利用GprMax实现ZOP水平井全波形反演

A. Klotzsche, J. van der Kruk, G. He, H. Vereecken
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引用次数: 1

摘要

探地雷达数据的全波形反演在许多应用中显示出巨大的潜力,可以获得精确、定量的高分辨率地下图像。我们实现了一种新的全波形反演方法,该方法结合了精确的3D正演建模方法和混合复杂演化方法,该方法结合了标准过程无法解决的复杂波相互作用和干扰。该方法应用于在水平钻孔中获取的零偏移剖面GPR数据,以监测不同土壤和处理条件下的土壤含水量和根系吸水情况。使用标准的基于射线的处理方法,由于临界折射空气波和穿过地下的直接波的干扰,确定的接近表面的介电常数值不可靠。综合研究表明,在深度0.1 m和0.2 m处的痕迹受到这些干扰的影响,因此无法通过标准的基于射线的方法获得可靠的介电常数值和土壤含水量值。利用新的全波形反演方法,在水平钻孔0.06 ~ 1.16m之间的3个不同处理地块和6个不同深度位置获得了可靠的介电常数和土壤含水量结果。反演结果与实测数据吻合较好,得到了各深度的定量介电常数结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
GPR full-waveform inversion of horizontal ZOP borehole data using GprMax
Full-waveform inversion of GPR data has shown a high potential in many applications to obtain accurate and quantitative high resolution images of the subsurface. We implemented a new full-waveform inversion that combines an accurate 3D forward modeling approach with a shuffled complex evolution method that incorporates the complicated wave interactions and interferences that cannot be resolved by standard processes. This new approach is applied to zero-offset profile GPR data that were acquired in horizontal boreholes to monitor soil water content and water uptake by roots under different soil and treatment conditions. Using standard ray-based processing methods, the determined permittivity values close to the surface were not reliable due to interferences from the critically refracted air wave and the direct wave through the subsurface. Synthetic studies showed that traces at depths 0.1 m and 0.2 m are affected by these interferences and hence no reliable permittivity values and soil water content values can be obtain by standard ray-based approaches. The new full-waveform inversion was used to obtain reliable permittivity and soil water content results for three different treatment plots and six different depth positions between 0.06-1.16m of the horizontal boreholes. The inverted results show a good fit with the observed data and quantitative permittivity results were obtained for all depths.
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