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GPR trace analysis for coastal depositional environments of southern Brazil

机译:巴西南部沿海沉积环境的GPR追踪分析

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Ground penetrating radar (GPR) is increasingly used for subsurface detection of structures due to nondestructive characteristics. Use of the method for studies of coastal depositional environments is growing in southern Brazil. In this paper, we propose an analysis of traces in the variation in signal amplitude, integrated with the degree of compaction determined in the drill hole, for the characterization of depositional environments in regressive barriers. Signal attenuation with depth was interpreted from the least squares method for two cases of contrast in volume of rainfall. Results show efficiency of the methodology in determination of contacts between different deposits at depth, showing an increase in signal amplitude at the contact between the original deposits from low to high compaction. Precipitation is not relevant for signal attenuation in the sandy deposits studied. (C) 2019 Elsevier B.V. All rights reserved.
机译:由于非破坏性特征,地面穿透雷达(GPR)越来越多地用于结构的地下检测。 巴西南部的沿海沉积环境研究的使用方法正在增长。 在本文中,我们提出了在信号幅度变化中的迹线分析,与钻孔中确定的压实程度集成,用于表征回归障碍中的沉积环境。 利用深度的信号衰减是从降雨量的两个案例中的最小二乘法解释。 结果表明,在深度的不同沉积物之间测定接触的方法的效率,显示出从低到高压实的原始沉积物之间的触点处的信号幅度的增加。 沉淀不适用于研究中的砂岩沉积物中的信号衰减。 (c)2019年Elsevier B.V.保留所有权利。

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