Small and Large Strain 1D 2D 3D Consolidation_Fredlund

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Small and Large-strain 1D/2D/3D Consolidation Murray Fredlund, PhD, PEng SoilVision Systems Ltd. Nov. 4rth, 2009 Tailings and Mine Waste Conference Banff, Canada

description

Geotechnical engineering, consolidation problem, Uni axial, Biaxial and triaxial consolidation of soils

Transcript of Small and Large Strain 1D 2D 3D Consolidation_Fredlund

Page 1: Small and Large Strain 1D 2D 3D Consolidation_Fredlund

Small and Large-strain1D/2D/3D Consolidation

Murray Fredlund, PhD, PEngSoilVision Systems Ltd.

Nov. 4rth, 2009Tailings and Mine Waste Conference

Banff, Canada

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Overview• Introduction• Benchmarking / Verification• Why 2D and 3D analysis?• Layered tailings pit analysis• Conclusions

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History• SOIL MECHANICS AND FOUNDATION ENGINEERING

EDUCATION IN 1949– Scope of field limited mainly to:

• Soil Classification• Capillarity and seepage• Stress analysis by elasticity• Consolidation and settlement analysis• Shear strength• Slope stability• Lateral pressures• Bearing capacity• Shallow and deep foundations

– Emphasis largely on saturated clays and sands

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History• Tower of Pisa

• Consolidation problemshave been with us for awhile

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Terzaghi Consolidation• Terzaghi proposed 1D small-strain

formulation a long time ago (1923, 1936)

• Problem is central to geotechnicalengineering practice

• Why has progress been so slow?– Coupling mechanism is inherently

mathematically very unstable

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Core Problem• Need to solve

– Stress / deformation (Large-strain)– Fluid flow (continuity)

3. PWP increase

1. Apply load

2. Deformations4. PWP dissipates

5. Load transferred toeffective stress

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Coupling• If true coupling is not properly handled

between the fluid andstress/deformation equations then theresults vary

• Uncoupled solutions do not produce thesame result as coupled solutions

• The difference between coupled anduncoupled in consolidation analysis issignificant

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Terzaghi Consolidation• Formulation research has been slow at best

and is mathematically complex

• SoilVision research has been in the area of1D, 2D, 3D small and large strain

Researcher Type Saturation 1D 2D 3D

Terzaghi Small-strain Saturated

Biot; Mendel Small-strain Saturated

Fredlund & Dakshanamurthy Small-strain Unsaturated

Gibson; Schiffman; Townsend Large-strain

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Formulations/Benchmarks• Significant work on small-strain coupled formulations

has been previously published by Biot (saturated),Mendel (saturated), Fredlund (unsaturated) andmany others

• Work on large-strain coupled consolidation has beenpublished by Schiffman, Gibson, Townsend, andothers

• Townsend published a series of 4 1D benchmarksand compared about 8 academic codes for eachbenchmark

• The Townsend benchmarks have been examined bySVS for the purposes of code comparison

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Comparisons Uncoupled solutions will not include lateral

effects of deformation Mendel-Cryer effect

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Comparisons Mandel-Cryer effect can be duplicated Varies based on Poisson’s Ratio

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

0.0 0.2 0.4 0.6 0.8 1.0

No

rm

al i

zed

Po

re

-Wa

t er

Pr

es

sur

e

Normalized Time

PR=0.49 PR=0.35 PR=0.05

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Formulations• Formulations needed:

– 1D, 2D, 2D Axisymmetric, 3D• Elastic, Nonlinear elastic• Ksat, k as a function• Formulations are completed and working well

Elastic Non-linear elastic

Fixedmesh

Movingmesh

Fixedmesh HM

Movingmesh HM

Fixedmesh

Movingmesh

Fixedmesh HM

Movingmesh HM

1D

2D

2D Axisymmetric

3D

* HM - hydrological and mechanical coupling

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Formulations/Benchmarks• Moving mesh / Lagrangian analysis• Difficult to find literature• Complex to benchmark results

No mesh updatingDeformation=0.5

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Formulations - Uncoupled• Lagrangian

– Pure Lagrangiandeformation = 0.40

– Lagrangian-Eulariandeformation = 0.33

– Non-lagrangiandeformation =0.5

– Non-lagrangian OVERESTIMATESdeformations

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Formulations/Benchmarks• Townsend scenario A: Time=1 year• Benchmark is reasonable

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Formulations/Benchmarks• Townsend Scenario A: Time=1 year

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Formulations/Benchmarks• Townsend Scenario A• Poisson’s ratio (0.3)• Ambiguity in boundary conditions

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Solution - Runtimes• Expected run-times for numerical models are

important• The risk is that run-times will become too long

to complete projects in a reasonable time• Extended support for multi-processors has

been added• This has implications on speed

Non-linear compression example (uncoupled - moving mesh)v6.01

Dimension Nodes

Runtime(minutes) P4-Quad 2.4GHz -1 Core(s)

Runtime (minutes)P4-Quad 2.4GHz - 2Core(s)

Runtime (minutes)P4-Quad 2.4GHz - 4Core(s)

Time(minutes)/node

1D 201 0.62 1.09 1.22 0.00312D 1335 4.72 4.43 3.72 0.00282D Axisymmetric 1758 8.45 8.52 8.45 0.00483D 274 8.87 7.47 4.62 0.0168

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Example Application – Pit• Sequenced tailings may be placed in

the pit as successive layers

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Pit Filling• An example model in 2D

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Differences

• Non-lagrangian solutions will OVER-ESTIMATE DEFORMATIONS– Easily demonstrated by SVS research

• Non-coupled solutions will most likelyUNDER-ESTIMATE PORE-WATERPRESSURES– If coupling is not properly performed it can

also lead to errors in solutions

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Benefits• Benefits to the approach include:

– Formulation is theoretically correct anddefensible for reviewers

– Truly coupled solution can demonstrate theMendel-Cryer effect

– 2D and 3D solutions are stable anddemonstrate reasonable run-times

– Layered solutions work well– Reasonable for application to tailings projects

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Thank you…!