Study of GPR image characteristics of dams' hidden weak points

S. Ge, Boyong Sun, Yonghui Zhao, Jun Chen, Lanbo Liu
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引用次数: 1

Abstract

For using GPR as a non-destructive testing to the hidden weak points in dam or seawall, how to reasonably analysis the GPR image and obtain the exact interpretations is still an unsolved problem. Combined with the dam engineering features and detection experiences, geophysical models of typical hidden weak points, such as horizontal non-homogeneous layer, slope non-homogeneous zones bearing coarse-grained or fine-grained material mezzanine and cavities filled with different materials in cohesive soil dam, were set up for numerical simulation. Numerical simulations of radar wave performance in these typical hidden weak point models were conducted by using the finite difference time domain (FDTD) solution over a 2D space, with a perfectly matched layer (PML) absorbing boundary conditions. Simulated results illustrated that spatial distribution of hidden weak points can be interpreted from the GPR image. On the condition of complicated environment, interpretation of local hidden weak point character relies upon careful analysis on dynamic characteristics including phase and frequency features of reflected wave, and diffracted wave character. Based on the wave field characteristics of the typical hidden weak points, some GPR images collected at a reservoir dam and seawall had been interpreted. Engineering applications indicated that appropriate numerical model construction and simulation interpretation could be a helpful guide to real GPR test for hidden weak points.
大坝隐蔽弱点探地雷达图像特征研究
利用探地雷达对大坝或海堤的隐蔽弱点进行无损检测,如何对探地雷达图像进行合理的分析并获得准确的解译仍然是一个有待解决的问题。结合大坝工程特点和探测经验,建立了黏性土坝中水平非均质层、含粗粒或细粒材料夹层的边坡非均质带、充填不同材料的空腔等典型隐蔽弱点的地球物理模型进行数值模拟。利用时域有限差分(FDTD)方法在二维空间上,采用完全匹配层(PML)吸收边界条件,对这些典型的隐藏弱点模型中的雷达波性能进行了数值模拟。模拟结果表明,探地雷达图像可以解释隐藏弱点的空间分布。在复杂环境下,局部隐藏弱点特征的解释依赖于对反射波的相位、频率特征和绕射波特征等动态特性的仔细分析。根据典型隐蔽弱点的波场特征,对某水库大坝和海堤的探地雷达图像进行了解译。工程应用表明,适当的数值模型构建和仿真解释有助于指导实际探地雷达测试中隐藏的弱点。
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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