Article ID Journal Published Year Pages File Type
4676120 Cold Regions Science and Technology 2011 6 Pages PDF
Abstract
► The relaxation process of warm frozen clay consists of three typical stages. ► The magnitude of pre-strain influences the volumetric changes during relaxation. ► Deviatoric stress-time relationship can be well described by a hyperbolic relation. ► Characteristic parameters during relaxation depend on the initial test condition.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth and Planetary Sciences (General)
Preview
Stress relaxation characteristics of warm frozen clay under triaxial conditions
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