EMD分解区域的数据研究

Data discussion of the EMD method in the practice

  • 摘要: 本文介绍了一种新的非线性、非平稳信号的处理方法—HHT方法,并运用此方法对地震波进行了理论分析,详细研究了其中的EMD方法及其实现过程;通过大量的数据分析,总结了这一方法的优越性,指出其具有良好筛分及不可良好筛分的适用数值范围,并总结了其中蕴涵的规律。当组合简谐波的频率固定,A2/A1很小,超过某一限值时;或者A2/A1很大,超过某一限值时,数据值不能用EMD方法进行筛分。当组合简谐波的幅值比A2/A1固定不变,而频率变化时,当f2/f1很小时,如超过某一限值;或者f2很接近f1,f2/f1超过某一限值时,数据y值不能用EMD方法进行筛分。

     

    Abstract: In this paper, a new nonlinear nonsteady method for signal treatment is introduced in detail, which is valid and predominant. It is used to analysed the seismic wave.The EMD method and its process are presented through a great amount of data study. A range of good-shift of data is given from a lot of data analysis and the rule is given. When the frequency of combined sine wave is constant, the value of A2/A1 is very small, and it is over a limit; or the value of A2/A1 is large, and it is over a limit, EMD method is not applicable. When amplitude ratio of sine wave A2/A1 is constant, but the frequency varies, if the value of f2/f1 is very small, and it is over a limit; or the value of f2 is very close to f1, and the ratio f2/f1 is over a limit, the value of y is not able to be shifted by EMD method.

     

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