Research on softening rule of direct shear strength parameters
of soil of slide zone in Three-Gorge Reservoir Region caused by water
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Research on softening rule of direct shear strength parameters
of soil of slide zone in Three-Gorge Reservoir Region caused by water
Vol. 27, Issue S1, (2006)
作者机构:
1. 长江科学院 水利部岩土力学与工程重点实验室,湖北,武汉,430010
2. 长江科学院重庆岩基研究中心,重庆,400014
3. 重庆市涪陵区水利电力局, 涪陵,重庆,408000
作者简介:
基金信息:
DOI:
CLC:P642.11+5
Online First:15 December 2006,
Published:2006
稿件说明:
移动端阅览
LI Wei-Shu, XIA Ye, LE Jun-yi. Research on softening rule of direct shear strength parameters
of soil of slide zone in Three-Gorge Reservoir Region caused by water[J]. 2006, 27(S1).
DOI:
LI Wei-Shu, XIA Ye, LE Jun-yi. Research on softening rule of direct shear strength parameters
of soil of slide zone in Three-Gorge Reservoir Region caused by water[J]. 2006, 27(S1).DOI:
Research on softening rule of direct shear strength parameters
of soil of slide zone in Three-Gorge Reservoir Region caused by water
According to the contrastive in-situ direct shear test of the slide zone in the Three-gorges Reservoir Region in different conditions
changed rule of direct shear strength parameters and the value of c andφ which change along with water content about three kinds of soil of slide zone in different water contents conditions
such as clay
silty clay and the earth-rock aggregate
is researched. Experimental relationship between values of c andφ and water conyenton soils of slide zone is established based on plentiful data; and functionary mechanism of different characterized soil of soils zone caused by water is analyzed; then experimental formula of value of c and φ when water is sluiced or water content changes; finally softening degree of direct shear strength parameters caused by water content(water level changing) is quantified .