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Investigation of Soil-water Coupled Behavior of Saturated Clay near/at Critical State and Its Application to Deformation and Failure Problems

Investigation of Soil-water Coupled Behavior of Saturated Clay near/at Critical State and Its Application to Deformation and Failure Problems
饱和粘土近/临界状态的土水耦合行为研究及其在变形和破坏问题中的应用
批准号:
06452267
负责人:
ASAOKA Akira
金额:
$4.1万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (B)
财政年份:
1994
资助国家:
日本
项目状态:
已结题
起止时间:
1994 至 1995

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中文摘要
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英文摘要
In order to investigate "time dependent behavior" of normally consolidated/overconsolidated clay, triaxial compression tests and the soil-water coupled analysis employing the sub-loading surface Cam clay model have been carried out. The bifurcation analysis can explain "time dependent behavior" of clays by using pore water migration effect instead of visco-plasticity. The triaxial compression tests carried out in this research showed that : 1) Undrained creep failure occurs due to the change of 1^<st> failure mode to 2^<nd> mode of soil specimen that associated with pore water migration. 2) Overconsolidated clay exhibits progressive failure under constant loading in drained condition due to the absorbed water during testing. It took about 6 hours for the failure of overconsolidated clay specimen. The progressive failure is observed with the fluctuations of axial strain rates against axial strain.Imperfection-sensitive bifurcation of a plane strain saturated soil column with undrained b … More oundaries is investigated by soil-water coupled finite deformation analysis. An initial cosine-curve geometrical imperfection of 2nd mode is applied to the soil specimen. The linear constraint conditions, "no angle change and no direction change" are imposed over the loaded boundary. The soil is assumed to follow the sub-loading surface Cam-clay model. When the load application to the specimen is held at a point near the bifurcation point, load displacement curve starts to deviate from the main path, ultimately approaching unstable 1st mode path. This mode switching due to pore-water migration after the peak in load-displacement curve, that yield low undrained shear strength describes the undrained creep, which is traditionally attributed to visco-plasticity. Similar to the experiment, the increase in axial strain rate against axial strain in heavily overconsolidated soil specimen when the applied load is kept constant, illustrates the initiation of progressive failure due to softening in the highly sheared zones. Less
期刊论文(48)
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会议论文
浅岡 顕 他1名: "Effects of pore water migration on the ultimate behaviour of Soils" Proccedings of 5th international Symposium on Plasticity and lts Current Application(IS' HIROSIMA),JSSFME. 1. 407-410 (1995)
Ken Asaoka 等 1 人:“孔隙水迁移对土壤最终行为的影响”第五届国际塑性研讨会论文集及其当前应用(IS HIROSIMA),JSSFME 1. 407-410(1995)。
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浅岡 顕 他2名: "Soil-water coupled behavior of heavily overconsolidated clay near/at critical state" Soils and Foundations. (1996)
Ken Asaoka 和其他 2 人:“接近/临界状态下严重超固结粘土的土水耦合行为”《土壤与基础》(1996 年)。
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浅岡 顕 他3名: "飽和土の「非排水クリープ」の1考察" 第31回地盤工学研究発表会. (1996)
Ken Asaoka 等 3 人:“饱和土中不排水蠕变的研究”第 31 届岩土工程研究会议(1996 年)。
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浅岡 顕 他2名: "Soil-Water coupled Behaviour of Saturated Clay near/at Critical State" Vol.34 No.1. 91-105 (1994)
Ken Asaoka 和其他 2 人:“临界状态附近饱和粘土的水土耦合行为”Vol.34 No.1 (1994)。
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