关于加速度在仪器烈度计算中的应用
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
地震动加速度作为计算仪器烈度的地震动参数是大家所公认的。美国Shake Map系统仪器烈度的计算利用水平向加速度峰值,日本气象厅则利用持时大于等于0.3 s的等效加速度峰值,选择何种加速度,是个值得探讨的问题,本文通过对大量强震记录的统计分析,讨论了不同持时下的有效峰值加速度和三分向合成加速度的关系。
It well be known thatthe acceleration astheimportant ground motion parameter for calculating the instrumental intensity. The horizontal peak acceleration and the effective peak acceleration has been adopted forthe rapid instrumental intensity maps for Shake Map and JMA. However,which of the acceleration will be adopted was a valuable discussing problem. The effect of filtering frequency on the peak acceleration was discussed by the statistic analysis of a large number of strong motion records,how to select the peak acceleration was discussed,the Aof which satisfies the different duration or the Aallwhich is synthesized by three components.
引文
[1]金星,等.地震仪器烈度标准研究报告[R].福州:福建省地震局,2010.
    [2]胡聿贤.地震工程学[M].北京:地震出版社,1988.
    [3]李敏.地震动加速度反应谱与地震烈度的关系研究[D].哈尔滨:中国地震局工程力学研究所硕士研究生学位论文.2010.
    [4]David J.Wald,M.Eeri,et al.Tri Net"Shake Map":Rapid generation of peak ground motion and intensity maps for earthquakes in southern California.Earthquake Spectra,Vol.15,No.3,1999.
    [5]胡聿贤.地震安全性评价技术教程[M].北京:地震出版社,1999.
    [6]周正华,周雍年,赵刚.强震近场加速度峰值比和反应谱统计分析[J].地震工程与工程振动,2002,22(3):15-18.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心