Large Strain Consolidation of Unsaturated Soil: Model Formulation and Numerical Analysis
Publication: International Journal of Geomechanics
Volume 23, Issue 9
Abstract
A nonlinear large strain consolidation model for unsaturated soils is presented in this paper. The model uses the Lagrangian–convective coordinate to track the flow of air and water through a deformed layer and the state surface approach to approximate the hydromechanical behavior of unsaturated soils. The model comprises a set of governing equations to integrate the water flow, airflow, and layer consolidation where large strain deformation of the layer occurs. The governing equations were discretized and solved using the finite-difference method, with the solutions verified against the analytical answers. The model was implemented to surcharge preloading studies with a focus on the effects of the initial wet degree of layers on consolidation. The results suggest that the initial wet degree affects the consolidation curves. Higher consolidation settlement occurs in the wet soil layers than in the less-wet layers. In the same layer, the pore air pressure dissipation is completed earlier than the pore-water pressure.
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Data Availability Statement
All data and models that support the findings of this study are available from the corresponding author upon reasonable request. All codes generated or used during the study are proprietary or confidential in nature and may only be provided with restrictions.
Acknowledgments
This work is jointly supported by the China Scholarship Council (CSC) and the University of Adelaide (Grant Number 202010210001).
Notation
The following symbols are used in this paper:
- A1, A2, A3
- coefficients of consolidation for airflow;
- af
- water retention curve fitting parameter;
- ash
- minimum void ratio;
- bsh
- slope of line of tangency;
- Ca1
- matric suction adjustment factor;
- Ca2
- matric suction adjustment factor;
- Cs
- swelling index;
- Caw
- compressibility of water–air mixture, kPa−1;
- Cw
- compressibility of water, kPa−1;
- csh
- curvature of shrinkage curve;
- cv
- coefficient of consolidation, m2/s;
- dMa
- air mass per time, kg/s;
- e
- soil void ratio;
- e0
- initial soil void ratio;
- ea
- air void ratio;
- initial air void ratio;
- ew
- water void ratio;
- initial water void ratio;
- g
- gravitational acceleration, m/s2;
- H
- height of soil layer, m;
- hr
- residual matric suction;
- i
- ith node in horizontal direction;
- hydraulic gradient in horizontal direction, m/m;
- hydraulic gradient in vertical direction, m/m;
- j
- jth node in vertical direction;
- k
- coefficient of permeability;
- permeability of air in dry condition, m/s;
- horizontal permeability of air in dry condition, m/s;
- initial permeability of air in dry condition, m/s;
- horizontal permeability of air, m/s;
- vertical permeability of air, m/s;
- permeability of water in the fully saturated condition, m/s;
- horizontal permeability of water in the fully saturated condition, m/s;
- vertical permeability of water in the fully saturated condition, m/s;
- horizontal permeability of water, m/s;
- vertical permeability of water, m/s;
- L
- spacing of vertical drains, m;
- M
- mesh node count in vertical direction;
- mf
- water retention curve fitting parameter;
- m1
- coefficient of soil volume change with respect to net stress, kPa−1;
- m2
- coefficient of soil volume change with respect to matric suction, kPa−1;
- ma
- air mass flux through the element, kg/m2/s;
- air mass flux in horizontal direction, kg/m2/s;
- air mass flow rate in horizontal direction, kg/s;
- air mass flux in vertical direction, kg/m2/s;
- air mass flow rate in vertical direction, kg/s;
- coefficient of air volume change with respect to net stress, kPa−1;
- coefficient of air volume change with respect to matric suction, kPa−1;
- coefficient of water volume change with respect to net stress, kPa−1;
- coefficient of water volume change with respect to matric suction, kPa−1;
- N
- mesh node count in horizontal direction;
- n
- porosity;
- nf
- water retention curve fitting parameter;
- p
- surcharge load, kPa;
- flow rate of water in horizontal direction, m2/s per m run;
- flow rate of water in vertical direction, m2/s per m run;
- R
- universal gas constant, J/mol/K;
- S
- degree of saturation;
- t
- elapsed time, s;
- Δt
- time-step increment, s;
- Uavg
- average degree of consolidation;
- ua
- excess pore air pressure, kPa;
- standard atmosphere, kPa;
- absolute pore air pressure, kPa;
- excess pore air pressure of node (i, j) at time t, kPa;
- initial excess pore air pressure, kPa;
- uw
- excess pore water pressure, kPa;
- hydrostatic pore water pressure, kPa;
- pore water pressure, kPa;
- excess pore water pressure of node (i, j) at time t, kPa;
- initial pore water pressure, kPa;
- average pore air pressure at time t, kPa;
- average pore water pressure at time t, kPa;
- V0
- initial volume of soil, m3;
- Va
- volume of pore air, m3;
- Vs
- volume of solids, m3;
- Vv
- volume of void, m3;
- Vw
- volume of pore water, m3;
- actual velocity of airflow in horizontal direction, m/s;
- actual velocity of airflow in vertical direction, m/s;
- velocity of soil particles in vertical direction due to airflow, m/s;
- velocity of soil particles in vertical direction due to water flow, m/s;
- apparent velocity of water flow in horizontal direction, m/s;
- apparent velocity of water flow in vertical direction, m/s;
- actual velocity of water in horizontal direction, m/s;
- actual velocity of water in vertical direction, m/s;
- W1, W2, W3
- coefficients of consolidation for water flow;
- ws
- saturated gravimetric water content;
- x
- Abscissa in Lagrangian coordinate;
- Δx
- mesh size in horizontal direction, m;
- y
- ordinate in Lagrangian coordinate;
- Δy
- mesh size in vertical direction, m;
- z
- time-step number;
- Δ
- differential change;
- α
- parameter for time-step increment;
- final volumetric strain of the layer;
- volumetric strain of the layer at time t;
- elevation of element (xt, yt) due to airflow;
- elevation of element (xt, yt) due to water flow;
- θ
- temperature in Kelvin scale, K;
- λ
- parameter for permeability function;
- ρa
- density of air, kg/m3;
- ρ
- density of element, kg/m3;
- σx
- horizontal total stress, kPa;
- σy
- vertical total stress, kPa;
- γw
- unit weight of water, kN/m3;
- ψ
- matric suction; and
- ω
- molecular mass of air, kg/mol.
Superscripts
- a
- pore air;
- s
- soil solid particles; and
- w
- pore water.
Subscripts
- t
- time;
- x
- horizontal direction in Lagrangian coordinate system;
- y
- veridical direction in Lagrangian coordinate system;
- ξ
- veridical direction in convective system;
- 0
- initial condition;
- 1
- with respect to net stress; and
- 2
- with respect to matric suction.
Coordinates
- x
- horizontal axis in Lagrangian coordinate system;
- y
- veridical axis in Lagrangian coordinate system; and
- ξ
- veridical axis in convective system.
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History
Received: Jul 18, 2021
Accepted: Apr 3, 2023
Published online: Jun 30, 2023
Published in print: Sep 1, 2023
Discussion open until: Nov 30, 2023
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