煤岩破裂微震信号的小波特征能谱系数分析法
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摘要
煤岩破裂微震信号是一种时变非平稳信号,具有不可预知性和突发瞬态性,为了提取能够表征微震源信息的有效特征,基于小波理论,选取了适合微震信号的小波基函数,并根据采样定理及Mallat算法确定了小波分解最大尺度,提出了用小波特征能谱系数分析煤岩破裂微震信号波形的状态分析方法。实验结果表明,微震信号与噪声信号有明显不同的小波特征能谱系数分布特征,而且可利用提取的能谱系数作为特征向量表示信号特征。这对于抑制微震信号的不稳定性和同频段的干扰信号,以及后续的特征编码非常有利,为实现煤岩破裂微震信号实时的模式识别打下了重要基础。
Coal rupture microseismic signal is characterized by time-varying,non-stationary,unpredictable and transient properties.To extract effective features representing microseismic source information,the wavelet basis function suitable for microseismic signal is selected based on wavelet theory.Besides,the maximum wavelet decomposition dimension is determined according to sampling theorem and Mallat algorithm.Furthermore,energy spectrum coefficients of wavelet features are proposed to analyze coal rupture microseismic signal.Experimental results indicate that microseismic signal and noise have different characteristics,which can be effectively demonstrated by energy spectrum coefficient of wavelet features.Moreover,fewer parameters can be used to analyze and characterize the signal in simple and direct-viewing ways.The above research is beneficial to suppress the interference signals in same frequency and the instability of microseismic signal,as well as is advantageous to subsequent feature encoding.It also lays an important foundation for real-time pattern recognition of coal rupture microseismic signal.
引文
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