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低延展性裂隙岩体REV存在性研究

Determination of the REV for Fractured Rock Mass of the Low Ductility

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【作者】 张莉丽王云张辛王允于青春

【Author】 ZHANG Li-li1,2,WANG Yun3,ZHANG Xin4,WANG Yun5,YU Qing-chun3 (1.North China Engineering Investigation Institute Co.,Ltd,Shijiazhuang,Hebei 050024,China; 2.College of Geoscience and Surveying Engineering,China University of Mining & Technology,Beijing 100083,China; 3.School of Water Resources and Environment,China University of Geosciences,Beijing 100083,China; 4.Xuzhou Institute of Architectural Technology,Xuzhou,Jiangsu 221116,China; 5.Beijing Huaqing Geothermal Exploitation Company Ltd.,Beijing 102218,China)

【机构】 华北有色工程勘察院有限公司中国矿业大学地球科学与测绘工程学院中国地质大学水资源与环境学院徐州建筑职业技术学院北京市华清地热开发有限责任公司

【摘要】 采用自行开发的离散元软件FractureToKarst,根据国际岩石力学协会对岩石的分类,讨论了低延展性裂隙岩体典型单元体(REV)的存在性及大小,并给出确定其存在性的一般方法。根据研究结果可知,低延展性裂隙岩体REV存在的条件为裂隙平均间距在0.6 m以下,即极密间距、很密间距、密间距和中等间距裂隙岩体存在REV;裂隙平均间距大于0.6 m,即宽间距、很宽间距和极宽间距裂隙岩体不存在REV。

【Abstract】 The FractureToKarst software which is a main analysis tool in this paper and developed by the listed authors,is a DFN(Discrete Fracture Network) software.According to the Standard of Rock Fracture Classification established by ISRM in 1978,this paper discussed the existence and sizes of representative elementary volume(REV) of low-ductility fractured rock masses using the FractureToKarst and proposed a general method to determine the existence of REV.Combined with the existing study of the fractured-rock flow,the major results are concluded as follows:(1)in the rock masses when their average spacing is less than 0.6 m,the REV exists;(2)when their average spacing is more than 0.6 m,the REV does not exist.

【基金】 国家自然科学基金项目(40372134)
  • 【分类号】TU452
  • 【被引频次】3
  • 【下载频次】148
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