土壤水分变异对探地雷达数据的影响

M. Ardekani, X. Neyt, D. Benedetto, E. Slob, B. Wesemael, P. Bogaert, C. Craeye, S. Lambot
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引用次数: 8

摘要

本文研究了天线足迹内土壤湿度的局地变率对探地雷达数据的影响。GprMax3D与Lambot和andr(2013)的GPR全波模型的组合用于一组无误差的测量。GprMax3D模拟用于几种基于物理配置的真实GPR测量。利用基于探地雷达全波模型的标定提取模拟数据的格林函数。将以地表小波反射为中心的水平局地土壤水分变异性反演结果与不同天线足迹内的平均土壤水分值进行了比较,结果表明-9 dB的天线足迹最优。土壤水分垂直变异性反演结果表明,浅层土壤水分分层对gpr反演的土壤水分值有显著影响,且与天线距地面高度密切相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil moisture variability effect on GPR data
In this paper the effect of local variability of soil moisture within the antenna footprint on GPR data is studied. A combination of GprMax3D with GPR full-wave model of Lambot and André (2013) is used for an errorless set of measurements. The GprMax3D simulations are used as real GPR measurements regarding several physical-based configurations. The Greens functions of the simulated data are extracted using calibrations based on GPR full-wave models. The inversion results of horizontal local soil moisture variability focusing on the surface wavelet reflection are compared with the averaged soil moisture values within different antenna footprints which led to the antenna footprint of -9 dB as the best. Finally, the inversion results of the vertical soil moisture variability shows significant effect of shallow soil moisture layering on the GPR-retrieved soil moisture values, which is highly correlated to the antenna height from the ground surface.
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