以频率、盐度和温度为函数的探地雷达表征水

K. Jadoon, F. André, J. van der Kruk, E. Slob, H. Vereecken, S. Lambot
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引用次数: 1

摘要

通过室内实验,验证了探地雷达(GPR)全波形正反演方法在水中的电磁波传播。该探地雷达系统由矢量网络分析仪与空射0.8-2.2 GHz喇叭天线相结合构成超宽带步进频率连续波雷达。利用现有的电学模型估计了水的表观频率、盐度和温度相关的介电常数和电导率。利用这些模型对雷达数据进行了模拟,得到了与实验室测量结果非常吻合的结果。忽略频率、盐度和温度的影响会导致不太令人满意的结果,特别是在信号振幅方面。雷达数据的反演允许重建空气和水层厚度,并在一定程度上,水的电性质。该分析特别表明,与常用的GPR正演和逆演简化方法相比,使用适当的水电模型具有优势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ground-penetrating radar characterization of water as a function of frequency, salinity and temperature
We conducted a laboratory experiment to test the ground penetrating radar (GPR) full-waveform forward and inverse modeling approach for electromagnetic wave propagation in water. The GPR system consisted of a vector network analyzer combined with an air-launched, 0.8–2.2 GHz horn antenna, thereby setting up an ultra wideband stepped-frequency continuous-wave radar. The apparent frequency-, salinity-, and temperature-dependent dielectric permittivity and electrical conductivity of water were estimated by using existing electrical models. Using these models, the radar data could be simulated and a remarkable agreement was obtained with the laboratory measurements. Neglecting the frequency-, salinity-, and temperature-effects led to less satisfactory results, especially regarding signal amplitude. Inversion of the radar data permitted to reconstruct the air and water layer thicknesses, and to some extent, the water electrical properties. This analysis particularly showed the benefit of using proper water electrical models compared to commonly used simplified approaches in GPR forward and inverse modeling.
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