José E. Barradas-Hernández, Sergio Márquez-Domínguez, Franco Antonio Carpio-Santamaria, Alejandro Vargas-Colorado, Abigail Zamora-Hernández, Roberto Rivera-Baizabal
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引用次数: 0
Abstract
The data presented here are the result of microtremor measurements at 44 points in three different soil types classified according to their fundamental vibration frequencies, on the metropolitan area of Veracruz-Boca del Río, Mexico. These Data are raw and was obtained using a GÜRALP 6TD model broadband orthogonal triaxial seismometer with an integrated 24-bit digitizer with a minimum recording time of 30 min and a recording rate of 100 samples per second (sps). The microtremor records were used to construct the H/V spectral ratios using the method of Nakamura. These H/V spectral ratios are a good approximation of the transfer function between the vibration waves in the sediment and the rigid stratum. Therefore, they can be used to construct seismic microzonation maps, seismic intensity maps and spectra for designing seismic resistant structures. One-dimensional stratigraphic soil models were obtained by processing the H/V spectral ratios. The relevant data from these models are layer thickness, primary wave velocities (Vp), secondary wave velocities (Vs) and density. These models represent a mathematical approximation of the soil structure that can be used to dynamically classify it according to Mexican technical codes.
这里展示的数据是在墨西哥Veracruz-Boca del Río的大都市区,根据其基本振动频率,在三种不同土壤类型的44个点进行微震测量的结果。这些原始数据是使用GÜRALP 6TD型宽带正交三轴地震仪获得的,该地震仪带有集成的24位数字化仪,最小记录时间为30分钟,记录速率为每秒100个样本(sps)。利用微震记录,采用Nakamura方法构建H/V谱比。这些H/V谱比很好地近似了泥沙和刚性地层中振动波之间的传递函数。因此,它们可用于构造地震微区划图、地震烈度图和抗震结构设计谱。通过对H/V谱比的处理,得到一维地层土壤模型。这些模型的相关数据是层厚、一次波速度(Vp)、二次波速度(Vs)和密度。这些模型代表了土壤结构的数学近似,可用于根据墨西哥技术规范对其进行动态分类。
期刊介绍:
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