井下钻孔电阻率法典型地电模型三维正演模拟
3D forward modeling of typical geo-electric model with borehole resistivity method
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摘要: 为了有效探测工作面底板水害发育情况,保证安全回采,采用井下钻孔电阻率法三维有限元对典型导含水地质异常体模型进行正演模拟;研究了全空间三维有限元正演理论,分析了不同装置类型的电位分布规律,建立了断层、陷落柱、采空区地电模型并进行三维有限元正演模拟,研究了不同地质异常体模型的电位分布情况。模拟结果表明:电位分布呈现低阻区域稀疏而高阻区域稠密的特点,电位梯度呈现低阻区域变小而高阻区域变大的规律;采用井下钻孔电阻率法探测底板水害更贴近目标体,模拟效果好。Abstract: In order to effectively detect the development of water damage in the working face floor and ensure the safety of mining, three-dimensional finite element method of borehole resistivity method is used to carry out forward simulation for the model of typical water-bearing abnormal body. In this paper, three-dimensional finite element forward modeling theory of the whole space is studied, the potential distribution rules of different types of devices are analyzed, the geo-electric models of fault, collapse column and goaf are established, and the three-dimensional finite element forward modeling is carried out, and the potential distribution of different geologic abnormal body models is studied. The simulation results show that the potential distribution is characterized by sparse in low resistance region and dense in high resistance region, and the potential gradient is characterized by the law that the low resistance region becomes smaller and the high resistance region becomes larger. It is more close to the target body to detect the floor water damage by borehole resistivity method. The simulation effect of 3D forward modeling is good.
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Keywords:
- mine resistivity method /
- geo-electric model /
- finite element /
- forward modeling /
- potential isoline
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[1] Rücker C, Günther T, Spitzer K. Three-dimensional modelling and inversion of dc resistivity data incorporating topography-I. Modelling[J]. Geophysical Journal International, 2006, 166: 495-505. [2] Li Y G, Spitzer K. Three-dimensional DC resistivity forward modelling using finite elements in comparison with finite-difference solutions[J]. Geophysical Journal International, 2002, 151: 924-934. [3] 吴小平,汪彤彤.利用共轭梯度算法的电阻率三维有限元正演[J].地球物理学报,2003,46(3):428. WU Xiaoping, WANG Tongtong. 3D finite element forward modeling of resistivity using conjugate gradient algorithm[J]. Journal of Geophysics, 2003, 46(3): 428.
[4] 刘志新.矿井直流电法三维有限元数值算法研究[D].徐州:中国矿业大学,2002. [5] 黄俊革.三维电阻率/极化率有限元正演模拟与反演成像[D].长沙:中南大学,2003. [6] 吕玉增.地-井、井-地IP三维快速正反演研究[D].长沙:中南大学,2008. [7] 欧东新,王超,闫凯暄,等.电导率线性变化直流电测深三维有限单元法正演模拟[J].桂林理工大学学报,2019,39(3):606-614. OU Dongxin, WANG Chao, YAN Kaixuan, et al. Three dimensional finite element forward modeling of linear variation of conductivity in DC electrical sounding[J]. Journal of Guilin University of technology, 2019, 39(3): 606-614.
[8] 鲁晶津.地球电磁三维数值模拟的多重网格方法及其应用研究[D].合肥:中国科学技术大学,2010. [9] 任政勇,汤井田.基于局部加密非结构化网格的三维电阻率法有限元数值模拟[J].地球物理学报,2009, 52(10):2627-2634. REN Zhengyong, TANG Jingtian. Finite element numerical simulation of 3D resistivity method based on locally densified unstructured grid[J]. Journal of Geophysics, 2009, 52(10): 2627-2634.
[10] 范翠松.基于有限元法的复电阻率正反演研究及应用[D].长春:吉林大学,2013. [11] 刘海飞,柳杰,高寒,等.五极纵轴激电测深三维有限元正演模拟[J].吉林大学学报(地球科学版),2016,46(3):884-892. LIU Haifei, LIU Jie, GAO Han, et al. 3D finite element forward modeling of five pole longitudinal IP sounding[J]. Journal of Jilin University(Geoscience Edition), 2016, 46(3): 884-892.
[12] 阮百尧,熊彬.电导率连续变化的三维电阻率测深有限元模拟[J].地球物理学报,2002,45(1):131-138. RUAN Baiyao, XIONG Bin. Finite element simulation of 3-D resistivity sounding with continuous change of conductivity[J]. Journal of Geophysics, 2002, 45(1): 131-138.
[13] 徐世浙.地球物理中的有限单元法[M].北京:科学出版社,1994. [14] 杨军.地球电磁场的连续与间断有限元三维数值模拟[D].合肥:中国科学技术大学,2016. [15] 刘志新,许新刚,岳建华.矿井电法三维有限元正演模拟[J].物探化探计算技术,2003,25(4):302-307. LIU Zhixin, XU Xxingang, YUE Jianhua. 3D finite element forward modeling of mine electrical method[J]. Geophysical and geochemical exploration calculation technology, 2003, 25(4): 302-307.
[16] 刘洋.基于非结构网格的电阻率三维正反演及其应用研究[D].合肥:中国科学技术大学,2016. [17] 乔中林.直流电法三维正演多重网格算法研究[D].北京:中国地质大学(北京),2007. [18] 欧东新,阮百尧.电性轴对称分布电阻率测井的有限元法模拟[J].桂林工学院学报,2002(2):123-128. OU Dongxin, RUAN Baiyao. Finite element simulation of electrical axisymmetric distribution resistivity logging[J]. Journal of Guilin Institute of technology, 2002(2): 123-128.
[19] 韩思旭,欧东新,李勇.修正的点源二维直流电测深有限元模拟[J].桂林理工大学学报,2010,30(4):518-521. HAN Sixu, OU Dongxin, LI Yong. Modified finite element simulation of point source 2D DC sounding[J]. Journal of Guilin University of technology, 2010, 30(4): 518-521.
[20] 刘海飞,阮百尧,柳建新,等.起伏地形电导率连续变化的三维激电数据有限元数值模拟[J].物探化探计算技术,2008,30(4):308-313. LIU Haifei, RUAN Baiyao, LIU Jianxin, et al. Numerical simulation of 3D IP data for continuous change of conductivity in undulating terrain[J]. Geophysical and geochemical exploration calculation technology, 2008, 30(4): 308-313.
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