A study of collapsible and rheological properties of kaolin clay during wetting in 1D consolidation test
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A study of collapsible and rheological properties of kaolin clay during wetting in 1D consolidation test
Vol. 34, Issue 10, (2013)
作者机构:
1. 上海交通大学 船舶海洋与建筑工程学院,上海,200240
2. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都,610059
3. 日本东京理科大学,野田市 2788510
作者简介:
基金信息:
DOI:
CLC:O37
Online First:18 October 2013,
Published:2013
稿件说明:
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DENG Jian-liang, XU Qiang, TATSUOKA Fumio. A study of collapsible and rheological properties of kaolin clay during wetting in 1D consolidation test[J]. 2013, 34(10).
DOI:
DENG Jian-liang, XU Qiang, TATSUOKA Fumio. A study of collapsible and rheological properties of kaolin clay during wetting in 1D consolidation test[J]. 2013, 34(10).DOI:
A study of collapsible and rheological properties of kaolin clay during wetting in 1D consolidation test
Connecting the plastic component and the viscous component in parallel
then connecting these two components and the elastic component in series
yields the three component model
where each component has a unique nonlinear constitutive relation. Based on the three-component model
a elasto-plasto-viscosity model is proposed by considering the effects of wetting on the viscous component and the plastic component. The effects of wetting on the plastic component are described by a decrease in the inviscid yield stress at a fixed irreversible strain
while the effects on the viscous component are described by the increase of the rate-sensitivity coefficient. Both the effects on the two components can be fully determined based on test results. Subsequently
based on this collapse-rheology model
a numerical analysis is performed on the collapse-rheology behavior of Kaolin clay in a 1D consolidation test. In the test
the creep is observed in a dried condition
while the collapse is observed during the stepwise wetting. The water content and strain in the test are precisely measured. The validity of the analysis method is shown by the well simulated water content-strain-time relation and the definite difference between the collapse during wetting and the creep under dried condition.