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首页> 外文期刊>物理探查 >An experimental study on the upper limits of wavelength of Rayliegh wave estimated by the Frequency-Wavenumber spectrum method or the Spatial Autocorrelation method using a microtremor array technique
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An experimental study on the upper limits of wavelength of Rayliegh wave estimated by the Frequency-Wavenumber spectrum method or the Spatial Autocorrelation method using a microtremor array technique

机译:频率-波数谱法或空间自相关法微震阵列技术估算瑞利波波长上限的实验研究

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摘要

In a microtremor array technique phase velocities must be obtained in a wide-range of wavelength in order to estimate underground structures precisely. Frequency-wavenumber spectrum (F-K) method and Spatial auto-correlation (SPAC) method are used to estimate phase velocities of surface waves in microtremors. Recent studies using techniques of numerical simulation or field experiment show that SPAC method can observe longer wavelength possible to estimate phase velocities in microtremors than F-K method. We also examine and discuss the upper limits of wavelength calculated using microtremor array data by the two kinds of methods. For the above purpose, microtremor array observations were carried out in four sites of Morioka city, Iwate Prefecture. The array configuration is a triangle with seven vertical seismometers. The array size defined by the distance between a center and an apex of the triangle ranges from 10 m to 100 m. Three or four arrays with different sizes were used at one observation site. Phase velocities of Rayleigh wave in microtremors were observed by F-K method and SPAC method. We defined a standard phase velocity which was calculated from all the array records at one site. To estimate the upper limits of wavelength, a residual between standard phase velocity and observed phase velocity for each array was defined within 0.1. The range of the estimated upper limits of wavelengths by F-K method were from 2.3 to 6.8 times for a distance between a center and an apex of the triangle array, and those by SPAC method were ranging from 3.2 to 17.2 times. These results show that SPAC method can observe longer wavelength possible to estimate phase velocities in microtremors than F-K method.
机译:在微震阵列技术中,必须在较宽的波长范围内获得相速度,以便精确估算地下结构。频率波数谱(F-K)方法和空间自相关(SPAC)方法用于估计微震中表面波的相速度。最近使用数值模拟或现场实验技术进行的研究表明,与F-K方法相比,SPAC方法可以观察到更长的波长来估计微震中的相速度。我们还将检查和讨论通过两种方法使用微震阵列数据计算出的波长上限。为了上述目的,在岩手县盛冈市的四个地点进行了微震阵列观测。阵列配置是一个具有七个垂直地震仪的三角形。由三角形的中心与顶点之间的距离定义的阵列大小在10 m至100 m的范围内。在一个观察点使用三个或四个大小不同的阵列。用F-K法和SPAC法观察微震中瑞利波的相速度。我们定义了一个标准相速度,该速度是从一个站点上的所有阵列记录计算得出的。为了估计波长的上限,每个阵列的标准相速度和观察到的相速度之间的残差定义在0.1以内。对于三角形阵列的中心和顶点之间的距离,通过F-K方法估计的波长上限的范围是2.3至6.8倍,而通过SPAC方法估计的波长上限的范围是3.2至17.2倍。这些结果表明,与F-K方法相比,SPAC方法可以观察到更长的波长来估计微震中的相速度。

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