Abstract
The slope stability analysis has many applications in the engineering projects such as the dams, the roads and open pits structures. The method of analysis is usually based on the equilibrium conditions of the potential plane and wedge failures. The zone of the potential failure is stable whenever the stability forces dominate instability characteristics of the slope. In most of the classic methods of slope stability analysis, the joint surfaces are assumed to be continuous along the potential failure zone. These can cause an underestimated solution to the analysis. In this research the joint trace length is considered to be discontinuous across the potential surface of failure as it happens in nature. Therefore, there exists a rock bridge between the local joint traces. Because of the numerous problems related to the rock slope stability the above assumption is satisfied and the shear strength characteristics of intact rock have taken part in the analysis. The analysis presented here gives a better concept, view, and idea of understanding the physical nature of rock slopes and includes more parameters governing the stability of the potential failure zone.
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References
Abel J F 1990 Rock mechanics. Colorado School of Mine, USA
Coates D F 1967 Rock mechanics principles. Canadian Department of Energy, Mines and Resources, Monograph 874
Goodman R E 1976 Methods of geological engineering in discontinuous rocks. St. Paul: West Publisher
Hoek E, Bray J 1974 Rock slope engineering. (London: Institute of Mine. and Metal.)
Hudson J A, Harrison J P 1997 Engineering rock mechanics: An introduction to the principles. (UK: Pergamon)
Londe D, Vigier G, Vormeringer R 1970 Stability of rock slopes: A three-dimensional study. J. Soil Mechanics and Found. Divi. Proc. Amer. Soc. of Civil Eng.
Priest S D 1985 Hemispherical projection methods in rock mechanics. (London: George Allen & Unwin)
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Zamani, M. A more general model for the analysis of the rock slope stability. Sadhana 33, 433–441 (2008). https://doi.org/10.1007/s12046-008-0028-z
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DOI: https://doi.org/10.1007/s12046-008-0028-z