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断层泥蠕变特性与含水量的关系研究
引用本文:周瑞光,成彬芳,高玉生,杨计申. 断层泥蠕变特性与含水量的关系研究[J]. 力学学报, 1998, 6(3): 217-222
作者姓名:周瑞光  成彬芳  高玉生  杨计申
作者单位:1. 中国科学院地质研究所工程地质力学开放研究实验室,北京100029;2. 水利部天津勘测设计研究院,天津300222
基金项目:国家自然科学基金,中国科学院kz952-j1-003资助
摘    要:断层泥的瞬时力学性质和蠕变特性与含水量关系密切,其力学参数随含水量增加而减少,呈负指数函数关系。界限含水量划分具有很大的意义,某地f246断层泥界限含水量为8%~10%.

关 键 词:断层泥  蠕变  含水量
收稿时间:1997-03-24
修稿时间:1997-08-31

RELATIONSHIP BETWEEN CREEP BEHAVIOR OF FAULT GOUGE AND ITS WATER CONTENTS
Zhou Ruiguang,Cheng Binfang,Gao Yusheng,Yang Jishen. RELATIONSHIP BETWEEN CREEP BEHAVIOR OF FAULT GOUGE AND ITS WATER CONTENTS[J]. chinese journal of theoretical and applied mechanics, 1998, 6(3): 217-222
Authors:Zhou Ruiguang  Cheng Binfang  Gao Yusheng  Yang Jishen
Affiliation:1. Institute of Geology, Academia sinica, Beijing 100029;2. Tianjin Institute for Investigation and Design, Ministry of Water Conservancy, Tianjin 300222
Abstract:The instantaneous mechanical properties and creep behavior of fault gouge are closely related with its water content. Its mechanical parameters will decrease with increasing water content and the relationship between them shows a negative exponential function. Demarcation of water content has great practical significance. The demarcated water content for f 246 gouge in a studied zone is 8 to 10 percents.
Keywords:Fault gouge  Creep  Water content
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