By Chin-Fu Tsang
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Sample text
Essentially, for any rock fracture some relationship must exist between the relative displacement between the two surfaces of the fracture and the shear stresses that arise from the resistance to sliding of these surfaces. This relationship specifies the complete strength of the fracture over all possible values of the relative displacement between its surfaces. ) We shall refer to this complete displacement-strength relationship as a reduced Griffith locus. In general, reduced Griffith loci are nonlinear and reflect the properties of the material and the changing geometry of the fracture.
Rapport GE 16, Institut de Mecanique des Fluides, Univ. de Toulouse, France. L. (1984). Thermodynamic coupling of heat and matter flows in near-field regions of nuclear waste repositories. Scientific Basis for Nuclear Waste Management VII, Materials Research Society Symposia Proceedings, Vol. 26, p. 1023-1030. L. (1985). Thermodynamically coupled mass transport processes in a saturated clay. Scientific Basis for Nuclear Waste Management VIII, Materials Research Society Symposia Proceedings, Vol.
Rock Mech. Min. , 16, 23-35. C. R. (1983).