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Application of surface wave and micro-tremor survey in landslide investigation in the Three Gorges reservoir area

机译:面波和微震测量在三峡库区滑坡调查中的应用

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The surface wave and micro-tremor survey are new methods of the engineering geophysicalinvestigation. They have been widely used in recent years because they are of low cost and easy operation andthey give the dynamic property of the ground,i.e. the shear wave velocity. This paper discusses the applicationof micro-tremor and surface wave in the Qianjiangping and Shuping landslides of the Three Gorges reservoirarea. For surface wave survey,we analyzed the dispersion of the recorded data and then estimated the shear wavevelocity structure by phase velocity inversion. For micro-tremor survey,we observed the ground micro-tremorsignals,and analyzed them by fast Fourier transform method (FFT). The soil response to frequency of groundmicro-tremor is revealed and the function with frequency-dependence and frequency-selection of micro-tremorfor different foundation strata are investigated. The vertical to horizontal spectra ratio (H/V,Nakamura technique)of micro-tremor observed at the surface was used to evaluate the site's predominant period. All of these haveprovided a more dependable basis for the landslide material classification and for analysis of these hazardousphenomena. The experimental foundation and the deduction process of the method were described in detail.Comparison of the geophysical investigation results with the geological data shows their good agreement,thusproving the applicability of the methods in landslide study.
机译:地表波和微震测量是工程地球物理研究的新方法。由于它们成本低廉,易于操作并且具有地面的动态特性,因此近年来已被广泛使用。剪切波速度。讨论了微震和地表波在三峡库区钱江坪和树坪滑坡中的应用。对于表面波测量,我们分析了记录数据的离散度,然后通过相速度反演来估计剪切波速度结构。对于微震调查,我们观察了地面微震信号,并通过快速傅里叶变换法(FFT)对其进行了分析。揭示了土壤对地面微震频率的响应,研究了不同基础层微震的频率依赖性和频率选择功能。在表面观察到的微震的垂直与水平光谱比(H / V,Nakamura技术)用于评估该部位的主要时期。所有这些为滑坡物质的分类和这些危险现象的分析提供了更可靠的依据。详细描述了该方法的实验基础和推导过程。地球物理调查结果与地质资料的比较表明两者具有很好的一致性,从而提高了该方法在滑坡研究中的适用性。

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