亮蓝渗透实验延时三维探地雷达成像

N. Allroggen, J. Tronicke, L. van Schaik
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引用次数: 1

摘要

指进、漏斗流或大孔流导致的优先流动导致了小尺度的入渗空间变异性。在地块尺度(~ 1 m × 1 m)上,表征这种渗透模式的常用方法是使用染料示踪剂进行喷洒实验。通常,在使用选定的垂直二维切片的数字照片进行挖掘后分析所得到的图案。观察到的优先流道在厘米到分米的宽度范围内变化,往往揭示出相当复杂的三维流动网络。在这项研究中,我们研究了基于表面的3D探地雷达(GPR)从这种染料示踪剂实验中成像地下流动模式的潜力。我们的方法是基于使用500 MHz天线的时间带3D(即4D)探地雷达调查。在一个案例研究中,我们将基于gpr的成像方法的结果与挖掘后的数字照片中观察到的模式进行了比较。我们的研究结果表明,GPR是一种可行的非侵入性3D成像技术,与传统侵入方法相比,它提供了成像相关浸润模式的时间演变的机会。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Time-lapse 3D GPR imaging of brilliant blue infiltration experiments
Preferential flow due to fingering, funnelling or macropore flow results in small scale spatial variability in infiltration. On the plot scale (~ 1 m × 1 m), a common method to characterize such infiftration patterns are sprinkling experiments using dye tracers. Typically, the resulting patterns are analyzed after excavation using digital photographs of selected vertical 2D slices. The observed preferential flow paths vary in scafe from centimeters to decimeters width, often reveafing rather compficated 3D flow networks. In this study, we examine the potential of surface based 3D ground-penetrating radar (GPR) to image subsurface flow patterns from such dye tracer experiments. Our approach is based on time-tapse 3D (i.e., 4D) GPR surveys using 500 MHz antennas. In a case study, we compare the resufts from our GPR-based imaging approach to the patterns observed in digitaf photographs after excavation. Our resuits show that GPR is a feasibie technique to non-invasiveiy image major flow patterns in 3D and, compared to the ctassicaf invasive approach, provides the opportunity to image the temporat evofution of the associated infiltration patterns.
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