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3-D Inversion of Semi-Airborne Transient Electromagnetic Data Based on Decoupled Mesh
被引:3
|作者:
Hui, Zhejian
[1
]
Wang, Xuben
[1
]
Yin, Changchun
[2
]
Liu, Yunhe
[2
]
机构:
[1] Chengdu Univ Technol, Coll Geophys, Chengdu 610059, Peoples R China
[2] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130021, Jilin, Peoples R China
来源:
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
|
2024年
/
62卷
关键词:
Receivers;
Three-dimensional displays;
Iron;
Data models;
Transient analysis;
Surveys;
Solid modeling;
3-D inversion;
decoupled mesh;
node cloud technique;
semi-airborne transient electromagnetic (SATEM);
3D CSEM;
FIELD;
D O I:
10.1109/TGRS.2024.3395628
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:
Semi-airborne transient electromagnetic (SATEM) method is an effective exploration tool in complex environments due to its utilization of unmanned aerial platforms for data collection. With the escalating demands of detection accuracy, the conventional 1-D inversion is no longer sufficient. Over the last two decades, there has been rapid development in 3-D electromagnetic (EM) inversions. SATEM method usually has a substantial number of receiver stations. To obtain accurate 3-D solutions, one has to refine the grids near the receiver points, which causes a huge number of grids and reduces computational efficiency. Thus, computational complexity is one of the primary factors restricting the practicality of 3-D inversions. In this article, we have developed an approach using decoupled meshes. This method uses a series of meshes to parallelly calculate the forward modeling and Jacobian information, with one mesh containing only a subset of receiver points. This scheme aims to decrease the number of grids and improve the efficiency. After that, we map the results to an overarching inversion mesh using the node cloud technique and renew the model parameters. We check our algorithm via both synthetic and field data. Numerical experiments show that the decoupled mesh inversion method can effectively recover the location and resistivities of the anomalies under the complex topography. When compared with the conventional inversion method, the decoupled mesh inversion method can significantly reduce the calculation time.
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页数:11
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