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Soil creep as rate process
Fundamental equation of theory of absolute reaction rates adapted for time-dependent soil deformations; this equation supports assumption of thermally activated creep process, predicted relationship between experimental activation energy and creep stress, and predicted stress dependence of creep rate; modification of equation is needed for variation of creep rate with time; techniques for study of deformation mechanisms in soils and test results suggest that interparticle bonding is probably of primary valence type; resistance to shear stresses cannot be accounted for in terms of viscous water films, and interparticle contacts must be effectively solid to solid.
Soil creep as rate process
Fundamental equation of theory of absolute reaction rates adapted for time-dependent soil deformations; this equation supports assumption of thermally activated creep process, predicted relationship between experimental activation energy and creep stress, and predicted stress dependence of creep rate; modification of equation is needed for variation of creep rate with time; techniques for study of deformation mechanisms in soils and test results suggest that interparticle bonding is probably of primary valence type; resistance to shear stresses cannot be accounted for in terms of viscous water films, and interparticle contacts must be effectively solid to solid.
Soil creep as rate process
ASCE -- Proc (J Soil Mechanics Foundation Div)
Mitchell, J.K. (author) / Campanella, R.G. (author) / Singh, A. (author)
1968
23 pages
Article (Journal)
English
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