首页 | 本学科首页   官方微博 | 高级检索  
     检索      

裂缝诱导HTI双孔隙介质中的裂缝参数分析
引用本文:孔丽云,王一博,杨慧珠.裂缝诱导HTI双孔隙介质中的裂缝参数分析[J].地球物理学报,2012,55(1):189-196.
作者姓名:孔丽云  王一博  杨慧珠
作者单位:1. 清华大学工程力学系, 北京 100084; 2. 中国科学院地质与地球物理研究所, 北京 100029
基金项目:国家重点基础研究发展计划(973计划),国家十二五大型油气田及煤层气开发重大专项子课题
摘    要:裂缝诱导HTI双孔隙介质模型是将一组垂直排列的裂缝系统嵌入到统计各向同性的孔隙岩石基质系统中而建立的.为了研究裂缝参数对地震波在该模型中传播规律的影响,本文分别对裂缝弱度、裂缝孔隙度和裂缝渗透率这三个主要的裂缝参数进行了分析研究.数值结果表明,裂缝诱导HTI双孔隙介质中,裂缝弱度越大,介质的各向异性强度越强;与基质孔隙系统相比,裂缝系统孔隙度对介质等效孔隙度的影响很小,而裂缝系统渗透率的增大则将显著提高介质在裂缝发育方向上的等效渗透率,这符合对裂缝系统"低孔"、"高渗"特性的认识.此外,裂缝系统渗透率的增大也使慢纵波的振幅显著增强.

关 键 词:HTI介质  双孔隙介质  裂缝弱度  裂缝孔隙度  裂缝渗透率  
收稿时间:2010-08-20

Fracture parameters analyses in fracture-induced HTI double-porosity medium
KONG Li-Yun , WANG Yi-Bo , YANG Hui-Zhu.Fracture parameters analyses in fracture-induced HTI double-porosity medium[J].Chinese Journal of Geophysics,2012,55(1):189-196.
Authors:KONG Li-Yun  WANG Yi-Bo  YANG Hui-Zhu
Institution:1. Department of Engineering Mechanics, Tsinghua University, Beijing 100084, China; 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:A fracture-induced horizontal transverse isotropic(HTI) double-porosity medium has been established by embedding a set of vertical fractures into the isotropic porous background rock in previous paper.In this paper,three main parameters of the fracture system,i.e.,fracture compliance,fracture porosity and fracture permeability,are studied to analyze their influence on seismic wave.The results show that the anisotropy increases with growing fracture compliance;comparing with the matrix system,the contribution of fracture porosity to equivalent porosity is small,while the influence of fracture permeability on equivalent permeability is great,which is in accord with the characteristic of low-porosity high-permeability of fracture system.Additionally,increasing fracture permeability can also enhance the amplitude of slow P-wave notably.
Keywords:HTI medium  Double porosity medium  Fracture compliance  Fracture porosity  Fracture permeability
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号