Simultaneous multi-channel GPR measurements for soil characterization

M. Kaufmann, A. Klotzsche, H. Vereecken, J. van der Kruk
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引用次数: 2

Abstract

For agricultural studies, the determination of soil properties such as electromagnetic wave velocity and electrical conductivity is essential for characterizing important hydrological parameters such as soil water content. GPR has shown a high potential to estimate these parameters by using either large-scale common offset measurements and, point-scale common mid-point (CMP) or wide-angle reflection and refraction (WARR) measurements. A new multi-channel ground penetrating radar system combines both techniques and allows fast simultaneous measurements with up to eight channels. Thereby, up to seven receivers are continuous performing common offset measurements that can be rearranged to WARRs. This allows fast tracking of velocity changes along a measurement profile. Here, we present multi-channel and single-channel 500 MHz GPR data measured on a profile with different soil characteristics to demonstrate the potential of this new approach. To eliminate time shifts that are caused by the different cables and receivers of the multi-channel system a time offset correction is suggested. For single- and multi-channel WARR measurements velocity variations of the ground wave along the profile are determined using the semblance analysis. The comparison of the single- and multi-channel data indicate that multi-channel GPR is able to provide velocities similar to single-channel measurements, and, that the method can be used to determine changes of the groundwave velocity with a high spatial coverage.
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同时多通道探地雷达测量土壤特性
在农业研究中,土壤特性(如电磁波速度和电导率)的测定对于表征土壤含水量等重要水文参数至关重要。GPR已经显示出利用大规模共偏移测量和点比例尺共中点(CMP)或广角反射和折射(WARR)测量来估计这些参数的巨大潜力。一种新的多通道探地雷达系统结合了这两种技术,并允许多达8个通道的快速同时测量。因此,多达7个接收器连续执行可重新排列为warr的常见偏移测量。这允许沿着测量剖面快速跟踪速度变化。在这里,我们展示了在具有不同土壤特征的剖面上测量的多通道和单通道500 MHz GPR数据,以展示这种新方法的潜力。为了消除多通道系统中不同的电缆和接收机所引起的时移,提出了一种时间偏移校正方法。对于单通道和多通道WARR测量,使用相似分析确定了沿剖面的地波速度变化。单通道和多通道探地雷达数据的对比表明,多通道探地雷达能够提供与单通道测量相似的速度,并且该方法可以用于确定高空间覆盖下的地波速度变化。
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