Technical Papers
Mar 29, 2024

Evolution of Limiting Slope Face in Rock Mass Using the Stress Characteristics Method

Publication: International Journal of Geomechanics
Volume 24, Issue 6

Abstract

The limiting stability of finite rock slopes is assessed in this paper by implementing the stress characteristics method (SCM) alongside the generalized Hoek‒Brown (GHB) yield criterion. By employing the SCM, a set of differential equations governing the equilibrium stress field is derived and later combined with the rock mass failure envelope characterized by the GHB criterion. Subsequently, the limiting slope face (LSF) with a global factor of safety (FS) as unity is obtained to preserve the state of plastic equilibrium. The current approach overcomes the necessity of a preconceived slip surface in the analysis. The resulting curvilinear LSFs exhibit more excellent compatibility with the shape of the naturally occurring slope profiles. The LSFs evolved from this investigation are generally found to be steeper than the traditionally encountered planar slopes without negotiating the mechanical stability. Numerical validation of the current approach using the finite-element limit analysis (FELA) is also established to authenticate the reliability of the present outcomes. The current results are suitably compared with the solutions available in the literature. Design charts are provided in the form of curvilinear slope faces for the ease of practicing rock engineers. Finally, the proposed LSF-based stability concept is applied to two selected case studies reported in the literature.

Practical Applications

Using the nonlinear generalized Hoek‒Brown strength criterion, this study directly determines the rock slope profile required to maintain limiting stability (factor of safety = 1.0). The profile thus derived is referred to as the LSF. The LSF serves as the basis for two potential field applications: designing the optimal rock slope profile and conducting routine stability checks on existing rock slopes. Taking the derived curvilinear LSF as a reference, optimal linear, bilinear, or multilinear/stepped slopes can be designed with a sufficient safety margin. Additionally, the LSF operates as an interface between the zone of stability and instability. Therefore, a simple profile-matching scheme between any existing rock slope and the corresponding LSF can provide the safety status of that existing slope. Therefore, the present design charts containing LSFs contribute to a readymade solution for a rapid and reliable rock slope stability assessment.

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Data Availability Statement

All data used in this study, and the MATLAB code employed for the determination of the response of the system, are available from the corresponding author upon reasonable request.

Acknowledgments

The first author acknowledges the Ministry of Education, Government of India, for the Prime Minister’s Research Fellows (PMRF) doctoral funding.

Notation

The following symbols are used in this paper:
Aa
parameter as defined in Eq. (4);
a
dimensionless HB material parameter as defined in Eq. (2a) representing the characteristics of rock mass;
D
disturbance factor of the rock mass;
d
depth of firm stratum from the base of the slope;
F
function defining the yield criterion in Eq. (6);
f
macroscopic yield condition;
H
any typical scalar function of x and y;
h
height of the rock slope;
k
parameter as defined in Eq. (4);
m
parameter as defined in Eq. (12);
mb
dimensionless HB material parameter as defined in Eq. (2b) related to mi;
mi
Hoek‒Brown constant of intact rock representing the hardness of the rock;
N
stability number, that is, σci/(γh·FS);
Ncr
critical stability number corresponding to FS=1.0;
p
average stress, that is, (σ1 + σ3)/2;
pg
magnitude of p along the top surface of the slope (OG);
ps
magnitude of p along the limiting slope face (OA);
q
uniformly distributed surcharge;
R
radius of the Mohr circle, that is, (σ1σ3)/2;
Rg
magnitude of R along the top surface of the slope (OG);
Rs
magnitude of R along the limiting slope face (OA);
s
dimensionless HB material parameter as defined in Eq. (2c) representing the degree of fragmentation of the rock;
u, v
horizontal and vertical displacement, respectively;
X
body force per unit volume in the x-direction;
x, y
axes in 2D Cartesian coordinate system;
Y
body force per unit volume in the y-direction;
α
horizontal inclination of the ELS;
αL
horizontal inclination of a linear slope, as reported in the literature;
βa
parameter as defined in Eq. (4);
γ
unit weight of the rock mass;
ζa
parameter as defined in Eq. (4);
θ
orientation of the major principal stress about the positive x-axis;
θg
magnitude of θ along the top surface of the slope (OG);
θs
magnitude of θ along the limiting slope face (OA);
μ
parameter as defined in Eq. (12);
ρ
instantaneous friction angle as defined in Eq. (16);
ρg
magnitude of ρ along the top surface of the slope (OG);
ρs
magnitude of ρ along the limiting slope face (OA);
σ+, σ
axes in the 2D curvilinear coordinate system representing the positive and negative characteristics, respectively;
σ1
major principal stress;
σ3
minor principal stress;
σci
uniaxial compressive strength of the intact rock;
σng
normal stress on the top surface of the slope (OG);
σx
normal stress on the x-plane;
σy
normal stress on the y-plane;
τg
shear stress on the top surface of the slope (OG);
τxy
shear stress in the xy-plane; and
ψ
magnitude of θ at OS.

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International Journal of Geomechanics
Volume 24Issue 6June 2024

History

Received: Aug 18, 2023
Accepted: Dec 21, 2023
Published online: Mar 29, 2024
Published in print: Jun 1, 2024
Discussion open until: Aug 29, 2024

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Shibsankar Nandi, S.M.ASCE https://orcid.org/0000-0002-7291-6793
Research Scholar, Dept. of Civil Engineering, Indian Institute of Technology, Kanpur, Kanpur 208 016, India. ORCID: https://orcid.org/0000-0002-7291-6793.
Professor, Dept. of Civil Engineering, Indian Institute of Technology, Kanpur, Kanpur 208 016, India (corresponding author). ORCID: https://orcid.org/0000-0002-9990-0468. Email: [email protected]

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