探地雷达探测铁路路基含水率

J. Cai, S. Liu, L. Fu, Y. Feng
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引用次数: 5

摘要

在寒冷地区,铁路路基隆起是高速铁路的重要安全隐患。为了保证铁路的正常运行,有必要对路基含水率进行监测。采用探地雷达(GPR)共中点(CMP)测量法估算铁路路基含水率。由于路基是典型的层状介质,CMP法适用于含水率的测量。首先,对CMP数据进行速度谱分析,得到叠加速度,利用Dix公式计算垂向层段速度剖面。水分含量可由介电常数由托普公式求得,介电常数与速度有关。然而,在轨道路基等浅层薄土层中,速度分析存在许多问题。通过gprMAX的时域有限差分仿真,我们发现在速度分析过程中,由于偏移量较大,存在许多倍波和折射波,导致错误结果较多。在模拟结果的指导下,利用优化后的数据对实际数据进行速度分析。结果表明,所得结果与诱导极化率(IP)的计算结果吻合较好。实践证明,利用探地雷达探测路基含水率确实是可行的。该方法可广泛应用于路基水分检测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Detection of railway subgrade moisture content by GPR
In cold regions, heaving of the railway subgrade is an important security risk to high-speed railways. It is necessary to monitor the moisture content of the subgrade in order to ensure normal railway operation. Common midpoint (CMP) measurement using ground penetrating radar (GPR) was carried out to estimate the moisture content of railway subgrade. As the subgrade is typically a layered medium, the CMP method is suitable for moisture content measurement. Firstly, the CMP data is analyzed through the velocity spectrum to obtain the stacking velocity, from which the vertical interval velocity profile can be calculated by Dix's formula. The moisture content can be obtained by Topp's formula from dielectric constant, which depends on the velocity. However, velocity analysis has lots of problems in shallow and thin layers like rail subgrade. With the help of FDTD simulation by gprMAX, we find that there are many multiples and refracted waves which cause many false results during velocity analysis as the offset is large. Under the guidance of the simulated result, we use optimized data for velocity analysis of the real data. It is found that the final result is good and in accordance with the result of induced polarizability (IP). It is proven that it is indeed feasible to use GPR to detect the moisture content of subgrade. This method can be widely applied in subgrade moisture detection.
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