Technical Papers
Sep 27, 2024

Efficacy of Utilizing Stress-Dependent SWRC in the Analysis of a Footing Resting on an Unsaturated Soil Slope

Publication: International Journal of Geomechanics
Volume 24, Issue 12

Abstract

The response and the safety of geostructures constructed on hilly regions or sloping grounds are receiving increased attention. As the foundation of geostructures resting on slopes is often in the vadose zone, accounting for appropriate properties of partially saturated soil is essential for effective design. Moreover, changes in climatic conditions will adversely affect the load-carrying capacity and the stability of the footing resting on unsaturated slopes. Often, the soil–water retention curve (SWRC) at null stress is adopted but is expected to be affected by various factors, including the stress state of the sample. In the present study, an attempt has been made to demonstrate the effectiveness of using stress-dependent SWRC (SDSWRC) in analyzing a footing resting on a slope exposed to seasonal variations. The SDSWRC along the drying–wetting path determined experimentally was fitted using the standard SWRC model. The key parameters of the SDSWRC, hydraulic conductivity function, and shear strength of unsaturated soils are utilized in numerical modeling. Transient state flux analysis is carried out to mark the effects of SDSWRC in the development of hydraulic response. The stability of an unsaturated slope subjected to a footing load located at a chosen setback distance was assessed under various hydromechanical conditions. The results demonstrate that the seasonal variation, water table position, and net stress significantly influence the stability and the load-carrying capacity of the footing resting on an unsaturated slope.

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Data Availability Statement

All data, models, and codes generated or used during the study appear in the published paper.

Acknowledgments

The authors express gratitude for the financial backing extended by the Science and Engineering Research Board, Department of Science and Technology, India (Grant Nos. SERB/F/4638/2013-14 and CRG/2018/004612), as well as the initial grant from IIT Kanpur (Grant No. 20110145).

Notation

The following symbols are used in this paper:
a, m, n
SWRC fitting parameters in the Fredlund and Xing (1994) model;
B
width of the footing/offset distance of footing from the crest;
c′
Cohesion intercept at zero matric suction;
e
natural number, i.e., 2.71828;
H
height of the slope;
H1
height of the domain at the crest of the slope;
H2
height of the domain at the toe of the slope;
hw
height of the water table from the base;
k
hydraulic conductivity;
ks
saturated hydraulic conductivity;
kvd
vapor conductivity;
kwx, kwy
HCF along x(horizontal) and y(vertical) directions;
m2w
first derivative of SWRC with respect to suction;
N
normal force;
R
radius of slip circle;
T1, T2, T3, T4, T5
monitoring time periods;
ua
pore air pressure;
uw
pore-water pressure;
WT
water table;
α
angle of inclination of water table with horizontal plane;
β
angle of inclination of slope with respect to the horizontal plane;
γw
unit weight of water;
Δl
arc length of slice;
θ
volumetric water content;
θ
first derivative of the Fredlund and Xing SWRC model;
θr
residual volumetric water content;
θs
saturated volumetric water content;
σ
normal stress;
ϕ
angle of internal friction of soil at zero suction level;
ϕb
friction angle of soil obtained on the shear stress–suction plane;
ψ
suction; and
ψAEV
air entry value

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 24Issue 12December 2024

History

Received: Feb 26, 2024
Accepted: Jun 12, 2024
Published online: Sep 27, 2024
Published in print: Dec 1, 2024
Discussion open until: Feb 27, 2025

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Research Scholar, Dept. of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur 208016, India. ORCID: https://orcid.org/0000-0002-3701-2502. Email: [email protected]
Professor, Dept. of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur 208016, India (corresponding author). ORCID: https://orcid.org/0000-0002-1108-3628. Email: [email protected]

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