基于小波包技术的爆破地震波特征提取及预报
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摘要
在微风化花岗岩石场地进行了孔径为76mm、孔深为5m的单孔和单段多孔爆破实验研究,获得了该类场地爆破地震波加速度衰减规律,加速度衰减系数为k=3698,α=2.046,并研究了该场地基频特征。运用了小波包技术对爆破地震波测试信号特征量提取,分析了试验所测爆破地震波不同频带下小波包系数的衰减规律。在此基础上建立了基于不同频带小波包系数的爆破地震波预报模型,该模型在爆破地震波波形、峰值及频率预报方面均具有较高的准确度。
The blasting experiments have been carried out in the weakly rotten granite site and the acceleration attenuation of blasting seismic waves in the site were measured, in which the deep hole for blasting was of 76mm in diameter and 5m in depth. The attenuation parameters are k=3698 and α=2046, meanwhile the base frequency characteristics of the site is acquired. With the wavelet packet analysis the blasting seismic wave characteristics are extracted, and the relationship of attenuation of wavelet packets in different frequency bands vs the scaled distance is studied. Based on the wavelet packet attenuation a model to predict the blasting seismic wave characteristics has been proposed in this paper and is of a good accuracy in preticting waveform, amplitude and frequencies of blasting seismic waves.
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