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首页> 外文期刊>Engineering Geology >Assessing the internal structure of landslide dams subject to possible piping erosion by means of microtremor chain array and self-potential surveys
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Assessing the internal structure of landslide dams subject to possible piping erosion by means of microtremor chain array and self-potential surveys

机译:通过Microtremor链阵列和自潜能调查,评估乘坐水坝的内部结构。

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摘要

An integrated geophysical approach comprising microtremor chain array and self-potential surveys was used to assess the internal structure of landslide dams subject to possible piping erosion in selected sites in Japan and Kyrgyzstan. The non-invasive geophysical approach is cost effective, environmentally friendly and portable, and hence, it has proven to be valuable for the geotechnical assessment of landslide dams where piping can trigger failure of the dam. While the microtremor chain array survey results revealed the internal structure of the landslide dam, the self-potential survey results indicated the path of anomalous seepage zones. In the surveyed sites of long-existing landslide dams, the presence of a seepage path in the dam was confirmed by a good correlation between the areas of low phase velocity and large negative self-potential anomalies. In summary, this integrated geophysical approach could be useful for the early risk assessment of landslide dams and prediction of landslide dam failure by piping.
机译:包括微调链阵列和自潜能调查的集成地球物理方法用于评估山体积坝的内部结构,在日本和吉尔吉斯斯坦的选定地点中可能的管道侵蚀。非侵入性地球物理方法具有成本效益,环保和便携,因此,已证明对山雀滑坡的岩土性评估是有价值的,其中管道可以触发大坝失败的地方。虽然MicroTremor链阵测量结果显示了山体滑坡大坝的内部结构,但自潜能调查结果表明了异常渗流区的路径。在长期现有滑坡坝的调查遗址中,通过低相速度和大负离子势异常之间的良好相关性来确认大坝中渗流路径的存在。总之,这种集成的地球物理方法可用于山体滑坡的早期风险评估和通过管道预测滑坡坝失效。

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