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Quantitative high-resolution observations of soil water dynamics in a complicated architecture using time-lapse ground-penetrating radar

机译:时移探地雷达对复杂建筑中土壤水分动力学的高分辨率定量观测

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摘要

High-resolution time-lapse ground-penetrating radar (GPR) observations of advancing and retreating water tables can yield a wealth of information about near-surface water content dynamics. In this study, we present and analyze a series of imbibition, drainage and infiltration experiments that have been carried out at our artificial ASSESS test site and observed with surface-based GPR. The test site features a complicated but known subsurface architecture constructed with three different kinds of sand. It allows the study of soil water dynamics with GPR under a wide range of different conditions. Here, we assess in particular (i) the feasibility of monitoring the dynamic shape of the capillary fringe reflection and (ii) the relative precision of monitoring soil water dynamics averaged over the whole vertical extent by evaluating the bottom reflection. The phenomenology of the GPR response of a dynamically changing capillary fringe is developed from a soil physical point of view. We then explain experimentally observed phenomena based on numerical simulations of both the water content dynamics and the expected GPR response.
机译:前进和后退地下水位的高分辨率时空穿透地面雷达(GPR)观测值可以提供有关近地表含水量动态的大量信息。在这项研究中,我们介绍并分析了一系列吸水,排水和渗透实验,这些实验已在我们的人工ASSESS测试现场进行,并通过基于地面的GPR进行了观察。测试现场具有复杂但已知的地下建筑,该建筑由三种不同类型的沙子构成。它可以研究GPR在各种不同条件下的土壤水分动力学。在此,我们特别评估(i)监测毛细条纹反射动态形状的可行性,以及(ii)通过评估底部反射来监测整个垂直范围内平均土壤水动力学的相对精度。从土壤物理角度发展了动态变化的毛细边缘的GPR反应的现象学。然后,我们将基于水分动力学和预期的GPR响应的数值模拟来解释实验观察到的现象。

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