轨道干扰下列车载瞬变电磁法近距离含水异常探测范围研究

Zongyang Li, Taiyue Qi
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摘要

中国高速铁路运营隧道中与地下水有关的疾病比例日益增加,迫切需要快速准确的疾病监测。因此,利用列车载瞬变电磁法监测运行中的隧道结构中5 ~ 10米含水异常是一种新的尝试。隧道环境中静止干扰源列车轨道对含水异常监测具有严重的电磁干扰。为此,本文将数值模拟与室内实验相结合,开展了列车载瞬变电磁法在轨道电磁干扰下近距离监测最小含水异常的研究。首先通过数值模拟对比研究了含水异常自身参数变化时的电磁特性,然后对比分析了列车轨道干扰下含水异常的电磁响应。针对数值模拟中线圈-金属-异常缺失的电磁响应,进行了全尺度物理模型实验,得到了三种干扰的时间范围。在实验中,通过对比不同的瞬变电磁仪器,验证了现有仪器近距离探测含水异常的可行性。最后,通过实验得到了列车轨道干扰下可近距离监测的最小含水异常。
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Study on detection range of short distance water‐bearing anomaly via train‐borne transient electromagnetic method under interference of train tracks
The proportion of groundwater‐related diseases in the operational high‐speed railway tunnels in China is increasing and rapid and accurate disease monitoring is urgently needed. Therefore, it is a new attempt to monitor 5‐ to 10‐m water‐bearing anomalies in operating tunnel structures by using train‐borne transient electromagnetic method. The stationary interference source train tracks in the tunnel environment have serious electromagnetic interference to the monitoring of water‐bearing anomalies. Thus, this paper combines numerical simulations and indoor experiments to carry out research on the minimum water‐bearing anomalies that can be monitored at such close distances by train‐borne transient electromagnetic method under electromagnetic interference from train tracks. First, a comparative study of the electromagnetic characteristics of the water‐bearing anomalies when their own parameters change is carried out by numerical simulation, followed by a comparative analysis of the electromagnetic response of the water‐bearing anomalies under the interference of train tracks. For the missing electromagnetic response of the coil‐metal‐anomaly in the numerical simulation, a full‐scale physical model experiment is conducted to obtain the time range of the three interferences. Also in the experiments, the feasibility of existing instruments for close range water‐bearing anomalies detection is verified by comparing different transient electromagnetic instruments. Finally, the minimum water‐bearing anomalies that can be monitored in close proximity under the interference of train tracks are obtained experimentally.
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