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复杂地形条件下激发极化有限单元法三维数值模拟

Three-Dimension Numerical Simulation of Induced Polarization & Finite Element Method Under Complicated Terrain

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【作者】 林家勇汤井田丁茂斌杨晓弘杨树云

【Author】 LIN Jia-yong1,2,3,TANG Jing-tian1,DING Mao-bin1,YANG Xiao-hong1,YANG Shu-yun21.School of Info-physics and Geomatics Engineering,Central South University,Changsha 410083,China2.Geophysics and Geochemistry Institute,Yunnan Geology Survey Academy,Yiliang,Yunnan 652100,China3.Geophysical and Geochemical Exploration Team,Yunnan Geology and Mineral Resources Bureau,Yiliang,Yunnan 652100,China

【机构】 中南大学信息物理工程学院云南省地质调查院物化探勘查所云南省地质矿产开发局地球物理地球化学勘查队

【摘要】 野外激电勘查过程中,据激电异常进行钻探验证时,常发生验证目标矿体擦边而过现象。究其原因是在实际勘查中,地形的起伏变化改变了地下电场的分布规律,导致激电异常发生位移及幅值改变。为了改善、克服这种现状,必须从理论上进行研究。运用四面体单元三维有限单元数值正演计算方法对此进行了理论研究,选用典型山谷地形水平层状极化体模型进行数值模拟计算。研究结果表明:①起伏地形不产生假的激电异常,仅对激电异常的形态和幅值产生影响;②采用四面体剖分单元有限单元法研究复杂地形条件对激电异常的影响是行之有效的。

【Abstract】 It often occurs that drilling according to IP anomaly missed the target.The reason is that in the actual survey,terrain changed the underground electric field,therefor changed and shifted the amplitude of IP anomaly.In order to overcome this problem,three-dimensional tetrahedral finite element numerical method is employed.We prudently selected and simulated a typical geological model.The results show that:①Undulating terrain does not produce a fake IP anomaly,only has an impact on the distribution pattern and the amplitude of IP anomaly;②The tetrahedral finite element method is feasible and effective for the IP simulation under a complicated terrain condition.

【基金】 国家科技支撑项目(2006BAB01A07)
  • 【文献出处】 吉林大学学报(地球科学版) ,Journal of Jilin University(Earth Science Edition) , 编辑部邮箱 ,2010年05期
  • 【分类号】P631.3
  • 【被引频次】10
  • 【下载频次】261
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