Assessing uncertainties in determining GPR ground wave velocities: An approach based on spectral velocity analysis

G. Hamann, J. Tronicke
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引用次数: 1

Abstract

We propose a spectral velocity analysis approach to determine ground wave velocity from multi-offset or common midpoint (CMP) ground-penetrating radar (GPR) data. Our method is based on the linear moveout equation of ground wave arrivals and uses the unnormalized crosscorrelation to measure the coherency of the waveforms across the data gather. Peaks in the resulting velocity spectra indicate optimum velocities of linear events present in the data. Thus, our method is conceptually similar to CMP velocity analysis of reflected events where velocity spectra are computed using different coherency measures along hyperbolic trajectories. Furthermore, we propose a simple method to estimate uncertainties of the determined velocities. The introduced measure of uncertainty is based on the width of the maxima in the calculated velocity spectrum. Using different synthetic data examples, we test our approach and evaluate the influence of the true subsurface velocity, the surveying geometry, and the signal frequency on the accuracy of ground wave velocity estimates. Furthermore, we demonstrate the impact of these uncertainties on soil water content derived from these velocity values.
评估确定探地雷达地波速度的不确定性:一种基于频谱速度分析的方法
我们提出了一种光谱速度分析方法,从多偏移或共中点(CMP)探地雷达(GPR)数据中确定地波速度。我们的方法是基于地波到达的线性移出方程,并使用非归一化相互关系来测量数据集上波形的相干性。所得速度谱中的峰表示数据中出现的线性事件的最佳速度。因此,我们的方法在概念上类似于反射事件的CMP速度分析,其中速度谱是沿着双曲线轨迹使用不同的相干测量来计算的。此外,我们提出了一种简单的方法来估计确定速度的不确定性。引入的不确定度度量是基于计算速度谱中最大值的宽度。利用不同的合成数据实例,我们验证了我们的方法,并评估了真实地下速度、测量几何形状和信号频率对地波速度估计精度的影响。此外,我们还证明了这些不确定性对由这些流速值得出的土壤含水量的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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