Gelifluction and Thixotropy of Maritime Antarctic Soils: Small-Scale Measurements with a Rotational Rheometer
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چکیده
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Thixotropy implies non-equilibrium initial conditions after remolding. At the macroscale, thixotropy manifests as the regain in mechanical properties. At the microscale, thixotropy involves phenomena such as contact creep and interparticle force redistribution, homogenization of pore pressure (in saturated and partially saturated soils), altered ionic distribution and mobility, and the effects ...
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ژورنال
عنوان ژورنال: Permafrost and Periglacial Processes
سال: 2016
ISSN: 1045-6740
DOI: 10.1002/ppp.1886