利用导引探地雷达波沿孔内金属圆柱体探测介电常数的数值研究

S. Stadler, J. Igel
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引用次数: 6

摘要

我们利用有限差分(FDTD)模拟,在钻孔中使用制导探地雷达(GPR)波进行介电常数探测。本文介绍的方法使用GPR天线,该天线放置在井眼旁边,其中降低了金属波导。天线在表面发出的电磁(EM)信号与波导耦合,并从金属波导的底端反射。通过对传播时间的分析,可以得到波速、介电常数和含水量在特定深度区间的精确垂直分布。我们对波导周围的场分布、塑料套管的影响以及该方法在层状介质中的分辨率进行了数值研究。在本研究中,通过实际400 MHz领结式探地雷达天线的三维模型,将探地雷达信号作为源引入仿真。我们复制了天线的基本部件,例如天线领结和金属外壳,以准确地再现发射信号。此外,高对比介电常数层的最大垂直分辨率约为5 cm,并推导了一个修正套管对介电常数计算影响的公式。我们设想,这种方法和这项研究的见解使土壤探测比其他现有的探地雷达方法或时域反射法(TDR)更精确。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A numerical study on using guided GPR waves along metallic cylinders in boreholes for permittivity sounding
We performed a numerical study on using guided ground-penetrating radar (GPR) waves in boreholes for permittivity soundings using finite-difference (FDTD) simulations. The method presented here uses a GPR antenna that is placed next to a borehole in which a metal waveguide is lowered. Electromagnetic (EM) signals that the antenna sends out on the surface, couple to the waveguide and are reflected from the bottom end of the metal waveguide. Analysing the traveltimes yields accurate vertical distributions of the wave velocity, permittivity and water content in specified depth intervals. We performed numerical studies of the field distribution around the waveguide, the influence of the plastic borehole casing, as well as the resolution capabilites of the method in layered media. In this study, as a source, the GPR signal is introduced in the simulation via a 3D model of a real 400 MHz bowtie GPR antenna. We replicated the essential components of the antenna, e.g. the antenna bowties and metal casing, to accurately reproduce the transmitted signal. The guided wave has a skin depth drop in amplitude away from the waveguide of about 4.1 cm, Furthermore a maximum vertical resolution of high-contrast permittivity layers of about 5 cm is possible, and a formula for correcting the effect of the borehole casing on permittivity calculations is derived. We envision that this method and the insight from this study enables more precise soil soundings than other established GPR methods or time-domain reflectometry (TDR).
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