Decomposed granites are often found in Galicia, Spain, where they are referred to as jabres. Similar decomposed granites are also found in many other parts of the world. Granite weathering rarely produces an homogeneous altered rock mass with all material decomposed to the same degree - or even a simple weathering profile where the degree of alteration decreases progressively with depth. This paper presents an empirically based approach that allows estimation of the shear strength of this type of materials in terms of Mohr-Coulomb cohesion and internal friction angle values. The approach is based on back analysis of failed slopes in decomposed granites, and it is implemented through simple in-situ testing and classification of the weathered granite, treating it as a soil material. An advantage of the used approach is that it allows prediction of shear strength values at different locations within the deposit in a quick and economical way, from which average values of shear strength parameters can be computed. This is particularly important when considering the heterogeneous nature of decomposed granite formations in relation to the scale of the engineering work involved. Analysis of three slopes instability cases in jabres in Galicia, illustrating the approach are described in detail. These correspond to a road cut, a natural slope and the wall of an open pit mine.
Bibliographical noteFunding Information:
The authors would like to thank the Spanish Office of Science and Technology for financial support through Contract Reference Number BIA2009-09673 , which funded developments in this paper related to rock mass strength characterization. The authors would also like to thank graduate student Jose Luis Ares Araujo, who assisted in the analysis of the road cut failure described in Section 4.1 .
- Back analysis
- Decomposed granite
- Limit equilibrium
- Mohr-Coulomb shear strength
- Slope stability
- Weathered granite