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Assessing the applicability of local and global sensitivity approaches and their practical utility for probabilistic analysis of rock slope stability problems: comparisons and implications

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Abstract

Characterization of properties governing the stability of rock slopes is essential for their design and analysis. Importance ranking of these properties can be obtained by the sensitivity indices that quantifies the extent to which different properties influence the stability of the slopes. This helps the designers to divert major laboratory/in situ investigation resources to evaluate highly ranked properties. Another usage is to perform the probabilistic stability analysis of slopes efficiently by treating low-ranked properties deterministically in the estimation of probability of failure (\({P}_{\mathrm{f}}\)). In this paper, the importance ranking of rock properties affecting the \({P}_{\mathrm{f}}\) of rock slopes prone to different failure mechanisms is performed using local/global sensitivity approaches (L/GSAs) and the accuracy of these approaches was assessed quantitatively. Four slope case studies indicating different structurally and stress-controlled failures were considered, and sensitivity analyses were performed using six different L/GSAs. Accuracy of the approaches was assessed by comparing the importance ranking of properties based on sensitivity approaches to that of the normalized errors, i.e., \({\varepsilon }_{i}\) invoked in the \({P}_{\mathrm{f}}\) by neglecting the uncertainties in these properties. Results indicated the superior accuracy of GSAs as compared to LSAs. Importance ranking was dependent upon the considered slope (failure mechanisms), with some slopes showing higher sensitivities to external parameters and others to inherent rock properties. An important guideline based on the analysis is suggested to consider the properties as deterministic/random variables in the probabilistic analysis. For the slopes with the minimum interaction effects in their sensitivity (planar, wedge, and stress controlled), uncertainties in multiple properties can be neglected based on the allowable error in the \({P}_{\mathrm{f}}\). Further, a dependence of \({\varepsilon }_{i}\) and corresponding importance ranking was observed on the selected value of property of interest (assumed as deterministic) across its domain in the analysis.

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Data availability

The datasets in the current study are available from the corresponding author on reasonable request.

Abbreviations

FOS:

Factor of safety

\({P}_{\mathrm{f}}\) :

Probability of failure

MCS:

Monte Carlo simulation

PEM:

Point estimate method

LSA:

Local sensitivity analysis

GSA:

Global sensitivity analysis

\({\varvec{x}}\) :

Vector of input properties \(\{{x}_{1}, {x}_{2}, ..., {x}_{n}\}\)

\(n\) :

Number of input parameters

\(y\) :

Model output of interest

\(M\) :

Model mapping \({\varvec{x}}\to y\)

\({\mu }_{{x}_{i}}\) :

Mean value of \({x}_{i}\)

\({\sigma }_{{x}_{i}}\) :

Standard deviations of \({x}_{i}\)

\({\varvec{z}}\) :

Vector \({\varvec{x}}\) in the standard normal space

CDF:

Cumulative distribution function

PDF:

Probability density function

\(E()\) :

Expectation operator

\(V()\) :

Variance operator

\(\sim i\) :

[Subscript] All the components of the vector except \({i}^{th}\)

\({F}_{i}\) :

CDF of \({x}_{i}\)

OAT:

One at a time

\(S{I}_{i}\) :

Sensitivity index of \({i}^{th}\) input using OAT method

\(D\) :

Variance of \(y\)

\({S}_{i}\) :

First-order Sobol’s indices of \({x}_{i}\)

\({S}_{{T}_{i}}\) :

Total effect Sobol’s indices of \({x}_{i}\)

HDMR:

High-dimensional model representation

\({\delta }_{i}\) :

Borgonovo’s sensitivity measure of \({x}_{i}\)

\({f}_{{X}_{i}}\left({x}_{i}\right)\) :

PDF of \({i}^{th}\) input parameter

\({f}_{Y}\left(y\right)\) :

PDF of output \(y\)

\({f}_{Y|{X}_{i}}\left(y\right)\) :

PDF of output \(y\) conditioned on \({x}_{i}\)

\({\mathcal{D}}_{{X}_{i}}\),\({\mathcal{D}}_{Y}\) :

Entire domain of \({x}_{i}\) and \(y\), respectively

RSA:

Reliability sensitivity analysis

\({\delta }_{i}^{\mathrm{RSA}}\) :

RSA measure of \({x}_{i}\)

\({\varepsilon }_{i}\left({z}_{0}\right)\) :

Error induced in the estimated \({P}_{\mathrm{f}}\) by assuming \({x}_{i}\) property as deterministic at \({z}_{0}\)

\(\gamma\) :

Unit weight of rock mass

LEM:

Limit equilibrium method

\({k}_{\mathrm{h}}\) and\({k}_{\mathrm{v}}\) :

Horizontal and vertical seismic coefficients, respectively

\(\mathrm{JCS}\) :

Joint wall compressive strength

\(\mathrm{JRC}\) :

Joint roughness coefficient

\({Z}_{\mathrm{w}}\) :

Depth of water in tension crack

\({\phi }_{\mathrm{r}}\) :

Residual friction angle of joints

\({P}_{\mathrm{w}}\) :

Water pressure

RBF:

Radial basis function

ISRM:

International Society of Rock Mechanics

RSM:

Response surface method

LHS:

Latin hypercube sampling

SSR:

Shear strength reduction

GSI:

Geological strength index

UCS:

Uniaxial compressive strength

\({m}_{i}\) :

Hoek–Brown constant for intact rock

\({E}_{i}\) :

Young’s modulus of intact rock

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Appendix

Appendix

1.1 Importance sampling

Importance sampling method is used to obtain a better estimate of \({P}_{f}\) of the system by sampling from a different distribution other than \({f}_{{\varvec{X}}}({\varvec{x}})\) that ensures preferred sampling from the failure region of the output domain leading to faster convergence and reduction in computational costs. The different distribution is known as importance sampling function \(\psi ({\varvec{x}})\).

$${P}_{\mathrm{f},\mathrm{IS}}=\frac{1}{N}\sum_{k=1}^{N}{I}_{\left(Y\le 0\right)}({{\varvec{x}}}^{(k)})\frac{{f}_{{\varvec{X}}}({{\varvec{x}}}^{(k)})}{\psi ({{\varvec{x}}}^{(k)})}$$
(44)

where {\({{\varvec{x}}}^{(1)}, {{\varvec{x}}}^{(2)},\dots ,{{\varvec{x}}}^{(N)}\)} is drawn from \(\psi ({\varvec{x}})\).

In this article, first a FORM analysis is conducted in the standard normal space (\({\varvec{U}}\)) for the rock slopes and design point \({{\varvec{U}}}^{*}\) is obtained. Then, to obtain an efficient importance sampling function, mean of \(n\)-dimensional standard normal distribution (\({\phi }_{n}({\varvec{u}})\)) is shifted to \({{\varvec{U}}}^{*}\) as suggested by Melchers [29]. Thus,

$$\psi \left({\varvec{u}}\right)= {\phi }_{n}\left({\varvec{u}}-{{\varvec{U}}}^{*}\right).$$
(45)

Sampling from \(\psi \left({\varvec{u}}\right)\) will ensure greater sampling density in the failure region. Additionally, approximately 50% of these samples fall under the failure region of the system [29].

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Pandit, B., Kumar, A. & Tiwari, G. Assessing the applicability of local and global sensitivity approaches and their practical utility for probabilistic analysis of rock slope stability problems: comparisons and implications. Acta Geotech. 18, 2615–2637 (2023). https://doi.org/10.1007/s11440-022-01739-7

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