One-dimensional full-waveform inversion for magnetic induction data in ground-based transient electromagnetic methods

Author:

Li Jianhui123ORCID,Wang Xingchun4ORCID,Hu Xiangyun12,Cai Hongzhu12,Zhi Qingquan4,Chen Shi5

Affiliation:

1. School of Geophysics and Geomatics, China University of Geosciences , Wuhan 430074 , China

2. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences , Wuhan 430074 , China

3. Key Laboratory of Geophysical Electromagnetic Probing Technologies, Ministry of Natural Resources of the People's Republic of China , Langfang 065000 , China

4. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences , Langfang 065000 , China

5. China Railway Liuyuan Group Co. , Ltd, Tianjin 300308 , China

Abstract

Abstract The full-waveform effects refer to the total effects of turn-on, steady and turn-off durations for a transmitting-current waveform as well as its repetition number in transient electromagnetic (TEM) methods. In this study, the full-waveform effects are investigated using both forward-modeling and inversion methods considering typical background noise. The forward-modeling results of homogeneous half-space models show that the magnetic induction, bz, is less affected by the background noise but more affected by the full-waveform effects than the time derivative of magnetic induction ∂bz/∂t. Therefore, this study focuses on investigating the full-waveform effects on bz. The inversion results for synthetic and field examples show that the inversion algorithm without considering the full-waveform effects leads to over-estimated resistivities in deeper parts of the recovered models compared to the true model. As a result, it is crucial to consider the full-waveform effects when processing TEM data. Furthermore, a standard deviation factor (STDF) is estimated for model parameters of the inversion. The results show that the STDF increases as the layer depth increases for 1D layered models. This indicates that the inverted parameters are well resolved for shallower layers and moderately to poorly resolved for deeper layers.

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Publisher

Oxford University Press (OUP)

Subject

Management, Monitoring, Policy and Law,Industrial and Manufacturing Engineering,Geology,Geophysics

Cited by 1 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Advances in transient electromagnetic methods;Journal of Geophysics and Engineering;2023-10-25

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