Strength anisotropy of layered soil system

Krishna Murthy, M. ; Sridharan, A. ; Nagaraj, T. S. (1980) Strength anisotropy of layered soil system Journal of the Geotechnical Engineering Division, 106 (10). pp. 1143-1147. ISSN 0093-6405

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Many natural clays acquire the property of cross anisotropy due to the process of sedimentation followed by one-dimensional consolidation. In some other cases, due to rhythmic fluctuations in the conditions of deposition, a layered deposit could be formed, as in the case of a varved clay which has alternate layers of silt and clay.

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