利用近场和远场探地雷达数据全波反演估算土壤水分:比较评价

A. Tran, F. Wiaux, S. Lambot
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引用次数: 10

摘要

采用一种新的近场探地雷达天线模型对比利时中部一个农业样带的土壤湿度进行了表征。该测量系统由连接喇叭天线的矢量网络分析仪和安装在摩托车上的差分GPS组成,用于快速采集数据。数值实验表明,由于天线与介质的距离较近,近场探地雷达数据比远场数据对土壤介电特性更敏感。在现场测量中,模拟的远场和近场探地雷达数据与实测值吻合较好。然而,由于近场数据的渗透深度更深,足迹更小,对土壤介电常数的灵敏度更高,近场数据估计的土壤含水量比远场数据更高,更符合Theta Probe测量结果。土壤湿度的空间格局主要受地形控制,而时间变化则受降雨强度和降雨事件与试验的时间差的影响。该方法在田间尺度上对土壤水分进行时空表征具有广阔的应用前景。
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 estimation using full-wave inversion of near- and far-field ground-penetrating radar data: A comparative evaluation
A new near-field ground-penetrating antenna model was applied for characterization of soil moisture in an agricultural transect in central Belgium. The measurement system consists of a vector network analyzer connected with a horn antenna and a differential GPS mounted on a motorcycle for quick data acquisition. Numerical experiments show that near-field GPR data are more sensitive to the soil dielectric properties than far-field data due to nearer distance between the antenna and medium. For the field measurements, the modeled GPR data from far-field and near-field configurations agree very well with the measured ones. However, soil water content estimated from near-field data is higher and more in agreement with Theta Probe measurements than far-field owning to the deeper penetration depth, smaller foot print and larger sensitivity with soil permittivity of near-field data. The results also show that the spatial pattern of the soil moisture is mainly controlled by the topography, while temporal variability is influenced by the rainfall intensity and time lag between rainfall event and experiment. The proposed approach shows a promising potential for temporal and spatial characterization of soil moisture at the field scale.
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