近斷層區(qū)域劃分及近斷層速度脈沖型地震動模擬
[Abstract]:Near-fault (near-fault) ground motion refers to the ground motion near the seismogenic fault. This kind of ground motion has attracted wide attention in the field of seismic engineering because it has different characteristics from far-field earthquakes and has a strong destructive effect on long-period structures. In this paper, the influence range of near-field region and the simulation of near-fault velocity pulse type ground motion are studied, so as to determine the parameter input of simulation velocity pulse and the synthetic method of near-fault velocity pulse type ground motion. According to the above research contents, this paper has done the following work: (1) reviewing the literature to summarize the present situation of recent fault seismic research and collecting 1296 seismic records of fault distance from 90kmm (horizontal 977, vertical 319). The earthquake motion is analyzed. (2) 19 parameters of potential failure potential are selected and calculated. Pearson correlation coefficient method is used to calculate the correlation coefficient between the parameters of potential failure potential. (3) according to fault type, The site category and magnitude range divide the records into 20 groups (11 horizontal groups, 9 vertical groups), determine the parameter combination of each group near fault area, and obtain the critical fault distance of each group of earthquakes by piecewise function fitting. Furthermore, different fault types, site types and the range of near-fault area under magnitude are determined. (4) based on wavelet analysis, velocity pulse earthquakes are identified, and pulse components in velocity pulse earthquakes are extracted, and the distribution characteristics of pulses are analyzed. The empirical formulas of pulse period T p, pulse peak velocity PGV and pulse peak corresponding time t are obtained by statistical regression. (5) the pulse period T p calculated based on wavelet analysis method and the pulse period calculated based on velocity response spectrum method are analyzed. The ratio of Tsv to Tsv and its influencing factors. (6) by comparing the power spectrum of pulse component with that of non-pulse component, we find that the ratio of Tsv to Tsv is very high. The calculation method of low frequency boundary frequency f _ r and the quantitative relation between f _ r and pulse period T _ p are determined. (7) the Tian pulse model is improved and the low-frequency pulse component is generated by using the statistical results of velocity pulse seismic parameters as parameters. Superposed with the high frequency component obtained by the response spectrum, the near fault velocity pulse ground motion is formed.
【學(xué)位授予單位】:西南交通大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2015
【分類號】:P315.9
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