TECHNICAL PAPERS
Jul 1, 1986

Stress Distribution in Anisotropic Compliance of Jointed Rock

Publication: Journal of Geotechnical Engineering
Volume 112, Issue 7

Abstract

In order to determine the deformational response of a rock mass, the rock mass is often considered and characterized as an anisotropic composite material. This compliance is generally defined in terms of deformation; the effects of stress distributions within the rock mass are not considered. Two simple models are used in this paper to define the total rock mass compliance. The one model represents the deformational mode where the stresses within the composite material are equal and the second model represents the stress distributions within the composite material where the strains between the composite material are equal. In addition to neglecting the effects of stress distribution on the compliance of the rock mass, relative volumes of the intact and joint material and their spatial distribution are generally neglected. These relative volumes and their spatial distribution relative to the applied loads are an important part of the rock mass compliance, especially when shear tractions are applied.

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References

1.
Barla, G. (1974). Rock Anisotropy—Theory and Laboratory Testing, International Centre for Mechanical Sciences, L. Muller, Ed., Udine, Springer, Vienna, 132–169.
2.
Chappell, B. A. (1984). “Determination of Rock Mass Modulus,” Fourth Australia‐New Zealand Conference, Geomechanical Institute Engineering Australian, Perth, Australia.
3.
Gerrard, C. M. (1982). “Joint Compliances as a Basis for Rock Mass Properties and the Design of Supports,” Int. J. Rock Mech. Min. Sci. & Geomech. Abstr., 19(6), 285–305.
4.
Jaeger, J. C., and Cook, N. G. W. (1979). Fundamentals of Rock Mechanics, 3rd ed., Methuen and Co. Ltd., London, 137–142.
5.
Kutter, H. K. (1974). Failure Mechanisms of Jointed Rock, International Centre for Mechanical Sciences, L. Muller, Ed., Udine, Springer, Vienna, 96–109.
6.
Reuss, A. (1929). “Berechung der Fliessgrenze von Mischkristallen auf Grund der Plastizitatsbedingung fur Einkristalle,” Z. Agnew Math. Mech., 9(1), 49–58.
7.
Saiamon, M. D. G. (1968). “Elastic Moduli of a Stratified Rock Mass,” Int. J. Rock Mech. Sci., 5(6), 519–527.
8.
Singh, B. (1973). “Continuous Characterization of Jointed Rock Masses. Part 1. The Constitutive Equations,” Int. J. Rock Mech. Min. Sci. and Geomech. Abstr., 10(4), 331–335.
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Voigt, W. (1928). Lehrbuch der Kristallphysik, Taubner, Liepsig.

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Go to Journal of Geotechnical Engineering
Journal of Geotechnical Engineering
Volume 112Issue 7July 1986
Pages: 682 - 700

History

Published online: Jul 1, 1986
Published in print: Jul 1986

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Authors

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Brian A. Chappell
Geotech. Engr. and Research Sci., Bureau of Mineral Resources, P.O. Box 398, Canberra, Australia 2801

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