|
|
Analysis of multi-component response characteristics of surface-to-borehole transient electromagnetic method with complex-shaped loop source |
WANG Zhi-Xin1,2( ), DENG Ju-Zhi1,2( ), CHEN Hui1,2, QIU Chang-Kai3, YU Hui1,2, YIN Min1,2, FENG Min1,2 |
1. State Key Laboratory of Nuclear Resources and Environment, Nanchang 330013, China 2. School of Geophysics and Measurement-control Technology, East China University of Technology, Nanchang 330013, China 3. Development and Research Center, China Geological Survey, Beijing 100083, China |
|
|
Abstract In actual exploration, the surface-to-borehole transient electromagnetic (TEM) method is prone to be affected by irregular transmitter loops and inclined boreholes, resulting in increased measurement errors of the three-component induced magnetic fields and decreased interpretation accuracy. By establishing surface-to-borehole TEM method-based three-component measurement models under the excitement of transmitter loops of various shapes, this study derived the calculation formulas for surface-to-borehole TEM responses under inclined boreholes through coordinate transformation. Then, it achieved one-dimensional forward modeling of the full-space TEM field using a numerical filtering algorithm. The calculation results of multiple typical models indicate that the three components of the transient magnetic fields were significantly influenced by the shapes of the transmitter loops, with the impacts on horizontal components x and y far more significant than those on vertical component z. The transmitter loops of regular polygons with even edges as the sources exhibited uniform and symmetric distribution of the TEM fields of the three components. Under the condition of the same perimeter, a greater number of edges of the transmitter loops associated with greater primary field energy excited by the loops. Therefore, rectangular transmitter loops as the sources prove the most cost-effective. The inclination and offset primarily affected the amplitude of the three-component responses. In contrast, the borehole azimuth mainly influenced the sign of the horizontal components, bearing rich information on location. Therefore, in the exploration using the surface-to-borehole TEM method, it is necessary to accurately determine source paths and the geometric morphologies of boreholes to make essential corrections, thus improving the accuracy and reliability of interpretations.
|
Received: 10 November 2023
Published: 22 April 2025
|
|
|
|
|
|
Borehole TEM system model with arbitrary loop sources
|
|
Numerical solution and Analytical solution comparison
|
|
Comparison of results for the irregular loop model example
|
|
Four loop source shapes
|
|
X-component response characteristic diagram of transient field of four loop sources
|
|
Z-component response characteristic diagram of transient field of four loop sources
|
|
Three-component response curves of different shape of sources (dashed lines indicate negative symbols)
|
|
X and Z component response curves of different well offset distances (dashed lines indicate negative symbols)
|
|
U and A component response curves of different well inclinations (dashed lines indicate negative symbols)
|
|
X and Y component response curves of different well orientations (dashed lines indicate negative symbols)
|
[1] |
蒋邦远. 实用近区磁源瞬变电磁法勘探[M]. 北京: 地质出版社, 1998.
|
[1] |
Jiang B Y. Transient electromagnetic exploration with practical near-field magnetic source[M]. Beijing: Geological Publishing House, 1998.
|
[2] |
牛之琏. 时间域电磁法原理[M]. 长沙: 中南大学出版社, 2007.
|
[2] |
Niu Z L. Principle of time domain electromagnetic method[M]. Changsha: Central South University Press, 2007.
|
[3] |
Woods D V. A model study of the Crone borehole pulse electromagnetic (PEM) system[D]. Kingston: Queen’s University, 1975.
|
[4] |
Dyck A V. The role of simple computer models in interpretations of wide-band,drill-hole electromagnetic surveys in mineral exploration[J]. Geophysics, 1984, 49(7):957.
|
[5] |
Eaton P A, Hohmann G W. The influence of a conductive host on two-dimensional borehole transient electromagnetic responses[J]. Geophysics, 1984, 49(7):861-869.
|
[6] |
Buselli G, Lee S K. Modelling of drill-hole TEM responses for multiple targets covered by a conductive overburden[J]. Exploration Geophysics, 1996, 27(2-3):141-153.
|
[7] |
孟庆鑫, 潘和平, 牛峥. 大地介质影响下地—井瞬变电磁的正演模拟分析[J]. 中国矿业大学学报, 2014, 43(6):1113-1119.
|
[7] |
Meng Q X, Pan H P, Niu Z. Forward simulation of surface-borehole TEM in geological medium effect[J]. Journal of China University of Mining & Technology, 2014, 43(6):1113-1119.
|
[8] |
易洪春. 地—井瞬变电磁响应特征研究[J]. 物探与化探, 2018, 42(5):970-976.
|
[8] |
Yi H C. Research on response of ground-borehole TEM[J]. Geophysical and Geochemical Exploration, 2018, 42(5):970-976.
|
[9] |
郭建磊, 姜涛, 郭恒, 等. 轴向各向异性地-井瞬变电磁三分量响应特征[J]. 地球科学与环境学报, 2020, 42(6):737-748.
|
[9] |
Guo J L, Jiang T, Guo H, et al. Characteristics of axial anisotropic borehole transient electromagnetic three-component response[J]. Journal of Earth Sciences and Environment, 2020, 42(6):737-748.
|
[10] |
郭建磊. 轴向各向异性地层瞬变电磁三分量响应特征[J]. 物探与化探, 2022, 46(2):362-372,382.
|
[10] |
Guo J L. Three-component responses of axially anisotropic formations using the transient electromagnetic method[J]. Geophysical and Geochemical Exploration, 2022, 46(2):362-372,382.
|
[11] |
Li H J, Mao Y R, Wang X Y, et al. Characterization of surface-borehole transient electromagnetic response in electrical anisotropic media[J]. Minerals, 2023, 13(5):674.
|
[12] |
张杰, 王兴春, 邓晓红, 等. 地—井瞬变电磁井旁板状导体异常响应特征分析[J]. 物探化探计算技术, 2014, 36(6):641-648.
|
[12] |
Zhang J, Wang X C, Deng X H, et al. Borehole transient electromagnetic method response characteristics of the borehole-side plate-like conductor[J]. Computing Techniques for Geophysical and Geochemical Exploration, 2014, 36(6):641-648.
|
[13] |
唐继强, 席振铢, 王鹤, 等. 三维体地—井瞬变电磁三分量测量响应规律研究[J]. 工程地球物理学报, 2015, 12(3):315-321.
|
[13] |
Tang J Q, Xi Z Z, Wang H, et al. The regularity of three-component measurement responses in surface-hole TEM[J]. Chinese Journal of Engineering Geophysics, 2015, 12(3):315-321.
|
[14] |
王鹏. 积水采空区地井瞬变电磁法探测[J]. 煤炭技术, 2017, 36(6):134-136.
|
[14] |
Wang P. Surface-hole TEM for detection of coal mine water collecting area[J]. Coal Technology, 2017, 36(6):134-136.
|
[15] |
宋汐瑾, 党瑞荣, 郭宝龙, 等. 井中磁源瞬变电磁响应特征研究[J]. 地球物理学报, 2011, 54(4):1122-1129.
|
[15] |
Song X J, Dang R R, Guo B L, et al. Research on transient electromagnetic response of magnetic source in borehole[J]. Chinese Journal of Geophysics, 2011, 54(4):1122-1129.
|
[16] |
姚伟华, 王鹏, 李明星, 等. 地孔瞬变电磁法超前探测数值模拟响应特征[J]. 煤炭学报, 2019, 44(10):3145-3153.
|
[16] |
Yao W H, Wang P, Li M X, et al. Numerical simulation response characteristics of down-hole TEM for advanced detection[J]. Journal of China Coal Society, 2019, 44(10):3145-3153.
|
[17] |
王鹏, 程建远, 姚伟华, 等. 积水采空区地面—钻孔瞬变电磁探测技术[J]. 煤炭学报, 2019, 44(8):2502-2508.
|
[17] |
Wang P, Cheng J Y, Yao W H, et al. Technology of detecting water-filled goaf beside borehole using downhole transient electromagnetic method[J]. Journal of China Coal Society, 2019, 44(8):2502-2508.
|
[18] |
Wang P, Li M X, Yao W H, et al. Detection of abandoned water-filled mine tunnels using the downhole transient electromagnetic method[J]. Exploration Geophysics, 2020, 51(6):667-682.
|
[19] |
张杰, 邓晓红, 谭捍东, 等. 地—井瞬变电磁资料矢量交会解释方法[J]. 物探与化探, 2015, 39(3):572-579.
|
[19] |
Zhang J, Deng X H, Tan H D, et al. A study of vector intersection for borehole transient electromagnetic method[J]. Geophysical and Geochemical Exploration, 2015, 39(3):572-579.
|
[20] |
赵友超, 张军, 范涛, 等. 地—井瞬变电磁三维响应特征分析与异常体快速定位方法研究[J]. 物探与化探, 2022, 46(2):383-391.
|
[20] |
Zhao Y C, Zhang J, Fan T, et al. Analysis of 3D ground-borehole TEM response characteristics and rapid positioning method for anomalous bodies[J]. Geophysical and Geochemical Exploration, 2022, 46(2):383-391.
|
[21] |
李建慧, 胡祥云, 陈斌, 等. 复杂形态回线源激发电磁场的矢量有限元解[J]. 石油地球物理勘探, 2017, 52(6):1324-1332,1125.
|
[21] |
Li J H, Hu X Y, Chen B, et al. 3D electromagnetic modeling with vector finite element for a complex-shaped loop source[J]. Oil Geophysical Prospecting, 2017, 52(6):1324-1332,1125.
|
[22] |
Kaufman A A, Kelland G V. Electromagnetic sounding of frequency domain and time domain[J]. Geological Publishing House, 1987.
|
[23] |
Guptasarma D, Singh B. New digital linear filters for Hankel J0 and J1 transforms[J]. Geophysical Prospecting, 1997, 45(5):745-762.
|
[24] |
朴化荣. 电磁测深法原理[M]. 北京: 地质出版社, 1990.
|
[24] |
Piao H R. Principle of electromagnetic sounding method[M]. Beijing: Geological Publishing House, 1990.
|
[25] |
李貅. 瞬变电磁测深的理论与应用[M]. 西安: 陕西科学技术出版社, 2002.
|
[25] |
Li X. Theory and application of transient electromagnetic sounding[M]. Xi'an: Shaanxi Science & Technology Press, 2002.
|
[26] |
戚志鹏, 智庆全, 李貅, 等. 大定源瞬变电磁三分量全域视电阻率定义与三分量联合反演[J]. 物探与化探, 2014, 38(4):742-749.
|
[26] |
Qi Z P, Zhi Q Q, Li X, et al. The definition of the full-zone apparent resistivity and the constrained inversion of the three components of fixed source TEM[J]. Geophysical and Geochemical Exploration, 2014, 38(4):742-749.
|
[27] |
王鹏飞, 王书明, 安永宁. 不规则回线瞬变电磁法一维烟圈反演研究[J]. 地球物理学进展, 2019, 34(3):1113-1120.
|
[27] |
Wang P F, Wang S M, An Y N. One-dimensional smoke ring inversion of irregular loop source transient electromagnetic method[J]. Progress in Geophysics, 2019, 34(3):1113-1120.
|
[1] |
ZHANG Fan, FENG Guo-Rui, QI Ting-Ye, YU Chuan-Tao, ZHANG Xin-Jun, WANG Chao-Yu, DU Sun-Wen, ZHAO De-Kang. Feasibility of the transient electromagnetic method in the exploration of double-layer waterlogged goafs with different layer spacings in coal mines[J]. Geophysical and Geochemical Exploration, 2023, 47(5): 1215-1225. |
[2] |
ZHANG Ying-Ying. An analysis of full-component response of multi-source semi-airborne TEM method[J]. Geophysical and Geochemical Exploration, 2021, 45(1): 102-113. |
|
|
|
|