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瞬变电磁扩散场到虚拟波场的精细积分变换算法
引用本文:鲁凯亮, 李貅, 戚志鹏, 樊亚楠, 周建美, 李文翰, 李贺, 张明晶, 王扬州. 2021. 瞬变电磁扩散场到虚拟波场的精细积分变换算法. 地球物理学报, 64(9): 3379-3390, doi: 10.6038/cjg2021O0454
作者姓名:鲁凯亮  李貅  戚志鹏  樊亚楠  周建美  李文翰  李贺  张明晶  王扬州
作者单位:1. 长安大学地质工程与测绘学院, 西安 710054; 2. 长安大学地球物理场多参数综合模拟实验室(中国地球物理学会重点实验室), 西安 710054; 3. 山东大学齐鲁交通学院, 济南 250061; 4. 山东省交通规划设计院, 济南 250031; 5. 北京探创资源科技有限公司, 北京 100071
基金项目:国家自然科学基金;多分辨地空瞬变电磁深部探测偏移成像理论与方法研究项目;国家自然科学基金;国家自然科学基金
摘    要:现有的瞬变电磁解释与反演方法主要对电阻率参数进行解释,较难给出准确的地质构造信息.为了能够较多获得地质构造信息,可将瞬变电磁扩散场信号转换为虚拟波场信号,提高瞬变电磁法的分辨率.本文采用精细积分法,实现了瞬变电磁扩散场到虚拟波场的转换.将一个高度病态的线性方程组转换成求积分的过程,大大降低了解决病态问题的难度.积分步长...

关 键 词:瞬变电磁  虚拟波场  精细积分
收稿时间:2020-11-24
修稿时间:2021-03-02

A precise integration transform algorithm for transformation from the transient electromagnetic diffusion field into the pseudo wave field
LU KaiLiang, LI Xiu, QI ZhiPeng, FAN YaNan, ZHOU JianMei, LI WenHan, LI He, ZHANG MingJing, WANG YangZhou. 2021. A precise integration transform algorithm for transformation from the transient electromagnetic diffusion field into the pseudo wave field. Chinese Journal of Geophysics (in Chinese), 64(9): 3379-3390, doi: 10.6038/cjg2021O0454
Authors:LU KaiLiang  LI Xiu  QI ZhiPeng  FAN YaNan  ZHOU JianMei  LI WenHan  LI He  ZHANG MingJing  WANG YangZhou
Affiliation:1. College of Geology Engineering and Geomatics, Chang'an University, Xi'an 710054, China; 2. Integrated Geophysical Simulation Lab of Chang'an University(Key Laboratory of Chinese Geophysical Society), Xi'an 710054, China; 3. School Qilu Transportation, Shangdong University, Jinan 250061, China; 4. Shandong Provincial Transportation Planning and Design Institute, Jinan 250031, China; 5. Beijing Tanchuang Resources Technology Co., Ltd, Beijing 100071, China
Abstract:The existing transient electromagnetic interpretation and inversion methods focus on the resistivity parameters, which are difficult to give accurate geological structure information. To solve this problem, the transient electromagnetic diffusion field signal can be transformed into a virtual wave field signal to improve the resolution of the transient electromagnetic method. In this paper, a precise integration method is proposed to realize the conversion of the transient electromagnetic diffusion field to the virtual wave field. It is found that by converting a highly ill-conditioned system of linear equations into an integration process, the difficulties related to solving ill-conditioned problems are greatly reduced. Besides, based on the premise of ensuring high accuracy results, the integration step lengths are exponentially increased by 2, and high computational efficiency is achieved. The applicability of the method proposed in this study is further improved by setting reasonable iteration stopping conditions. The calculations of the typical geoelectric models show that this method has high precision. Then, by reducing the distances between two wave peaks, it was proven that the method introduced in this study had better resolution. Furthermore, through the wavefield inverse transformations of diffusion fields containing noise, it is confirmed that the proposed method also has better noise-resistant capability. Finally, calculations of the pseudo wave fields of 3D models and field data permit to identify well the interfaces of 3D geological bodies, which further demonstrates that the method proposed in this study is stable and reliable. Compared with the preconditioned regularization method, the efficiency of the proposed method is improved by about 4 times. The relative error of the method in this work is within 5%, while the maximum relative error of PRCG can reach 40%~50%, and the accuracy can be improved by 10 times. In terms of resolution and stability, this method also shows better performance.
Keywords:Transient electromagnetics  Virtual wave-fields  Precise integration
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