Optimal survey parameters for the borehole-to-surface controlled source electromagnetic method

The Frequency-domain borehole-to-surface controlled source electromagnetic (FD-BSCSEM) method is a geophysical technique used to explore mineral resources and assess engineering geology. However, the optimal selection of operational parameters for borehole-to-surface measurements remains a topic of...

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Published inJournal of applied geophysics Vol. 241; p. 105840
Main Authors Zhang, Zhenghu, Zhou, Nannan
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.10.2025
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Abstract The Frequency-domain borehole-to-surface controlled source electromagnetic (FD-BSCSEM) method is a geophysical technique used to explore mineral resources and assess engineering geology. However, the optimal selection of operational parameters for borehole-to-surface measurements remains a topic of debate. Through three-dimensional numerical simulations, we investigate the propagation characteristics of current in the BSCSEM method and the impact of various operational parameters on the simulated responses. Using a high resistivity plate-shaped anomaly as a case study, we analyze the effects of offset, source position, and source length on the radial electric field component (Er). Our results show that for anomalies buried at a depth of 500 m, the offset should be limited to within 2000 m to ensure sufficient signal strength and resolution. Charge accumulation is primarily concentrated at the top and bottom surfaces of the anomaly. When the source is sufficiently close to the anomaly, a stronger anomalous response will occur at the surface. When the source length is significantly longer than the thickness of the anomaly, the anomalous signal experiences rapid attenuation; therefore, it is advisable to limit the source length to prevent excessive energy dispersion. Finally, we examined the response of low-resistivity bodies. Compared to high-resistivity anomalies, horizontal currents are more likely to dominate in low-resistivity bodies, leading to differences in parameter selection. •Innovative Approach: We studied BSCSEM survey parameters and found they significantly impact resolution in synthetic model.•3D Numerical Simulation: We analyzed current propagation in anomalies and its impact on responses, offering a basis for optimizing survey parameters.•Key Parameter Analysis: The study shows that for 500 m deep anomalies, offset should be under 2 km to maintain signal strength and resolution.•Electric Field Response Characteristics: The vertical current source are sensitive to high-resistivity bodies, revealing their distribution and relation to anomalies.•Survey Optimization Recommendations: Limiting source length is advised to reduce energy dispersion; source depth and position also affect resolution capability.
AbstractList The Frequency-domain borehole-to-surface controlled source electromagnetic (FD-BSCSEM) method is a geophysical technique used to explore mineral resources and assess engineering geology. However, the optimal selection of operational parameters for borehole-to-surface measurements remains a topic of debate. Through three-dimensional numerical simulations, we investigate the propagation characteristics of current in the BSCSEM method and the impact of various operational parameters on the simulated responses. Using a high resistivity plate-shaped anomaly as a case study, we analyze the effects of offset, source position, and source length on the radial electric field component (Er). Our results show that for anomalies buried at a depth of 500 m, the offset should be limited to within 2000 m to ensure sufficient signal strength and resolution. Charge accumulation is primarily concentrated at the top and bottom surfaces of the anomaly. When the source is sufficiently close to the anomaly, a stronger anomalous response will occur at the surface. When the source length is significantly longer than the thickness of the anomaly, the anomalous signal experiences rapid attenuation; therefore, it is advisable to limit the source length to prevent excessive energy dispersion. Finally, we examined the response of low-resistivity bodies. Compared to high-resistivity anomalies, horizontal currents are more likely to dominate in low-resistivity bodies, leading to differences in parameter selection. •Innovative Approach: We studied BSCSEM survey parameters and found they significantly impact resolution in synthetic model.•3D Numerical Simulation: We analyzed current propagation in anomalies and its impact on responses, offering a basis for optimizing survey parameters.•Key Parameter Analysis: The study shows that for 500 m deep anomalies, offset should be under 2 km to maintain signal strength and resolution.•Electric Field Response Characteristics: The vertical current source are sensitive to high-resistivity bodies, revealing their distribution and relation to anomalies.•Survey Optimization Recommendations: Limiting source length is advised to reduce energy dispersion; source depth and position also affect resolution capability.
ArticleNumber 105840
Author Zhang, Zhenghu
Zhou, Nannan
Author_xml – sequence: 1
  givenname: Zhenghu
  surname: Zhang
  fullname: Zhang, Zhenghu
  organization: Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
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  givenname: Nannan
  surname: Zhou
  fullname: Zhou, Nannan
  email: zhounannan@mail.iggcas.ac.cn
  organization: Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
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Keywords BSCSEM
Grounded-wire
Vertical current sources
Survey parameters
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Snippet The Frequency-domain borehole-to-surface controlled source electromagnetic (FD-BSCSEM) method is a geophysical technique used to explore mineral resources and...
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SubjectTerms BSCSEM
Grounded-wire
Survey parameters
Vertical current sources
Title Optimal survey parameters for the borehole-to-surface controlled source electromagnetic method
URI https://dx.doi.org/10.1016/j.jappgeo.2025.105840
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