediction and Interpretation of the Performance of a Deep Excavation in Berlin Sand. Journal of Geotechnical and Geoenvironmental Engineering, 1047-1048.

Pietruszczak, S. (2010). Fundamentals of Plasticity in Geomechanics. CRC Press.

Azami, A., Yacoub, T., Curran, J., A practical constitutive model for sands (2015). 68th Canadian Geotechnical Conference, GéoQuébec 2015.

Hardening Soil

Softening Hardening

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Figure 5 – Comparison of simulation results using Softening Hardening and Hardening Soil models; Undrained triaxial compression test starting at confinement of 50 kPa

Figure 6 - Horizontal displacement of the diaphragm wall after tensioning the bolt

Figure 7 - Horizontal displacement of the diaphragm wall at the final excavation stage

Hardening Soil

Softening Hardening