Abstract

Slope failure in highway embankments is common in central Mississippi due to the presence of the Yazoo Formation clays that are highly plastic in nature and experience extreme shrink–swell movement with seasonal moisture variation. The current study presents a performance evaluation of a repaired landslide along a highway exit ramp slope that contains Yazoo clay. It is a 3H:1V slope located along the exit of Sowell road from I55 south, which is around 32.18 km (20 mi) north of downtown Jackson, Mississippi. The slope was rebuilt and reinforced with H-piles and two layers of uniaxial geogrid. Automated soil moisture sensors and water potential probes were installed at the crest and middle of the slope to monitor the moisture content and matric suction variation. An automated rain gauge and vertical inclinometers were installed at the slope site to monitor the real-time rainfall and deformation of the slope. A sliding slope movement was observed near the toe of the slope in October 2018, a few months after the landslide repair of the slope was complete. Based on the instrumentation results, the slope was observed to be fully saturated. Considering both site investigation and field instrumentation results, a back analysis was conducted using the finite-element method in Plaxis 3D and the potential influencing factors and failure states were replicated. Based on the monitoring results, the topsoil of the slope is fully saturated, which is a clear indication of the formation of perched water conditions. The Plaxis 3D flow analysis results indicated that within a 4-month wet rainfall period of monitoring the slope, the progressive rainfall saturated the near-surface soil which reduced the soil’s matric suction significantly. The successive rainfall and buildup of a perched water zone in the slope eventually caused another failure of this recently repaired slope.

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Acknowledgments

The authors sincerely appreciate the contribution of Cindy Smith, P.E. of the Research Division of MDOT in the study. This work was supported by the Mississippi Department of Transportation (MDOT) as State Study 286.

Notation

The following symbols are used in this paper:
A
section area;
C
cohesion;
d
section overall depth;
E
Young’s modulus;
fs
sleeve friction;
ɣ
unit weight;
Ix
moment of inertia;
kx = ky = kz
permeability;
n, α, m
Van Genuchten fitting parameters;
qt
tip resistance;
u2, u0
pore pressure;
θres
residual water content;
θsat
saturated water content;
ν
Poisson’s ratio;
ξint
strength reduction factor;
ϒsat
saturated unit weight;
ϒunsat
bulk unit weight; and
ϕ
friction angle.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 22Issue 1January 2022

History

Received: Dec 2, 2020
Accepted: Sep 11, 2021
Published online: Nov 10, 2021
Published in print: Jan 1, 2022
Discussion open until: Apr 10, 2022

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Associate Professor, Dept. of Civil and Environmental Engineering, Jackson State Univ., 1400 J.R. Lynch St., JSU Box 17068, Jackson, MS 39217-0168 (corresponding author). ORCID: https://orcid.org/0000-0002-0150-6105. Email: [email protected]
Graduate Research Assistant, Dept. of Civil and Environmental Engineering, Jackson State Univ., 1400 J.R. Lynch St., JSU Box 17068, Jackson, MS 39217-0168. ORCID: https://orcid.org/0000-0001-8457-7234. Email: [email protected]
Mike Stroud [email protected]
Geotechnical Design Engineer, Geotechnical Engineering Dept., Mississippi Dept. of Transportation, 401 North West St., Jackson, MS 39201. Email: [email protected]
Sean Ferguson [email protected]
Senior Geotechnical Engineer, Geotechnical Engineering Associates, LLC, 1647 West Government Cove, Brandon, MS 39042. Email: [email protected]
John Ivoke, S.M.ASCE [email protected]
Graduate Research Assistant, Dept. of Civil and Environmental Engineering, Jackson State Univ., 1400 J.R. Lynch St., JSU Box 17068, Jackson, MS 39217-0168. Email: [email protected]

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