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基于3D双流网络的地下岩层破裂微震震源定位

Location of underground microseismic source based on 3D two-stream network

  • 摘要: 地下微震震源中心探测技术主要用于地下岩层破裂,矿井爆破振动监测,工程爆破定向拆除等定位问题。针对目前微震采集传感器采集时钟误差以及采集数据高频信息缺失的问题,提出了基于3D双流网络的方法对地下岩层破裂进行分布式微震震源定位。该方法通过空间扫描的方式使低维的振动波信息高维化,把地震波形数据从时间域转化为能量域,建立震源中心与高维能量分布的对应关系;然后通过3D-CNN网络提取能量域特征,convLSTM网络逐步优化震源中心区域,以得到精准的震源中心定位。结果表明,基于3D双流网络的地下岩层破裂微震震源定位明显优于传统的基于走时类震源定位方法,该方法在高信噪比数据中,具有更强的数据拟合能力和抗干扰能力。并且通过小场地静态爆炸试验结果表明,该定位方法在近场微震震源定位中优于传统方法。

     

    Abstract: The detection technology of the microseismic source center of underground damage is mainly used for the location of the underground damage, positioning of explosion point of artillery shells in weapon testing ground. Aiming at the problem that clock error of microseismic acquisition sensor and the lack of high frequency information of acquisition data, this paper proposes a distributed microseismic source location for underground damage based on 3D two-stream network. The method uses spatial scanning to make the low-dimensional vibration wave information highly dimensional, transforms the seismic waveform data from the time domain into the energy domain, and establishes the correspondence between the source center and the high-dimensional energy distribution. Then, the energy domain features are extracted through the 3D-CNN network, and the LSTM network gradually optimizes the focal center region to obtain accurate focal center location. The results show that the source location of underground damage microseismic based on 3D dual-current network is obviously superior to the traditional traveltime-like source location method, and the proposed method has stronger data fitting ability and anti-interference ability in high SNR data. The results of static explosion test in small field show that the proposed method is superior to the traditional method in near field microseismic source location.

     

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