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应用地球物理  2025, Vol. 22 Issue (3): 835-847    DOI: 10.1007/s11770-025-1184-1
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音频大地电磁测深法在隧道超前探测中应用——以和邢铁路天河山隧道为例
赵远程*
1. 中国地质大学(北京) 地球物理与信息技术学院,北京 100083;2. 中铁第五勘察设计院集团有限公司,北京,102600)
Application of audio magnetotelluric method in tunnel advanced detection--Taking Tianheshan tunnel of Hexing Railway as an Example
Yuan-cheng Zhao*
1. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China; 2. China Railway Fifth Survey and Design Institute Group Co., LTD, Beijing 102600, China;
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摘要 隧道在施工过程中经常伴随着塌陷、突泥、涌水等地质灾害的发生,因此探明隧道前方隐藏的地质灾害至关重要。在太行山地区天河山隧道掘进过程中使用音频大地电磁测深法(AMT)进行超前探测研究,在隧道上方布设了3条测深剖面,对野外获得的数据进行了电性主轴分析,由浅至深,电性主轴方向发生变化,总体在NE30°~60°之间,与太行山大断裂的方向相近,数据表现了一定的三维特性。采取了二维和三维反演方法共同研究地下结构信息,对电阻率模型进行了地球物理和地质解释,研究发现两组低阻异常,推测东部的近直立低阻异常可能为破碎带,而西部向西倾斜的低阻异常,可能为与区域大断裂相关的构造或破碎带,隧道掘进结果证实了反演解释的可靠性。三维反演可以全面反映出破碎带的发育规模和形态变化,反演模型更为可靠。最后,认为采用先进采集、处理和反演解释技术的音频大地电磁测深法是隧道超前探测的有效手段。
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关键词太行山   天河山隧道   破碎带   音频大地电磁测深   二维与三维反演     
Abstract: The geological disasters such as collapse, mud bursting and water gushing often occur during tunnel construction. Thus, it is of great significance to detect the hidden geological disasters ahead of the tunnel face. The audio magnetotelluric (AMT) was applied for the advanced detectionstudy during the boring process of the Tianheshan tunnel in the Taihang Mountains. Three AMT profiles were deployed above the tunnel, and the data obtained in the fi eld were analysed in terms of electrical principal axes. From shallow to deep, the direction of the geoelectric strike angle changes, generally between 30° and 60° NE, which is consistent with similar to the direction of the Taihangshan Uplift, and the data show some 3D characteristics. Two-dimensional(2D) and three-dimensional(3D) inversion methods were adopted to jointly study the subsurface structural information, and the resistivity model was geophysically and geologically interpreted.Two sets of low resistance anomalies were found, and it was hypothesised that the near-erect low-resistivity anomalies in the east might be a fragmentation zone, while the low resistance anomalies in the west, which are inclined to the westward, might be a tectonic structure or fragmentation zone related to the regional major fault, and the results of the tunnelling confirmed the reliability of the inversion interpretation. The 3D inversion can fully reflect the development scale and morphological changes of the fracture zone, and the inversion model is more reliable. Finally, it is concluded that the audio magnetotelluric method, which adopts advanced acquisition, processing and inversion interpretation techniques, is an effective means of over-detection of tunnels.
Key wordsTaihangshan    Tianheshan tunnel    fault   AMT    2D and 3D inversion    advanced detection   
收稿日期: 2024-12-05;
基金资助:China Railway Beijing Group Company Limited. (No. 2016CG23)
通讯作者: Yuan-cheng Zhao (zhaoyc@email.cugb.edu.cn).     E-mail: zhaoyc@email.cugb.edu.cn
作者简介: Yuan-cheng Zhao, born in September 1992. Now he is a physical exploration engineer, working in China Railway Fifth Survey and Design Institute Group Company Limited, engaged in engineering physical exploration. At the same time, he is also a doctoral student, studying in China University of Geosciences (Beijing), the main research direction is magnetotelluric.
引用本文:   
. 音频大地电磁测深法在隧道超前探测中应用——以和邢铁路天河山隧道为例[J]. 应用地球物理, 2025, 22(3): 835-847.
. Application of audio magnetotelluric method in tunnel advanced detection--Taking Tianheshan tunnel of Hexing Railway as an Example[J]. APPLIED GEOPHYSICS, 2025, 22(3): 835-847.
 
没有本文参考文献
[1] 乔勇,张慧*. 低阻覆盖区深层地热探测方法及应用实例[J]. 应用地球物理, 2025, 22(1): 99-109.
[2] 徐明才, 高景华, 荣立新, 王广科, 王小江. 地震方法探测太行山山前断裂的活动特征[J]. 应用地球物理, 2010, 7(4): 392-398.
[3] 乔勇,张慧*. 低阻覆盖区深层地热探测方法及应用实例[J]. 应用地球物理, 0, (): 99-109.
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