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个人信息Personal Information
教授
博士生导师
硕士生导师
任职 : 土木工程学院副院长
性别:男
毕业院校:大连理工大学
学位:博士
所在单位:土木工程系
学科:岩土工程
办公地点:海宇楼215室
联系方式:116024 大连市高新区凌工路2号 大连理工大学土木学院岩土所
电子邮箱:tknian@dlut.edu.cn
Strength behavior of slip-zone soils of landslide subject to the change of water content
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论文类型:期刊论文
发表时间:2013-09-01
发表刊物:NATURAL HAZARDS
收录刊物:SCIE、Scopus
卷号:68
期号:2
页面范围:711-721
ISSN号:0921-030X
关键字:Landslide; Soil mechanics; Slip-zone soil; Shear strength behavior; Water content
摘要:Landslides are the major natural hazards in many countries all over the world and are usually caused by heavy rainfall, water level change of reservoir, excavation, earthquake, etc. Whether the landslide occurs or not in rainfall season, the strength variation of slip-zone soils of landslide is regarded as the vital control factor. Thus, strength behavior for slip-zone soils of landslide subject to the change of water content is required to be evaluated in a potential landslide area. In this paper, the shear strength of typical slip-zone soil, six groups of 25 specimens of remolded clay samples from Daxishan reservoir landslide, was systemically investigated using the improved direct shear test apparatus in order to fully understand its physical and mechanical properties, and also the shear and failure behavior. Furthermore, the fitting equations for expressing the relationship between the shear strength (effective cohesion and internal friction angle) and vertical loadings, initial water contents of slip-zone clay were established based on the experimental results. In particular, a series of shear stress-shear strain curves under various vertical loadings and different water contents were observed. The results show that a "softening" stress-strain behavior is achieved for unsaturated slip-zone soil, while a "hardening" curve is found for saturated slip-zone soil.