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• W2083443588 abstract "Under uniaxial or triaxial load, stress inhomogeneties are generated in crystalline rock at point contacts and at boundaries between grains of dissimilar elastic constants. These stress inhomogeneities may be responsible for the extension of dilatant cracks. Theoretical models are developed to study these possibilities. The models predict axial splitting in rocks under uniaxial compression. Application of moderate confining pressures severely limits crack extension and thus inhibits axial splitting. Interaction between cracks, together with these stress inhomogeneities, tends to form a zone of intense deformation inclined 30–40° to the maximum principal stress where larger angles are associated with higher confining pressures. The axially-oriented cracks in such a zone tend to grow towards each other and thus may coalesce to form the diagonal macroscopic fracture found in brittle rocks under triaxial conditions." @default.
• W2083443588 created "2016-06-24" @default.
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• W2083443588 date "1981-06-01" @default.
• W2083443588 modified "2023-09-24" @default.
• W2083443588 title "Some mechanisms of microcrack growth and interaction in compressive rock failure" @default.
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• W2083443588 doi "https://doi.org/10.1016/0148-9062(81)90974-8" @default.
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