This paper deals with the influence of NaCl concentration and mineralogical content on the residual shear strength of soil from a mudstone dominated landslide region. Soil samples were collected from the sliding surface and from intact rock in the landslide area. Samples prepared from powdered, intact rock showed values of residual ɸ about 40% higher than those for samples taken from the sliding surface. Similarly, higher electrical conductivity was observed in the intact rock samples compared with the sliding surface soil. The intact rock showed a reduction in the shear strength when leached with distilled water. This research provides a useful insight into the post failure behaviour of soils comprising NaCl rich pore water and a variety of mineral types.

  • Background and objectives

  • Geological and mineralogical background of the study area

  • Sample collection and preparation

  • Equipment

  • Testing procedure

  • Discussion

  • Conclusion

  • References

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