中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Analysis of a microcrack model and constitutive equations for time-dependent dilatancy of rocks

文献类型:期刊论文

作者Chen, Z
刊名GEOPHYSICAL JOURNAL INTERNATIONAL
出版日期2003-11-01
卷号155期号:2页码:601-608
关键词constitutive equation crack growth creep dilatancy microcrack
ISSN号0956-540X
英文摘要Based on experimental observations and theoretical analyses, the author introduces an ideal microcrack model in which an array of cracks with the same shape and initial size is distributed evenly in rocks. The mechanism of creep dilatancy for rocks is analysed theoretically. Initiation, propagation and linkage of pre-existing microcracks during creep are well described. Also, the relationship between the velocity of microcrack growth and the duration of the creep process is derived numerically. The relationship agrees well with the character of typical experimental creep curves, and includes three stages of creep. Then the damage constitutive equations and damage evolution equations, which describe the dilatant behaviour of rocks, are presented. Because the dilatant estimated value is taken as the damage variable, the relationship between the microscopic model and the macroscopic constitutive equations is established. In this way the mechanical behaviour of rocks can be predicted.
语种英语
WOS记录号WOS:000186173500023
出版者BLACKWELL PUBLISHING LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/78983]  
专题中国科学院地质与地球物理研究所
通讯作者Chen, Z
作者单位Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Chen, Z. Analysis of a microcrack model and constitutive equations for time-dependent dilatancy of rocks[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2003,155(2):601-608.
APA Chen, Z.(2003).Analysis of a microcrack model and constitutive equations for time-dependent dilatancy of rocks.GEOPHYSICAL JOURNAL INTERNATIONAL,155(2),601-608.
MLA Chen, Z."Analysis of a microcrack model and constitutive equations for time-dependent dilatancy of rocks".GEOPHYSICAL JOURNAL INTERNATIONAL 155.2(2003):601-608.

入库方式: OAI收割

来源:地质与地球物理研究所

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