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2009:08 Shear-induced Fracture Slip and Permeability Change - Implications for Long-term Performance of a Deep Geological Repository
4703 kB ... A1 A2 A3 C1 C2 C3 repository Section View • • • B1 B2 B3 x z • A1, A2, A3 • B1, B2, B3 • D1, D2, D3 repository Plan View • C1, C2, C3 x y Figure 8. Location ... horizontal stresses are isotropic. Notable anisotropic horizontal compressive stresses (B3 and C3) were observed near the periphery of the repository. The time for maximum compressive stress...
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2009:09 Analysis of three sets of SWIW tracer test data using a two-population complex fracture model for matrix diffusion and sorption
course of the development of the complex fracture model, three different conceptual models, C1, C2 and C3, have been considered to de- scribe how the different populations operate relative to each other. ... the semi-infinite case for large times, when the finite blocks are saturated. Conceptual model C3, proposed by Tsang and Doughty (2009), is the ap- proach used in the present paper. In this model...
Innehållstyp: Dokument
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