中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
COMPOSITE MATERIALS METHOD FOR STUDYING MECHANICAL AND DEFORMATION PROPERTIES OF LAYERED SALT ROCK

文献类型:会议论文

作者Wang, A. M.1; Yang, C. H.3; Chen, J. W.4; Zhang, X. Z.2; Huang, Z. Q.1
出版日期2011
会议日期MAY 22-26, 2011
会议地点Shanghai Univ, Shanghai, PEOPLES R CHINA
关键词layered salt rock geological materials Composite materials
页码421
英文摘要In this paper, layered salt rock was seen as the layered composite materials, composite materials method was proposed to study the mechanical and deformation properties of layered rock salt, the sandwich was taken as the "reinforcement" in the laminated Composite materials, and the salt rock was taken as the "Matrix", Then, Creep mechanism of fiber reinforced composite materials and layered rock salt were compared; Dislocation motion from the composite materials was used to analyze stress transfer process, stress concentration and the fracture of layered rock salt, finally, layered rock salt was considered heterogeneous at the microscopic level and continuous and uniform at the macro scale, representative volume element could be adopted to study the effective properties of layered rock salt. The proposed study consideration in this paper provided a new approach for the deformation and mechanical properties of layered rock salt geological materials.
源文献作者Fan, JH ; Zhang, JQ ; Chen, HB ; Jin, ZH
会议录ADVANCES IN HETEROGENEOUS MATERIAL MECHANICS 2011
会议录出版者DESTECH PUBLICATIONS, INC
会议录出版地LANCASTER
语种英语
WOS研究方向Materials Science ; Mechanics
WOS记录号WOS:000297713100104
源URL[http://119.78.100.198/handle/2S6PX9GI/4599]  
专题岩土力学所知识全产出_会议论文
作者单位1.N China Univ Water Resources & Elect Power ;
2.Henan Provincial Coalfield Geol Bureau ;
3.Chinese Acad Sci, Inst Rock & Soil Mech ;
4.China Univ Geosci
推荐引用方式
GB/T 7714
Wang, A. M.,Yang, C. H.,Chen, J. W.,et al. COMPOSITE MATERIALS METHOD FOR STUDYING MECHANICAL AND DEFORMATION PROPERTIES OF LAYERED SALT ROCK[C]. 见:. Shanghai Univ, Shanghai, PEOPLES R CHINA. MAY 22-26, 2011.

入库方式: OAI收割

来源:武汉岩土力学研究所

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