利用稀疏模型评价脉冲信号的内部结构

A. Kim, O. Lukovenkova, Y. Marapulets, A. Tristanov
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引用次数: 1

摘要

复杂地球物理系统产生的脉冲性质信号需要特殊的方法来研究其内部结构。这些信号的特点是脉冲持续时间短,结构多变。传统的谱法和时频法的应用难度很大。提出了一种基于稀疏逼近的脉冲信号模型和一种识别模型的算法。该算法是一种改进的匹配追踪算法,使用基于物理的函数(字典)系统。建模结果的研究在于估计模型分量的时频特性。本文给出了该模型在堪察加半岛地震活跃区地声发射信号上的应用实例。所提出的模型和模型研究方法可用于大范围的脉冲性质信号。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Using a sparse model to evaluate the internal structure of impulse signals
Impulse nature signals generated by complex geophysical systems require special methods to study their internal structure. These signals are characterized by a short duration of impulses and the variability of their structure. The use of classical spectral and time-frequency methods raises great difficulty. The authors propose a model of an impulse signal based on a sparse approximation and an algorithm for identifying a model. The algorithm is a modified matching pursuit algorithm using a physically based system of functions (dictionary). The study of modeling results consists in estimating the time-frequency characteristics of the model components. The paper gives an example of the model application on geoacoustic emission signals of a seismically active region (Kamchatka peninsula). The proposed model and approaches to the model investigation can be used for a wide range of impulse nature signals.
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