Methods for Increasing the Accuracy of Geoacoustic Emission Signal Models Based on Sparse Approximation

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

Abstract

The acoustic emission phenomenon arises due to local changes of dynamic structure of solid body. Main sources of emission are micro and macro cracks, friction and shifts. Active and passive acoustic emission methods are widely used to study the strength of materials, the landscape stability and various stages of seismic process. Geoacoustic emission is an acoustic emission of the sound range and it describes the interaction of micro and macro dislocations. Anomalies of geoacoustic signals may be earthquake precursors and they are of great interest to researchers. A typical geoacoustic signal consists of sequence of specific shape short pulses. Authors propose an additive model of geoacoustic signal. According to the model the signal decomposes into a sum of components described by the modulated Berlage and Gauss functions. The use of the matching pursuit method was offered to determine model coefficients. Unfortunately, this method has cubic computational complexity depending on number of functions on which the signal is decomposed. This article is devoted to ways to improve accuracy of the model offered by authors. Various numerical schemes allowed to increase the adaptive property of matching pursuit method with respect to geoacoustic emission signals are considered and compared.
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基于稀疏逼近提高地声发射信号模型精度的方法
声发射现象是由于固体动力结构的局部变化而产生的。发射源主要有微观和宏观裂纹、摩擦和位移。主动声发射和被动声发射方法被广泛用于研究材料强度、景观稳定性和地震过程的各个阶段。地声发射是一种声音范围内的声发射,它描述了微观和宏观位错的相互作用。地声信号异常可能是地震的前兆,引起了研究人员的极大兴趣。一个典型的地声信号由一系列特定形状的短脉冲组成。提出了一种地声信号的加性模型。根据该模型,信号分解为由调制的伯拉奇函数和高斯函数描述的分量和。提出了采用匹配追踪法确定模型系数的方法。不幸的是,这种方法具有三次计算复杂度,这取决于分解信号的函数的数量。本文致力于探讨作者提出的提高模型准确性的方法。考虑并比较了提高匹配追踪方法对地声发射信号自适应性能的各种数值格式。
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