Abstract
The paper presents a computational procedure for reliability analysis of earth slopes considering spatial variability of soils under the framework of the Limit Equilibrium Method. In the reliability analysis of earth slopes, the effect of spatial variability of soil properties is generally included indirectly by assuming that the probabilistic critical slip surface is the same as that determined without considering spatial variability. In contrast to this indirect approach, in the direct approach, the effect of spatial variability is included in the process of determination of the probabilistic critical surface itself. While the indirect approach requires much less computational effort, the direct approach is definitely more rigorous. In this context this paper attempts to investigate, with the help of numerical examples, how far away are the results obtained from the indirect approach from that obtained from the direct approach. In both the approaches, it is required to use a model of discretization of random fields into finite random variables. A few such models are available in the literature for one-dimensional (1D) as well as two-dimensional (2D) spatial variability. The developed computational scheme is based on the First Order Reliability Method (FORM) coupled with the Spencer Method of Slices valid for limit equilibrium analysis of general slip surfaces. The study includes bringing out the computational advantages and disadvantages of the three commonly used discretization models. The sensitivity of the reliability index to the magnitudes of the scales of fluctuation has also been studied.
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Acknowledgments
This research has been supported by the AORC Scheme of the INSPIRE Program of the Department of Science & Technology (DST), Government of India and the first author is employed as a INSPIRE Fellow with DST support. This support is gratefully acknowledged. The writers also thank two anonymous reviewers for their constructive comments and suggestions.
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Metya, S., Bhattacharya, G. Reliability Analysis of Earth Slopes Considering Spatial Variability. Geotech Geol Eng 34, 103–123 (2016). https://doi.org/10.1007/s10706-015-9932-2
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DOI: https://doi.org/10.1007/s10706-015-9932-2