地下矿山微震响应空间探测概率特征与数据补偿方法

Characteristics of spatial detection capability for seismic response and data compensation method in underground mines

  • 摘要: 深部复杂地质环境高强度开采造成煤岩动力灾害频发,但地下矿山微震监测台网在数据探测完整性仍存在不足,极大增加了灾害预警的误报漏报风险。因此,将地震学中基于概率的完整性震级评价方法(PMC)应用于某井工煤矿,分析了各微震台站的震动波拾波能力,探究了台网对采场微震响应探测概率的空间分布特征,并提出了基于探测概率的微震活动补偿方法。结果表明:相比于地震学中经典的最小完整性震级评价,PMC具有不依赖古登堡−里克特关系、计算简单、评价精度高的特点,更适用于地下矿山台网布置受限、震源来源复杂、震动波高噪音、强衰减的微震监测环境。微震台站对震动波的拾波能力受其所在区域采动煤岩体环境影响,对不同距离、不同能级微震事件的拾波概率具有显著差异:震源与台站距离越短、震源能级越高,台站对震动波到时标定的概率则越大。微震台网对微震事件的探测能力与震源能级直接相关,探测概率受台站布置影响在采场空间呈现高度非均匀分布特征。针对微震台网探测数据不完整的问题,提出了基于探测概率的微震活动补偿方法,还原了超前工作面煤体微震能级与频次的空间分布特征,其高能释放区域所在超前巷道位置与动力显现频发区域基本吻合,验证了采场微震数据补偿结果的有效性。研究成果可为地下矿山高质量微震监测与高效灾害防治提供理论与数据基础。

     

    Abstract: Coal and rock dynamic hazards frequently occur in deep and complex geological environments undergoing intensive mining activities. Nevertheless, the seismic monitoring in underground mines still has deficiencies in data integrity, which significantly increases the erroneous or missed hazard pre-warnings. Therefore, this study introduces the Probability-based Magnitude of Completeness (PMC) method in an underground coal mine. PMC method assesses the seismic wave picking capabilities of geophones, explores the spatial characteristics of seismic event detection probability within the seismic network, and proposes a detection probability-based seismic compensation method. The results show that: PMC offers advantages over the classic Minimum Magnitude of Completeness approach in seismology, including independence from the Gutenberg-Richter law, simpler computation, and higher evaluation accuracy. These attributes make PMC particularly suitable for seismic monitoring in underground mines constrained by network layout, complex seismic sources, significant signal noise, and attenuation. The picking capabilities of geophones for seismic waves are influenced by local coal and rock environments, leading to substantial variations in picking probabilities for seismic events of different distances and energy levels: The shorter the distance between the seismic source and the geophone, and the higher the source energy level, the greater the probability that the geophone can identify the arrival time of the seismic wave. The detection capability of the seismic network is directly linked to the energy levels of seismic events, resulting in a highly heterogeneous spatial distribution within the mining area due to geophone layout. By applying the detection probability-based seismic compensation method, the study reconstructs the spatial distribution characteristics of seismic energy levels and frequencies ahead of the longwall face, revealing a close correspondence between areas of high-energy release and locations prone to dynamic failures, which validates the seismic compensation results. The research outcomes contribute theoretical and data foundations for enhancing the quality of seismic monitoring and improving hazard early-warning in underground mines.

     

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