Technical Papers
Jun 30, 2023

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;
e0a
initial air void ratio;
ew
water void ratio;
e0w
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;
ixw
hydraulic gradient in horizontal direction, m/m;
iξw
hydraulic gradient in vertical direction, m/m;
j
jth node in vertical direction;
k
coefficient of permeability;
kda
permeability of air in dry condition, m/s;
kd,xa
horizontal permeability of air in dry condition, m/s;
kd,ξa
initial permeability of air in dry condition, m/s;
kxa
horizontal permeability of air, m/s;
kξa
vertical permeability of air, m/s;
ksw
permeability of water in the fully saturated condition, m/s;
ks,xw
horizontal permeability of water in the fully saturated condition, m/s;
ks,ξw
vertical permeability of water in the fully saturated condition, m/s;
kxw
horizontal permeability of water, m/s;
kξw
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;
mxa
air mass flux in horizontal direction, kg/m2/s;
m˙xa
air mass flow rate in horizontal direction, kg/s;
mξa
air mass flux in vertical direction, kg/m2/s;
m˙ξa
air mass flow rate in vertical direction, kg/s;
m1a
coefficient of air volume change with respect to net stress, kPa−1;
m2a
coefficient of air volume change with respect to matric suction, kPa−1;
m1w
coefficient of water volume change with respect to net stress, kPa−1;
m2w
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;
qxw
flow rate of water in horizontal direction, m2/s per m run;
qξw
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;
uatma
standard atmosphere, kPa;
uporea
absolute pore air pressure, kPa;
uta(i,j)
excess pore air pressure of node (i, j) at time t, kPa;
u0a
initial excess pore air pressure, kPa;
uw
excess pore water pressure, kPa;
uhydrow
hydrostatic pore water pressure, kPa;
uporew
pore water pressure, kPa;
utw(i,j)
excess pore water pressure of node (i, j) at time t, kPa;
u0w
initial pore water pressure, kPa;
u¯ta
average pore air pressure at time t, kPa;
u¯tw
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;
vxa,act
actual velocity of airflow in horizontal direction, m/s;
vξa,act
actual velocity of airflow in vertical direction, m/s;
vξs,a
velocity of soil particles in vertical direction due to airflow, m/s;
vξs,w
velocity of soil particles in vertical direction due to water flow, m/s;
vxw
apparent velocity of water flow in horizontal direction, m/s;
vξw
apparent velocity of water flow in vertical direction, m/s;
vxw,act
actual velocity of water in horizontal direction, m/s;
vξw,act
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;
εf
final volumetric strain of the layer;
εt
volumetric strain of the layer at time t;
ξt+1a
elevation of element (xt, yt) due to airflow;
ξt+1w
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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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 23Issue 9September 2023

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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Authors

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School of Architecture and Civil Engineering, Univ. of Adelaide, Adelaide, SA 5005, Australia. ORCID: https://orcid.org/0000-0002-5941-0712.
School of Architecture and Civil Engineering, Univ. of Adelaide, Adelaide, SA 5005, Australia (corresponding author). ORCID: https://orcid.org/0000-0002-3897-9803. Email: [email protected]

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