肖梅玲, 叶燎原, 李淑一. 谐波小波下的地震能量输入模型[J]. 云南大学学报(自然科学版), 2012, 34(S2): 62-67.
引用本文: 肖梅玲, 叶燎原, 李淑一. 谐波小波下的地震能量输入模型[J]. 云南大学学报(自然科学版), 2012, 34(S2): 62-67.
XIAO Mei-ling, YE Liao-, LI Shu-yi. Earthquake energy input model based on harmonic wavelet[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S2): 62-67.
Citation: XIAO Mei-ling, YE Liao-, LI Shu-yi. Earthquake energy input model based on harmonic wavelet[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S2): 62-67.

谐波小波下的地震能量输入模型

Earthquake energy input model based on harmonic wavelet

  • 摘要: 地震动时频局部特性很强,在不同的时刻及不同的频率段,其能量差别很大.本文根据谐波小波的时频特性,通过地震动的多尺度小波变换,可以得到的不同频段的时变能量表达式,最后通过分析一实际的时频非平稳明显的强震记录,得到结果表明:低频的地震能量较小,且分布在整个时段内,能量衰减也不明显;中频的初始时段的地震能量较大,其衰减较快;高频的地震能量最大,且分布在初始的时段内,能量衰减很快.结果为能量法进行结构设计的提供了基础.

     

    Abstract: For Seismic have its own time-frequency localization characteristics,in other words,the energy is variable with time and frequencies.In this paper,according to the time-frequency characteristics of harmonic wavelet,the different frequency bands of the time varying energy expression was given by the ground motion of multi-scale wavelet transform,finally,a practical strong motion record which owned its time-frequency non-stationary characteristics has been analyzed,the results show that: not only seismic energy which distributes with the whole period of time at low frequency is smaller,but also energy attenuation is not obvious; seismic energy of intermediate frequency at the initial time is bigger with its rapid attenuation; seismic energy of high frequency is the biggest with the initial period,which decreases rapidly with time.The energy method in the paper provides a theory basis for structural design.

     

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