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Seismic Signal Processing by Wavelet Based Multifractal Analysis

机译:基于小波多重分形分析的地震信号处理

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摘要

Fractal geometry and wavelets are a new and promising approach to analyze and characterize non-stationary signals such as seismic signals, ECG, stock prices, etc. Short-term Fourier transform analysis imposes the assumption that signals are stationary over small temporal segments. Such an assumption is inappropriate for seismic signals because conditions inside mines undergo constant change. Because they do not impose this assumption, wavelet-based techniques are proving useful for processing seismic data. In this paper, we propose a wavelet-based method to analyze seismic signals, which is superior to many conventional methods used in the industry today. The fractal dimension and other measures are calculated by using wavelets, in which time is irrelevant. Another measure, Multifractal Spectrum is computed with the help of a scaling exponent. Using this strategy, our method distinguishes between a seismic signal and a noisy signal or truly chaotic signal by fractal dimension. Further our result shows that the larger fractal dimension indicates a rock burst in mines. The approach introduced here should be useful in the analysis of other non-stationary biological signals.
机译:分形几何和小波是分析和表征非平稳信号(如地震信号,ECG,股票价格等)的一种新的有前途的方法。短期傅立叶变换分析提出了这样的假设:信号在较小的时间段内是平稳的。这样的假设不适用于地震信号,因为矿井内部的条件会不断变化。由于基于小波的技术没有强加此假设,因此对处理地震数据很有用。在本文中,我们提出了一种基于小波的方法来分析地震信号,它优于当今行业中使用的许多常规方法。分形维数和其他度量是通过使用小波来计算的,其中时间是无关紧要的。另一种测量方法是在定标指数的帮助下计算多重分形谱。使用这种策略,我们的方法可以通过分形维数区分地震信号和噪声信号或真正的混沌信号。此外,我们的结果表明,较大的分形维数表明矿山中发生了岩石破裂。此处介绍的方法应可用于分析其他非平稳生物信号。

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