|Table of Contents|

Jointly Inversion of Multi-source Data of Frequency-domain Controlled Source Electromagnetic Method(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2021年第06期
Page:
1057-1068
Research Field:
应用地球物理
Publishing date:

Info

Title:
Jointly Inversion of Multi-source Data of Frequency-domain Controlled Source Electromagnetic Method
Author(s):
HAN Si-xu12 CHEN Wei-ying345* XUE Guo-qiang3456 LEI Kang-xin345 SONG Wan-ting345
(1. Guangdong Provincial Geophysical Prospecting Team, Guangzhou 510800, Guangdong, China; 2. Guangdong Provincial Institute of Geological and Geophysical Engineering Survey, Guangzhou 510800, Guangdong, China; 3. Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 4. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China; 5. Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China; 6. Northwest Nonferrous Geological and Mining Group Co., Ltd., Xi'an 710054, Shaanxi, China)
Keywords:
frequency-domain controlled source electromagnetic method multi-source data joint inversion ARIA formation wave 3D model
PACS:
P631; P319
DOI:
10.19814/j.jese.2021.07002
Abstract:
In the traditional land frequency-domain controlled source electromagnetic method(FCSEM), an observing point generally only corresponds to a single transmitting source. Thus, it is necessary to explore the multi-source joint inversion method of land FCSEM. Firstly, the joint inversion of multi-source data was realized by using one-dimensional ARIA. Then, based on the three-layer model, the effects of different source combinations and source numbers on the joint inversion were analyzed. Finally, the results of this joint inversion on complex models were evaluated. The results show that compared with the single source inversion, joint inversion of multi-source data improves the accuracy of inversion results, making the obtained geoelectric parameters are closer to the real value especially when the models are more complicated; with the increase of the number of sources involved in the inversion, the results will be further improved. Except the combined broadside sources are not sensitive to the resistive target, the other forms of combined sources are all sensitive to the conductive and resistive bodies. The above research is willing to provide a guide for establishing a reasonable observation technology of multi-source FCSEM and processing pratical data.

References:

[1] 何继善.可控源音频大地电磁法[M].长沙:中南工业大学出版社,1990.
HE Ji-shan.Controlled-source Audio Frequency Magnetotelluric Method[M].Changsha:Central South Institute of Technology Press,1990.
[2] 何继善.广域电磁法和伪随机信号电法[M].北京:高等教育出版社,2010.
HE Ji-shan.Wide Field Electromagnetic Method and Pseudorandom Signal Electrical Method[M].Beijing:Higher Education Press,2010.
[3] CONSTABLE S.Ten Years of Marine CSEM for Hydrocarbon Exploration[J].Geophysics,2010,75(5):A67-A81.
[4] CONSTABLE S,WEISS C J.Mapping Thin Resistors and Hydrocarbons with Marine EM Methods:Insights from 1D Modeling[J].Geophysics,2006,71(2):G43-G51.
[5] 底青云,王 若.CSAMT数据正反演及方法应用[M].北京:科学出版社,2007.
DI Qing-yun,WANG Ruo.CSAMT Forward Modeling and Inversion and Its Application[M].Beijing:Science Press,2007.
[6] 汤井田,任政勇,周 聪,等.浅部频率域电磁勘探方法总述[J].地球物理学报,2015,58(8):2681-2705.
TANG Jing-tian,REN Zheng-yong,ZHOU Cong,et al.Frequency-domain Electromagnetic Methods for Exploration of the Shallow Subsurface[J].Chinese Journal of Geophysics,2015,58(8):2681-2705.
[7] 陈明生,闫 述.CSAMT勘探中场区、记录规则、阴影及场源复印效应的解析研究[J].地球物理学报,2005,48(4):951-958.
CHEN Ming-sheng,YAN Shu.Analytical Study on Field Zones,Record Rules,Shadow and Source Overprint Effects in CSAMT Exploration[J].Chinese Journal of Geophysics,2005,48(4):951-958.
[8] 李 貅,胡伟明,薛国强.多辐射源地空瞬变电磁响应三维数值模拟研究[J].地球物理学报,2021,64(2):716-723.
LI Xiu,HU Wei-ming,XUE Guo-qiang.3D Modeling of Multi-radiation Source Semi-airborne Transient Electromagnetic Response[J].Chinese Journal of Geophysics,2021,64(2):716-723.
[9] 王显详,底青云,许 诚.CSAMT的多偶极子源特征与张量测量[J].地球物理学报,2014,57(2):651-661.
WANG Xian-xiang,DI Qing-yun,XU Cheng.Characteristics of Multiple Sources and Tensor Measurement in CSAMT[J].Chinese Journal of Geophysics,2014,57(2):651-661.
[10] 张莹莹,李 貅,姚伟华,等.多辐射场源地空瞬变电磁法多分量全域视电阻率定义[J].地球物理学报,2015,58(8):2745-2758.
ZHANG Ying-ying,LI Xiu,YAO Wei-hua,et al.Multi-component Full Field Apparent Resistivity De-finition of Multi-source Ground-airborne Transient Electromagnetic Method with Galvanic Sources[J].Chinese Journal of Geophysics,2015,58(8):2745-2758.
[11] 张继锋,刘寄仁,冯 兵,等.多源频率域地空系统三维电磁响应分析[J].地球物理学报,2021,64(4):1419-1434.
ZHANG Ji-feng,LIU Ji-ren,FENG Bing,et al.Three-dimensionla Response of the 3D Grounded Multiple-source Airborne EM System in the Frequency Domain[J].Chinese Journal of Geophysics,2021,64(4):1419-1434.
[12] ZHANG L B,XUE G Q,KHAN M Y,et al.Exploration of a Magnetite Deposit Buried Under Thick and Conductive Sediments with Multiple-source CSEM[J].Journal of Applied Geophysics,2020,180:104112.
[13] 李 海,薛国强,钟华森,等.多道瞬变电磁法共中心点道集数据联合反演[J].地球物理学报,2016,59(12):4439-4447.
LI Hai,XUE Guo-qiang,ZHONG Hua-sen,et al.Joint Inversion of CMP Gathers of Multi-channel Transient Electromagnetic Data[J].Chinese Journal of Geophysics,2016,59(12):4439-4447.
[14] 陈明生,石显新.电磁测深法原理与应用[M].北京:科学出版社,2020.
CHEN Ming-sheng,SHI Xian-xin.Principle and Application of Electromagnetic Sounding Method[M].Beijing:Science Press,2020.
[15] 底青云,朱日祥,薛国强,等.我国深地资源电磁探测新技术研究进展[J].地球物理学报,2019,62(6):2128-2138.
DI Qing-yun,ZHU Ri-xiang,XUE Guo-qiang,et al.New Development of the Electromagnetic(EM)Me-thods for Deep Exploration[J].Chinese Journal of Geophysics,2019,62(6):2128-2138.
[16] WIRIANTO M,MULDER W A,SLOB E C.A Feasibility Study of Land CSEM Reservoir Monitoring:The Effect of Airwave[J].PIERS Online,2010,6(5):440-444.
[17] 陈小斌,赵国泽,汤 吉,等.大地电磁自适应正则化反演算法[J].地球物理学报,2005,48(4):937-946.
CHEN Xiao-bin,ZHAO Guo-ze,TANG Ji,et al.An Adaptive Regularized Inversion Algorithm for Magnetotelluric Data[J].Chinese Journal of Geophysics,2005,48(4):937-946.
[18] 刘 颖,李予国,韩 波.可控源电磁场三维自适应矢量有限元正演模拟[J].地球物理学报,2017,60(12):4874-4886.
LIU Ying,LI Yu-guo,HAN Bo.Adaptive Edge Finite Element Modeling of the 3D CSEM Field on Unstructured Grids[J].Chinese Journal of Geophysics,2017,60(12):4874-4886.
[19] 殷长春,贲 放,刘云鹤,等.三维任意各向异性介质中海洋可控源电磁法正演研究[J].地球物理学报,2014,57(12):4110-4122.
YIN Chang-chun,BEN Fang,LIU Yun-he,et al.MCSEM 3D Modeling for Arbitrarily Anisotropic Media[J].Chinese Journal of Geophysics,2014,57(12):4110-4122.
[20] 付长民,底青云,王妙月.海洋可控源电磁法三维数值模拟[J].石油地球物理勘探,2009,44(3):358-363.
FU Chang-min,DI Qing-yun,WANG Miao-yue.3D Numeric Simulation of Marine Controlled Source Ele-ctromagnetics(MCSEM)[J].Oil Geophysical Pro-specting,2009,44(3):358-363.
[21] 张继锋,汤井田,喻 言,等.基于电场矢量波动方程的三维可控源电磁法有限单元法数值模拟[J].地球物理学报,2009,52(12):3132-3141.
ZHANG Ji-feng,TANG Jing-tian,YU Yan,et al.Three-dimensional Controlled Source Electromagnetic Numerical Simulation Based on Electric Field Vector Wave Equation Using Finite Element Method[J].Chinese Journal of Geophysics,2009,52(12):3132-3141.
[22] 杨 悦,翁爱华,张艳辉,等.基于可控源电磁法阻抗信息的有限内存拟牛顿法三维反演[J].吉林大学学报(地球科学版),2019,49(2):591-602.
YANG Yue,WENG Ai-hua,ZHANG Yan-hui,et al.Three-dimensional Inversion Based on the Impedance Information of Controlled Source Electromagnetic Method by Limited Memory Quasi-Newton Method[J].Journal of Jilin University(Earth Science Edition),2019,49(2):591-602.

Memo

Memo:
-
Last Update: 2021-11-10