Mechanism of hydraulic fracturing for controlling strong mining-induced earthquakes induced by coal mining

IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL International Journal of Rock Mechanics and Mining Sciences Pub Date : 2024-08-02 DOI:10.1016/j.ijrmms.2024.105840
Junpeng Zou , Quan Zhang , Yujing Jiang , Yu-Yong Jiao , Sitao Zhu , Guohua Zhang
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Abstract

The complex geological conditions of coal mine, especially the geological characteristics of coal-bearing strata, determine that mining is one of the most hazardous occupations worldwide. Strong mining-induced earthquakes (E ≥ 105 J) frequently occur in coal mines, where the high-strength thick and hard roofs are developed above coal seams. It seriously threatens the safety of underground miners and ground residents, as well as the productivity and effectiveness of mining activities. The fracture characteristics of the overlying strata and the distribution of mining-induced earthquake characteristics before and after field experiment of hydraulic fracturing is analyzed and revealed using the methods of field monitoring and numerical analysis, and reveals the effect of hydraulic fracturing technology in preventing and controlling strong mining-induced earthquakes, for the frequent occurrence of mining-induced earthquakes in Dongtan coal mine. Combined with the results of microseismic monitoring after hydraulic fracturing, as mining advances, the frequency of small-energy microseismic events is dominant, and the percentage of strong mining-induced earthquakes was reduced by 51.3 %. Numerical calculations show that the existence of hydraulic fractures provided the necessary paths for the expansion of the fracture network in the overlying strata. This results in rock masses near the hydraulic fracture slipping along the fracture under the action of mining stresses. The implementation of hydraulic fracturing can effectively weaken and fracture the integrity of thick and hard rock strata to reduce or eliminate the occurrence of hazardous mining-induced earthquakes with large energy.

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水力压裂法控制煤矿开采引发的强矿震的机理
煤矿复杂的地质条件,特别是含煤地层的地质特征,决定了采矿是世界上最危险的职业之一。在煤层之上发育有高强度厚硬顶板的煤矿中,经常发生矿井诱发强震(E ≥ 10 J)。它严重威胁井下矿工和地面居民的安全,以及采矿活动的生产率和效益。针对东滩煤矿矿井诱发地震频发的现状,采用现场监测和数值分析的方法,分析揭示了水力压裂现场实验前后上覆地层的断裂特征和矿井诱发地震的分布特征,揭示了水力压裂技术在防治矿井强诱发地震中的作用。结合水力压裂后的微震监测结果,随着开采的推进,小能量微震事件的发生频率占主导地位,开采诱发强震的比例降低了 51.3%。数值计算表明,水力断裂的存在为上覆地层断裂网络的扩展提供了必要的路径。这导致水力断裂附近的岩块在采矿应力的作用下沿着断裂滑动。实施水力压裂法可以有效地削弱厚硬岩层的完整性并使其断裂,从而减少或消除由采矿引发的大能量危险地震的发生。
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来源期刊
CiteScore
14.00
自引率
5.60%
发文量
196
审稿时长
18 weeks
期刊介绍: The International Journal of Rock Mechanics and Mining Sciences focuses on original research, new developments, site measurements, and case studies within the fields of rock mechanics and rock engineering. Serving as an international platform, it showcases high-quality papers addressing rock mechanics and the application of its principles and techniques in mining and civil engineering projects situated on or within rock masses. These projects encompass a wide range, including slopes, open-pit mines, quarries, shafts, tunnels, caverns, underground mines, metro systems, dams, hydro-electric stations, geothermal energy, petroleum engineering, and radioactive waste disposal. The journal welcomes submissions on various topics, with particular interest in theoretical advancements, analytical and numerical methods, rock testing, site investigation, and case studies.
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