Three-dimensional adaptive finite-element method for time-domain airborne EM over an anisotropic earth

被引:9
作者
Qi YanFu [1 ,2 ]
Li Xiu [1 ]
Yin ChangChun [2 ]
Qi ZhiPeng [1 ]
Zhou JianMei [1 ]
Sun NaiQuan [1 ]
Liu YunHe [2 ]
Zhang Bo [2 ]
机构
[1] Changan Univ, Coll Geol Engn & Geomat, Xian 710054, Peoples R China
[2] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130021, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2020年 / 63卷 / 06期
关键词
Time-domain airborne EM; Anisotropy; Adaptive finite element; 3D forward modeling; Abnormal recognition; SUPERCONVERGENT PATCH RECOVERY; LOOP-SOURCE; DIFFERENCE; INVERSION; WAVE;
D O I
10.6038/cjg2020N0031
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
How to generate a reasonable mesh for the anisotropic medium model with complex electrical structure is the key to obtaining high-precision modeling results. In this paper, we study the adaptive finite-element (FE) method for 3D time-domain airborne EM modeling over an anisotropic earth. By combining the time-domain unstructured FE algorithm and the adaptive mesh refinement technology, we successfully realize the 3D time-domain airborne EM adaptive forward modeling for anisotropic media. To deal with the big difference of EM responses at different time channels, we bring in a temporal weighting to achieve a synchronous refinement of shallow and deep meshes. The reliability of our algorithm is verified by comparing our results with 1D semi-analytic solution. The numerical experiments show that the anisotropic conductivity has a big influence on the mesh refinement. The value of the maximum principal-axis conductivity and its distribution directly determines the mesh refinement. In addition, anisotropic conductivity can also seriously affect the distribution pattern and anomalous amplitude of the three-component EM responses. By using the polarity maps for full-domain apparent resistivity, the direction of the anisotropic principal axis can be well identified.
引用
收藏
页码:2434 / 2448
页数:15
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