Abstract
In this paper, a new concept for rock mass involving distributed discontinuities in the body is proposed. The effect of distributed discontinuities is characterized with a second-order symmetric tensor (the damage tensor). The damage tensor is built in the system of a continuum mechanics theory, and plays a role of transformation operator for the Cauchy stress. Since the damage tensor is introduced as a field variable in addition to stress and strain, one may need one more field equation which governs the propagation of damage. A form of the propagation equation is proposed. The theory is applied to typical problems and the results are compared with ones of other numerical schemes. (Edited author abstract. )
Original language | English |
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Title of host publication | Unknown Host Publication Title |
Publisher | A.A. Balkema |
Pages | 469-480 |
Number of pages | 12 |
ISBN (Print) | 9061915813 |
Publication status | Published - 1985 |