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电阻率三维反演中加权光滑因子的影响及注浆检测应用 被引量:5

Weighted smooth factor impact on 3D DC resistivity inversion and application in grouting effect detection
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摘要 为提高电阻率三维反演效果,提出采用光滑约束构造三维反演函数中粗糙度矩阵的方法并给出了加权光滑因子的表达式,指出加权光滑因子与网格剖分密切相关。利用共轭梯度算法对建立的地电模型进行三维反演数值模拟,分析水平和竖直方向上网格剖分对反演效果的影响。结果表明:光滑因子即网格剖分有相对最佳的选择,对地表数据,水平方向XOY平面应尽量保持等比例剖分;竖直方向XOZ和YOZ平面可以适当增大纵向(Z方向)网格剖分,但剖分比例不宜超过水平方向的4倍。依据模拟结果,应用于电阻率法注浆检测,取得了良好的效果. A smoothness constraint method was used to construct the roughness matrix in 3D inversion function to improve the 3D DC resistivity inversion. The expression of weighted smooth factor was given in detail, showing close relation between weighted smooth factor and the mesh dissection. Using conjugate gradient algorithms was to simulate the 3D DC resistivity inversion of established geoelectric model. The impacts of horizontal and vertical mesh dissection on resistivity inversion were analyzed in this study. The results show that there is an optimum solution in weighted smooth factor (meshed dissection). For the surface data, it should try to keep equal proportional dissection on the XOY plane, and increase dissection of Z direction on the XOZ plane and YOZ plane but the part of dissection proportion should not be more than four times of horizontal direction. Finally, results of simulation of 3D resistivity inversion were applied to detect the grouting effect, achieving very good effects.
出处 《中国矿业大学学报》 EI CAS CSCD 北大核心 2013年第1期88-92,共5页 Journal of China University of Mining & Technology
基金 国家重点基础研究发展计划(973)项目(2007CB209400)
关键词 电阻率三维反演 加权光滑因子 网格剖分 注浆 3D DC resistivity inversion weighted smooth factor~ mesh dissection grouting
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  • 1周熙襄 钟本善.电法勘探数值模拟技术[M].成都:四川科学技术出版社,1986.. 被引量:21
  • 2徐世浙著..地球物理中的有限单元法[M].北京:科学出版社,1994:308.
  • 3胡祖志,胡祥云.大地电磁三维反演方法综述[J].地球物理学进展,2005,20(1):214-220. 被引量:50
  • 4MACK IE R L, MADDEN T R. Three-dimensionalmagnetotelluric inversion using conjugate gradients[J]. Geophys J Int,1993,115(1) :215-229. 被引量:1
  • 5ZHANG J’MACKIE R L. MADDEN T R. 3-D resis-tivity forward modeling and inversion using conjugategradients [J]. Geophysics, 1995,60(5) : 1313-1325. 被引量:1
  • 6NEWMAN G A, ALUMBAUGH D L. Three-dimen-sional magnetotelluric inversion using non-linear con-jugate gradients [J]. Geophys J Int, 2000, 140 ( 2 ):410-424. 被引量:1
  • 7SPICHAK V,POPOVA. Artificial neural network in-version of magnetotelluric data in terms of three-dei-mensional earth macroparameters [J]. Geophys J Int,2000,142(1) :15-26. 被引量:1
  • 8ZHDANOV M S,FANG S,HURSAN G. Electro-magnetic inversion using quasi-linear approximation[J]. Geophysics?2000,65(5) :1501-1513. 被引量:1
  • 9谭捍东,余钦范,John Booker,魏文博.大地电磁法三维快速松弛反演[J].地球物理学报,2003,46(6):850-854. 被引量:66
  • 10YUTAKA SASAKI. 3-D resistivity inversion usingthe finite-element method [J]. Geophysics,1994,59(11):1839-1848. 被引量:1

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