深部开采上覆岩层破坏与异常瓦斯排放的微震响应特征

IF 5.3 2区 工程技术 Q1 MECHANICS
Erhui Zhang , Hongqing Zhu , Jinhai Liu , Linsheng Gao
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引用次数: 0

摘要

异常瓦斯排放是威胁矿山安全的重要动力危害。在深部开采过程中,上覆岩层的严重破裂大大增加了此类事件发生的可能性。利用高精度微震监测系统,研究了山西1200工作面开采过程中微震事件的时空分布和演化规律。该方法能够分析与深部开采过程中上覆地层破裂和异常气体排放相关的动态微震响应特征。微震事件在煤层上方0 ~ 20 m范围内高密度分布,在煤层上方20 ~ 80 m范围内低密度分布,在底板以下0 ~ 10 m范围内低密度分布。36%的微地震事件的次数在10到30之间,而24%的微地震事件的次数在30到60之间。72.3%的微震事件能量集中在103 ~ 104 j,崩落带(煤层上方0 ~ 16 m)微震事件横向分布;该带微震反应强烈,事件集中度高。裂缝带(裂缝上方16 ~ 39 m)微震事件较少,但分布相对集中。在弯曲沉降带内,微震响应弱,事件分散,频率低。利用顶板截获的微地震事件的最小累积能量阈值(9.8 × 105 J),确定上覆岩层裂缝的超前影响距离为5 ~ 20 m。异常气体排放模式与微地震事件震级、位置和分布密度相关。本研究旨在揭示上覆地层压裂与异常气体排放之间的内在关系。研究结果有望提供有效的预警系统和控制策略,促进矿山安全的实时监控,减轻灾难性事故,保护矿工的生命安全。研究结果为研究高瓦斯开采工作面煤岩破坏-瓦斯涌出关系、加强瓦斯防治措施和矿井整体安全提供了新的视角。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Microseismic response characteristics of overlying strata failure and unusual gas emissions in deep mining
Unusual gas emissions constitute a critical dynamic hazard threatening mining safety. Severe fracturing within the overlying strata during deep mining substantially increases the likelihood of such incidents. A high-precision microseismic monitoring system was employed to investigate the spatiotemporal distribution and evolution patterns of microseismic events during mining operations at the 1200 mining face in Shanxi, China. This approach enabled analysis of the dynamic microseismic response characteristics linked to overlying strata fracturing and unusual gas emissions during deep mining. Microseismic events exhibited high-density distribution within 0–20 m above the coal seam, low-density distribution between 20–80 m above the seam, and within 0–10 m below the floor. Thirty-six percent of microseismic events had counts between 10 and 30, whereas 24 % ranged from 30 to 60 events. Additionally, 72.3 % of microseismic events had energies concentrated within 103 to 104 J. The caving zone (0–16 m above the coal seam) displayed microseismic events distributed laterally across its extent; this zone exhibited an intense microseismic response and high event concentration. The fracture zone (16–39 m above the seam) contained fewer microseismic events, though distribution was relatively concentrated. Within the bending subsidence zone, the microseismic response was weak, with events being scattered and infrequent. Utilizing the minimum cumulative energy threshold (9.8 × 105 J) of microseismic events intercepted by the roof, we determined the advance influence distance of overlying strata fractures to be 5–20 m. Patterns of unusual gas emissions showed correlation with microseismic event magnitude, location, and distribution density across the area. This study was designed to reveal the intrinsic relationship between overlying strata fracturing and unusual gas emissions. The findings are expected to provide effective early warning systems and control strategies, facilitate real-time monitoring of mine safety, mitigate catastrophic accidents, and safeguard miners’ lives. These results offer a novel perspective on coal-rock failure–gas emission relationships at high-gas mining faces, enhancing gas prevention measures and overall mine safety.
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来源期刊
CiteScore
8.70
自引率
13.00%
发文量
606
审稿时长
74 days
期刊介绍: EFM covers a broad range of topics in fracture mechanics to be of interest and use to both researchers and practitioners. Contributions are welcome which address the fracture behavior of conventional engineering material systems as well as newly emerging material systems. Contributions on developments in the areas of mechanics and materials science strongly related to fracture mechanics are also welcome. Papers on fatigue are welcome if they treat the fatigue process using the methods of fracture mechanics.
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