Combining cross-hole georadar velocity and attenuation tomography for site characterization: a case study in an unconsolidated aquifer

J. Tronicke, H. Paasche, K. Holliger, A. Green
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引用次数: 5

Abstract

Information extracted from crosshole georadar data has been used to characterize a gravel- and sand-dominated aquifer. Inversions of direct arrival traveltimes and amplitudes have provided electromagnetic velocity and attenuation tomograms that have allowed critical hydrological structures and parameters to be determined. An integrated interpretation of the velocity and attenuation tomograms was performed via a k-means cluster analysis. As a result of this multivariate statistical analysis, major trends in the relationship between velocity and attenuation were identified, thus enabling us to outline the major hydrostratigraphicu nits ofthe surveyedd eposit.
结合井间地质雷达速度和衰减层析成像进行现场表征:一个松散含水层的案例研究
从井间地质雷达数据中提取的信息已用于描述砾石和砂岩为主的含水层。直接到达时间和振幅的反演提供了电磁速度和衰减层析图,从而可以确定关键的水文结构和参数。通过k均值聚类分析对速度和衰减层析图进行综合解释。通过这种多元统计分析,确定了速度与衰减之间关系的主要趋势,从而使我们能够概述所调查矿床的主要水文地层单元。
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