隧道瞬变电磁法超前预测的可行性:三维正演模拟研究

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-11-28 DOI:10.1155/2023/8486173
Jiannan Fu, Xiaodong Yang, Guanqun Zhou, Xueliang Jin, Fuqin Zhai, Fanbin Meng, Yafei Wang
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引用次数: 0

摘要

瞬变电磁法在隧道超前预测中应用已久。然而,地质异常体对掘进工作面前方感应电磁响应的影响程度尚不明确。造成这种困境的部分原因是观测到的透射电镜数据经常用经验公式或比例关系来解释,而且还没有建立定量测量方法。在本文中,我们努力从三维有限元时域(FETD)建模的角度来理解瞬变电磁法的特征。该建模算法基于非结构化空间网格化和无条件稳定时间离散化,保证了建模的精度和稳定性。通过半空间模型对建模算法进行了验证,在半空间模型中,我们所关注的晚时信道的失配率一般在1%以下。该算法还应用于不同类型瞬变电磁法装置下隧道模型的瞬变电磁法响应。通过模型研究,我们发现传统的中心环装置和新开发的弱耦合对线圈装置在隧道超前探测中都是可行的。然而,后一种装置更好地识别了迎头前方30 m处的低电阻率异常,在某些时间通道上(有异常和没有异常的模型之间)的相对差异超过1000%,而中心环装置的差异仅为10%。此外,我们认为垂直电磁场分量应与水平场一起记录和解释,以提供更有说服力的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Feasibility of Tunnel TEM Advanced Prediction: A 3D Forward Modeling Study
The transient electromagnetic (TEM) method has long been applied in tunnel advanced prediction. However, it remains questionable to what extent a geologic anomaly body will influence the induced electromagnetic response in front of the heading face. The dilemma is partly because observed TEM data are frequently interpreted by empirical formulas or proportional relationships, and a quantitative measurement has not been established. In this paper, we strive to understand the TEM characteristics from a 3D finite-element time-domain (FETD) modeling aspect. The modeling algorithm is based on unstructured space meshing and unconditional stable time discretization, which ensures its accuracy and stability. The modeling algorithm is verified by a half-space model, in which the misfit of late-time channels that we are concerned with is generally below 1%. The algorithm has also been utilized to carry out the TEM response of tunnel models with different types of TEM devices. Through model studies, we find that both the traditional central-loop device and the recently developed weak-coupling opposing-coil device are feasible in tunnel advanced detection. Nevertheless, the latter type of device better distinguishes low-resistivity anomalies at 30 m ahead of the heading face with a relative difference (between models with and without the anomaly) of more than 1000% at certain time channels, compared with only a 10% difference of the central-loop device. Also, we conclude that the vertical electromagnetic field component should be recorded and interpreted together with the horizontal field to provide more convincing results.
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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