A New Inversion Method Based on Distorted Born Iterative Method for Grounded Electrical Source Airborne Transient Electromagnetics

被引:31
作者
Liang, Bingyang [1 ]
Qiu, Chen [1 ]
Han, Feng [1 ]
Zhu, Chunhui [1 ]
Liu, Na [1 ]
Liu, Hai [1 ]
Liu, Fubo [2 ]
Fang, Guangyou [2 ]
Liu, Qing Huo [3 ]
机构
[1] Xiamen Univ, Inst Electromagnet & Acoust, Dept Elect Sci, Xiamen 361005, Peoples R China
[2] Chinese Acad Sci, Inst Elect, Key Lab Electromagnet Radiat & Sensing Technol, Beijing 100190, Peoples R China
[3] Duke Univ, Dept Elect & Comp Engn, Durham, NC 27708 USA
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2018年 / 56卷 / 02期
基金
中国国家自然科学基金;
关键词
1-D layered media; distorted Born iterative method (DBIM); Frechet derivative; grounded electrical source airborne transient electromagnetic (GREATEM) survey; semianalytical solution of line source; GREATEM SURVEY; RECONSTRUCTION; MULTICOMPONENT; ALGORITHM; EFFICIENT;
D O I
10.1109/TGRS.2017.2756086
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
A new iterative inversion algorithm is proposed to reconstruct the electrical conductivity profile in a stratified underground medium for the grounded electrical source airborne transient electromagnetic (GREATEM) system. In forward modeling, we simplify the mathematical expressions of the magnetic fields generated by a finite line source in the layered ground to semianalytical forms in order to save the computation time. The Frechet derivative is derived for the electromagnetic response at the receivers due to a small perturbation of the conductivity in a certain layer underground. The initial expression of the Frechet derivative has an expensive triple integral and contains the Bessel function in the integrand. It is simplified by partially eliminating the integration along the source line and deriving the analytical expression for the integration in the vertical direction inside the perturbed layer. In the inverse solution, we use the distorted Born iterative method (DBIM). This is the first time that the DBIM is applied to data measured by the GREATEM system. Besides, the forward and inverse procedures are carried out in the frequency domain and based on the Frechet derivative of a line source. We demonstrate the validity of our forward model, Frechet derivative, inverse model, and the precision as well as robustness of the inversion algorithm through numerical computation and comparisons. Finally, we apply the inversion algorithm to the measured data and compare the retrieved conductivity to the actual drilling data.
引用
收藏
页码:877 / 887
页数:11
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