淡水水体中视频脉冲探地雷达问题的数值模拟结果

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY
O. Gulevich, L. Volkomirskaya, I. Mingalev, V. Varenkov, Z. Suvorova, O. Akhmetov, O. Mingalev, A. Reznikov
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引用次数: 0

摘要

水体表面探地雷达剖面在各种地质和工程研究中都有应用。在这里,我们给出了视频脉冲电磁信号在近底层具有介电常数和电导率梯度的淡水水体中传播的数值模拟结果。在快速变化过程的一般情况下,不受介质参数变化幅度的限制,应用麦克斯韦方程组的时域数值解方法。研究结果可以解释探地雷达资料相对于真实水深的明显下降以及底层雷达图上附加反射边界的出现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Results of numerical modelling of the problem of video pulse ground penetrating radar research in freshwater bodies
Ground-penetrating radar profiling on the surface of water bodies is applied in various geological and engineering studies. Here, we present the results of numerical simulation of the propagation of a video pulse electromagnetic signal in a freshwater body with gradients of the permittivity and electrical conductivity in the near-bottom layer. The method of numerical solutions of Maxwell's equations in the time domain is applied, in the general setting for rapidly changing processes, without restrictions on the magnitude of the change in the parameters of the medium. The results make it possible to explain the apparent decrease in water depth according to GPR data in comparison with the true depth and the appearance of additional reflecting boundaries on radargrams in the bottom layer.
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来源期刊
Russian Journal of Earth Sciences
Russian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.90
自引率
15.40%
发文量
41
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