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Amount of secondary deformation, measured when shear-testing laboratory sample of kaolin, is shown to depend largely on its effective stress state; such deformation does not appear to influence basic stress-strain curve for material; secondary deformation data from drained shear tests are decomposed into volumetric and shear components; creep in shear is interpreted as stress-dilatancy phenomenon, and as such may be contrasted with similar relationships which describe process of primary deformation in shear tests. (26407)
Amount of secondary deformation, measured when shear-testing laboratory sample of kaolin, is shown to depend largely on its effective stress state; such deformation does not appear to influence basic stress-strain curve for material; secondary deformation data from drained shear tests are decomposed into volumetric and shear components; creep in shear is interpreted as stress-dilatancy phenomenon, and as such may be contrasted with similar relationships which describe process of primary deformation in shear tests. (26407)
Secondary compression in shear of clays
ASCE J Soil Mech Found Div
Walker, L.K. (author)
1968
22 pages
Article (Journal)
English
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