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用随机方法模拟唐山7.1级余震地震动场
引用本文:李启成,宋志勇.用随机方法模拟唐山7.1级余震地震动场[J].国际地震动态,2012(7):13-19.
作者姓名:李启成  宋志勇
作者单位:1. 辽宁工程技术大学,阜新123000;黑龙江科技学院,哈尔滨150027
2. 黑龙江科技学院,哈尔滨,150027
基金项目:黑龙江省教育厅科学技术研究项目
摘    要:在系统介绍用随机方法模拟地震动的基础上,用该方法模拟了唐山7.1级余震地震动场。模拟结果表明,唐山地区发生MS7.1级余震时,该地区产生了强烈的地震动,很多区域加速度峰值超过400cm/s2,地震断层面长65km,宽13.5km,地震过程中断层面的平均滑动为1.08m。模拟与记录的地震动持时符合得不好,其原因是随机方法中的经验关系大都是在美国大陆得到的,所以建议加强中国大陆相应的地震动经验关系的研究,使随机方法能更好地适用于中国大陆。尽管如此,由于用随机方法模拟的地震动峰值和反应谱与记录符合得比较好,这些模拟结果可以作为建筑物抗震设防的地震动输入。

关 键 词:地震动  迁安  随机方法

Ground motion field simulation of Tangshan Ms7.1 aftershock with stochastic method
Li Qicheng , Song Zhiyong.Ground motion field simulation of Tangshan Ms7.1 aftershock with stochastic method[J].Recent Developments in World Seismology,2012(7):13-19.
Authors:Li Qicheng  Song Zhiyong
Institution:1) Liaoning Technical University, Fuxin 123000, China 2) Heilongjiang Institute of Science&Technology, Harbin 150027, China
Abstract:Based on the systematic introduction of ground motion simulation with sto- chastic method, the ground motion fields of Tangshan Ms7.1 aftershock was; simulated with this method. Results show that the strong ground motion produced in Qian' an region when earthquake (Ms7.1) took place. Peak acceleration exceeds 400 cm/s2. The fault is 65 km long, 13.5 km wide, and its average slip is 1.08 m. The simulated seismic duration do not accord with that of the real records. The reason may lie in that the experiential relations used in simulation were got from the American continent. Therefore, it is suggested that experi- mental relations for Chinese continent should be studied. However, the peak acceleration and response spectrum obtained by simulation are in good agreement wflh real records, which can be used as the seismic motion input of anti-seismic design of construction.
Keywords:ground motion  Qian'an  stochastic method
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