Technical Papers
Mar 21, 2024

A Closed-Form Equation for Effective Stress of Unsaturated Saline Clay Considering Capillary and Osmosis Effects

Publication: International Journal of Geomechanics
Volume 24, Issue 6

Abstract

The interaction mechanism between matric suction and osmotic suction was clarified through the analysis of certain physicochemical effects on unsaturated saline clay. The Young–Laplace equation for unsaturated saline clay was then derived by considering the contribution of the chemical potential to the Gibbs free energy at the air–solution interface. An effective stress equation for unsaturated saline clay considering the capillary and osmotic effects was obtained by utilizing a soil skeleton stress equilibrium analysis method. The definition and calculation formula for the osmotic efficiency parameter was determined by analyzing the chemical osmotic effect. Finally, the volume deformation and shear strength of unsaturated saline silty clay were tested under different salt content and matric suction conditions, and the validity of the effective stress equation was verified through tests on expansive clay saturated with salt solution. The results indicated that the effective stress–based generalized effective stress equation for unsaturated saline clay, taking into account the effect of the salt solution on the pore liquid pressure, usw, was related to osmotic suction and the osmotic efficiency parameter. The osmotic efficiency parameter is the ratio of change in the surface tension at the air–solution interface to the change in the corresponding osmotic suction, which reflects the strength of the chemomechanical coupling in the micropore space and its smooth transition to the macroscopic scale. In addition, the validation demonstrated that the proposed effective stress equation was able to uniformly describe the mechanical phenomena of unsaturated saline clay. Our findings provide a convenient way to simulate the mechanical behavior of unsaturated clay in saline environments.

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Data Availability Statement

Some or all data, models, or code generated or used during the study are available from the corresponding author upon request.

Acknowledgments

This work was supported by the National Natural Science Foundation of China (Nos. 12362032, 11962016, and 51978320), the Foundation for Innovation Groups of Basic Research in Gansu Province (No. 20JR5RA478), and the Natural Science Foundation of the Gansu Province of China (No. 20JR10RA471). The authors are grateful to the reviewers for their insightful and constructive comments.

Notation

The following symbols are used in this paper:
A
area of air–solution interface;
A~
effective electrostatic attraction between clay particles;
aw
activity of salt solution;
D
fractal dimension;
e
void ratio;
eC
void ratio of sample containing sodium chloride solution;
eS
void ratio of sample containing sodium sulfate solution;
eW
void ratio of sample containing distilled water;
fs
shape factor;
H
pore scale within aggregate;
h
pore scale within clay platelet;
KD
material constant;
m
molality;
N
number of moles in air–solution interface system;
NAir
number of moles of pore air;
NLiquid
number of moles of pore solution;
Nσ
number of moles of the interfacial, or excess number of moles of the air–solution, system;
nl
volume fraction of salt solution in pore;
p
mean principal stress;
pf
peak mean principal stress;
p
Terzaghi’s effective stress;
qf
peak shear stress;
R
gas constant;
R~
effective electrostatic repulsion between clay particles;
r
mean radius of curvature;
S
entropy of air–solution interface system;
Sre
effective saturation;
Sr
saturation;
Srs
residual saturation;
Sσ
entropy of air–solution interface;
s
matric suction;
sσ
entropy per unit area of air–solution interface;
T
absolute temperature;
U
internal energy of air–solution interface system;
Uσ
internal energy of gas–solution interface;
u
pressure;
ua
pore air pressure;
usw
pore liquid pressure caused by salt solution;
uw
pore water pressure;
u¯w
real pore water pressure of unsaturated saline clay;
V
volume of air–solution interface system;
Vla
volume of aqueous solution in the macroscopic pore space;
Vg
volume of air;
VwH
volume of salt solution absorbed in the micropore space;
Vwh
volume of salt solution absorbed by each unit on surface of clay platelet;
Vli
volume of aqueous solution in the microporous space;
Vr
volume of representative element volume;
Vs
volume of clay particles;
Vmw
molar volume of water;
Vσ
volume of air–solution interface;
α
VG model parameters associated with air entry value;
α~
parameter related to contribution of osmotic suction;
β
VG model parameter related to curve shape;
γ
surface tension at the air–water interface;
γ¯
surface tension at the air–solution interface;
δ
unit tensor;
κb(r)
mean curvature function;
μ
chemical potential of interface system;
μa
chemical potential of air–water interface system;
μb
chemical potential of air–solution interface system;
ν
total number of ions after solute ionization;
Π
generalized osmotic pressure;
π
osmotic suction;
πf
final osmotic suction;
πr
reference osmotic suction;
π0
initial osmotic suction;
σ
total stress tensor;
σsk
mean soil skeleton stress tensor;
σ1
vertical stress;
σ1
vertical effective stress;
σ
effective stress tensor;
σ¯
normal stress;
τf
peak shear strength;
τr
residual shear strength;
ϕ
osmotic coefficient of solute;
φs
capillary pressure;
χo
osmotic efficiency parameter;
ψ
Gibbs free energy of air–solution interface system;
ψσ
Gibbs free energy of air–solution interface; and
ω
hydrodynamic membrane efficiency.

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International Journal of Geomechanics
Volume 24Issue 6June 2024

History

Received: Jun 26, 2023
Accepted: Nov 28, 2023
Published online: Mar 21, 2024
Published in print: Jun 1, 2024
Discussion open until: Aug 21, 2024

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Ph.D. Candidate, School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; Institute of Geology of Natural Disaster Prevention, Gansu Academy of Sciences, Lanzhou, Gansu 730000, China. Email: [email protected]
Fengxi Zhou [email protected]
Professor, School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; Engineering Research Center of Disaster Mitigation in Civil Engineering of Ministry of Education, Gansu, Lanzhou, Gansu 730050, China (corresponding author). Email: [email protected]
Xiaolin Cao, Ph.D. [email protected]
School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; Engineering Research Center of Disaster Mitigation in Civil Engineering of Ministry of Education, Gansu, Lanzhou, Gansu 730050, China. Email: [email protected]
Yuwang Liang [email protected]
Ph.D. Candidate, School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China. Email: [email protected]
Institute of Geology of Natural Disaster Prevention, Gansu Academy of Sciences, Lanzhou, Gansu 730000, China. Email: [email protected]

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