随掘地震含断层模型三维数值模拟与波场分析

    Three-dimensional numerical simulation and wave field analysis of seismic-while-digging model with faults

    • 摘要: 随掘地震勘探技术是煤巷掘进智能化发展中的重要勘探手段之一,与传统的勘探技术相比,具有安全、高效、探掘同步等优点,能够提高掘进生产效率和保障掘进生产安全。针对随掘震源的特点,研究掘进机截割头受力方式,对其进行受力分析,将随掘震源真实数据加载到三维断层模型进行正演模拟,得出径向、横向、竖向分量相关结论(径向、横向、竖向分量简称为xyz分量);在随掘震源受力分析基础上,对每个受力点加载雷克子波点震源并模拟单炮震源,验证随掘记录互相关处理有效性。结果表明:随掘x分量互相关处理过后效果较差,y分量和z分量互相关处理过后,分离的单炮记录波形完整;在x分量上,折射横波和Rayleigh槽波能量较强,随掘记录中2组波相互干涉,导致互相关处理效果不佳;在y分量上, Love槽波能量较强,随掘记录经过互相关处理后能够分离出Love槽波;在z分量上,随掘记录通过互相关处理后能分离出Rayleigh槽波;yz分量断层落差小于煤厚时,落差越大,随掘记录互相关处理过后反射波越明显,落差超过煤厚时,反射波变化不大;断层夹角在45°~90°范围内,随掘记录y分量互相关处理后反射波能量变化不大,z分量则是断层夹角越小,随掘记录互相关处理后反射波能量越小。

       

      Abstract: Seismic-while-digging exploration technology is one of the important exploration means in the intelligent development of coal roadway. Compared with the traditional exploration technology, it has the advantages of safety, high efficiency and synchronous exploration, which can improve the production efficiency and ensure the safety of mining production. According to the characteristics of the seismic-while-digging source, the stress mode of the cutting head of the boring machine is studied, and the force analysis is carried out. The real data of the seismic source is loaded into the three-dimensional fault model for forward simulation, and the correlation conclusions of radial, transverse and vertical components are obtained( the radial, transverse and vertical components are collectively referred to as x, y and z components); on the basis of the force analysis of source of the seismic-while-digging, a Ricker wavelet point source is loaded on each point of force, and a single shot source is simulated to verify the effectiveness of cross-correlation processing of the following excavation seismic records. The results show that the effect of cross-correlation processing of x-component is poor, and the waveform of single shot recording is complete after cross-correlation processing of y-component and z-component; the energy of refracted shear wave and Rayleigh channel wave is strong in the x component, and these two groups of waves interfere with each other in the excavated seismic records, which leads to the poor effect of cross-correlation pulse processing; in y-component, the energy of Love channel wave is strong, and the energy of other wave groups is weak. After cross-correlation pulsation processing, the Love channel wave can be separated from the digging record; on the z component, Rayleigh channel wave can be separated after cross-correlation processing with the seismic-while-digging records; when the fault drop of y and z components is less than the coal thickness, the larger the drop is, the more obvious the reflected wave is after the cross-correlation processing with seismic-while-digging records. The fault angle ranges from 45° to 90°, and the reflected wave energy changes little with the cross-correlation of y component of excavation records. The z component is that the smaller the fault angle, the smaller the reflected wave energy after cross-correlation with seismic-while-digging records.

       

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