沙梁煤矿随掘地震数值模拟技术与应用

Numerical simulation technology and application of seismic-while-excavation in Shaliang Coal Mine

  • 摘要: 【目的】为实现掘进过程中掘进工作面前方地质异常的实时识别,针对传统超前探测方法存在的施工周期长、分辨率低等问题,开展随掘地震的震源机理与传播规律研究。【方法】建立掘进机截割头受力模型,分析轴向推力与剪切作用下P波、SV波和SH波的产生机理;构建含巷道、煤层和断层破碎带的三维地质–地球物理模型,采用弹性波三维有限差分法开展数值模拟,研究不同波型的传播特征与能量分布。【结果】模拟结果表明,P波能量集中、传播速度快,是主要波型;S波在低速层和断层处易发生反射和波型转换。巷道与煤层内存在明显的管波、槽波,断层破碎带对波场能量具有屏蔽作用。随掘地震信号频带集中于50~450 Hz,主频约200 Hz。【结论】揭示了掘进机震源的形成机制与辐射规律,明确了随掘地震信号在复杂介质中的传播特征。研究结果可为随掘地震信号的识别、有效反射信息提取及地质构造成像提供了理论依据。

     

    Abstract: To achieve real-time identification of geological anomalies ahead of the excavation face, this study investigates the seismic-while-excavating (SWE) signal mechanism and propagation law, addressing the limitations of conventional pre-exploration methods such as long operation cycles and low resolution. A mechanical model of the roadheader cutting head was established to analyze the generation of P-, SV-, and SH-waves under axial thrust and shear forces. A 3-D geological–geophysical model containing the roadway, coal seam, and fault fracture zone was constructed. The 3-D elastic wave finite-difference method was used to simulate wave propagation and energy distribution. Simulations show that P-waves dominate with concentrated energy and fast velocity, while S-waves exhibit reflection and mode conversion at low-velocity layers and faults. Guided and channel waves appear in the roadway and coal seam, and the dominant frequency band of SWE signals is 50 ~ 450 Hz with a peak near 200 Hz. The study reveals the generation mechanism and radiation characteristics of the SWE source and clarifies its propagation behavior in complex media, providing theoretical support for SWE signal recognition and geological imaging.

     

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