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Application of the microtremor measurements to a site effect study

机译:微震测量在部位效应研究中的应用

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Abstract Earthquake has left much life and property damages. The occurrence of such events necessitates the execution of plans for combating the earthquakes. One of the most important methods for combating earthquakes includes assessing dynamic characteristics of soil and site effect. One of the methods by which one can state dynamic characteristics of the soil of an area is the measurement of microtremors. Microtremors are small-scale vibrations that occur in the ground and have an amplitude range of about 0.1–1 microns. Microtremor measurement is fast, applicable, cost-effective. Microtremor measurements were taken at 15 stations in the Babol, north of Iran. Regarding H / V spectral ratio method, peak frequency and amplification factor were calculated for all microtremor stations. According to the analysis, the peak frequency varies from 0.67 to 8.10?Hz within the study area. Also, the authors investigated the validity of the results by comparing them with SESAME guidelines and geotechnical conditions of study area. The microtremor analysis results are consistent with SESAME guidelines and geotechnical condition of study area. The results show that the microtremor observations are acceptable methods for assessing dynamic characteristics of soil and site effect in the Babol City.
机译:摘要地震给人们的生命和财产造成了巨大破坏。这些事件的发生使得必须执行抗震计划。应对地震最重要的方法之一是评估土壤的动态特性和场地效应。可以描述一个地区土壤动态特性的一种方法是测量微震。微震是发生在地面的小规模振动,振幅范围约为0.1-1微米。微震测量快速,适用,具有成本效益。在伊朗北部的巴博尔的15个站点进行了微震测量。关于H / V谱比法,计算了所有微震台站的峰值频率和放大因子。根据分析,研究区域内的峰值频率在0.67至8.10?Hz之间变化。此外,作者通过将结果与SESAME指南和研究区域的岩土条件进行比较,研究了结果的有效性。微震分析结果与SESAME指南和研究区域的岩土条件一致。结果表明,微震观测是评估巴博尔市土壤动力特性和场地效应的可接受方法。

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