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Exploring a correction technology for ground resistance in audio-frequency magnetotelluric measurements |
LI Dong( ), ZHANG Ming-Cai( ), WU Yuan-Yang |
Northwest Engineering Corporation Limited, PowerChina, Xi’an 710065, China |
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Abstract Ground resistance is a significant factor affecting the accuracy of audio-frequency magnetotelluric (AMT) measurements. Hence, reducing the interference from ground resistance is critical for enhancing the reliability and interpretation accuracy of AMT data. By delving into the impacts of ground resistance on the measured electric field, apparent resistivity, and impedance phase, this study proposed a numerical correction method for reducing the impacts of ground resistance to a negligible level. As indicated by the theoretical calculation results, too high ground resistance can reduce the apparent resistivity in high-frequency bands to a quarter of the original value and shift the impedance phase by a maximum of 20°. The correction results of measured data demonstrate that the proposed method can enhance the accuracy of the AMT method in detecting shallow information by effectively reducing the interference from ground resistance. Therefore, this study holds critical significance for improving the application of the AMT method in engineering exploration.
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Received: 19 April 2024
Published: 22 July 2025
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Equivalent circuit diagram of receiving loop
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Diagram of the relationship between electric field amplitude and grounding resistance
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Diagram of the relationship between apparent resistivity and ground resistance
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Diagram of the relationship between impedance phase and ground resistance
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桩号/m | R/Ω | 桩号/m | R/Ω | 桩号/m | R/Ω | 桩号/m | R/Ω | 0 | 12 407 | 180 | 7 917 | 370 | 10 456 | 580 | 12 644 | 30 | 18 037 | 210 | 11 800 | 400 | 6 305 | 610 | 9 207 | 60 | 13 930 | 240 | 8 561 | 430 | 5 389 | 640 | 10 434 | 90 | 22 457 | 270 | 11 571 | 460 | 4 123 | 670 | 9 534 | 120 | 12 914 | 300 | 8 323 | 490 | 5 392 | 700 | 9 506 | 150 | 12 849 | 340 | 8 030 | 550 | 7 340 | 730 | 7 846 |
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Grounding resistance of each measuring point on L1 line
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Curve of 90 m point apparent resistivity before and after correction
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Curve of 580 m point apparent resistivity before and after correction
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Impedance phase polar coordinate diagram before L1 line correction
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Impedance phase polar coordinate diagram after L1 line correction
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Inverted resistivity profile before correction of L1 line
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Inverted resistivity profile after correction of L1 line
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层底深度/m | 地层时代 | 岩性 | 地质描述 | 16.7 | 第四系 | 粉土 | 全新统冲湖积粉土,灰黄色,结构松散,成分以粉粒为主,含云母,土质均匀,呈软塑状态,较为饱和。 | 60.6 | 第四系 | 粉质黏土 | 上更新统冲洪积粉质黏土,灰黄色,土质均匀,以粉粒、黏粒为主,黏性较好,切面光滑,呈可塑状态,较为饱和。 | 69.8 | 第四系 | 粉质黏土 | 中更新统冲洪积粉质黏土,灰黄色,土质均匀,黏粒含量较高,含粉砂及云母,呈可塑状态,较为饱和。 | 94.0 | 白垩系 | 砂岩 | 白垩系砂岩,红褐色,粗粒结构,中厚层构造。层面裂隙发育强烈,泥质充填。 | 99.7 | 白垩系 | 泥质粉砂岩 | 白垩系泥质粉砂岩,青灰色,细粒结构,中薄层构造,层间裂隙发育强烈,含有较多泥质充填。 |
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The catalog data of ZK204
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