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非平坦地形条件下电阻率三维反演
引用本文:吴小平.非平坦地形条件下电阻率三维反演[J].地球物理学报,2005,48(4):932-936.
作者姓名:吴小平
作者单位:中国科学技术大学地球与空间科学学院,合肥,230026
基金项目:国家自然科学基金(40004005),国土资源部十五重点科技资助项目.
摘    要:本文实现了非平坦地形条件下电阻率三维反演,讨论了几种消除反演中地形影响的方法. 结果表明,只有将地形直接带入反演算法中,进行带地形电阻率三维反演才能有效消除地形影响及其对反演结果的偏差,得到与地下电性结构相符的反演结果.

关 键 词:非平坦地形  电阻率  三维反演  共轭梯度方法
文章编号:0001-5733(2005)04-0932-05
收稿时间:2004-04-19
修稿时间:2005-03-25

3_D resistivity inversion under the condition of uneven terrain
WU Xiao-Ping.3_D resistivity inversion under the condition of uneven terrain[J].Chinese Journal of Geophysics,2005,48(4):932-936.
Authors:WU Xiao-Ping
Institution:University of Science and Technology of China, School of Earth and Space Science, Hefei 230036, China
Abstract:3-D resistivity inversions under the condition of uneven terrain are presented in this study, and several methods for erasing topographic influence in the inversion are discussed. It is shown that only the inversion incorporating topography, in which the topography is directly incorporated into the inversion algorithm, can effectively erase the topographic influence and correct the error in inversion result, obtaining the inverted model in agreement with subsurface geoelectrical structure.
Keywords:Uneven terrain  Resistivity  3_D inversion  Conjugate gradient method
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