Formation Mechanism and Accurate Identification of Spontaneous Combustion Hazard Zones in Gob-Side Entry Driving Goafs Under Small Coal Pillar Damage

IF 1.3 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-10-13 DOI:10.1155/gfl/1018583
Jiace Guo, Gang Wang, Weizhi Zhao
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Abstract

Mining-induced damage to a narrow retained coal pillar can establish preferential air leakage pathways between an active goaf and an adjacent previously mined goaf, thereby altering oxygen transport and the spatial distribution of residual coal oxidation regions. Taking the 31119 gob-side entry driving panel of Nalinhe No. 2 Coal Mine as the engineering background, this study combined buried tube monitoring, gob-side directional borehole sampling, and CFD porous medium simulations to investigate the effects of retained coal pillar damage on airflow and oxygen migration. A coal pillar damage–air leakage–oxygen transport model was established, and steady-state simulations were conducted for different prescribed coal pillar damage conditions. Field monitoring showed that the oxygen-defined oxidation zone in the 31119 goaf extended from 37.5 to 83.9 m on the intake side and from 16.2 to 49.0 m on the return side, whereas the corresponding simulated ranges were 35–84 m and 16–51 m, respectively. More importantly, in the adjacent 31120 goaf, the monitored oxidation zone range along the gob-side strike direction was approximately −45 to 14 m, compared with a simulated range of −48 to 13 m. With increasing retained coal pillar damage, fracture connectivity and equivalent permeability increased, promoting deeper oxygen penetration and progressive expansion of the oxidation zone in the adjacent goaf, whereas the three-zone distribution in the 31119 active goaf changed only slightly. These results indicate that damage to the retained coal pillar primarily controls the reactivation of oxygen-accessible oxidation conditions in the adjacent goaf. The proposed approach provides a basis for identifying potential spontaneous combustion–prone regions and for targeted leakage sealing, gas monitoring, and fire prevention measures in gob-side entry driving panels.

小煤柱破坏下采空区侧进巷自燃危险区形成机理及准确识别
采动对窄留煤柱的破坏可以在活动采空区和相邻已开采采空区之间建立优先的漏风通道,从而改变氧气输送和残余煤氧化区的空间分布。本研究以纳林河二矿31119采空区掘进盘为工程背景,结合地埋管监测、采空区定向钻孔取样和CFD多孔介质模拟,研究留煤柱损伤对气流和氧气运移的影响。建立了煤柱损伤-漏风-氧输运模型,并对不同规定煤柱损伤条件进行了稳态模拟。现场监测结果表明,31119采空区吸入侧的氧限定氧化带范围为37.5 ~ 83.9 m,返回侧的氧限定氧化带范围为16.2 ~ 49.0 m,模拟范围分别为35 ~ 84 m和16 ~ 51 m。更重要的是,在邻近的31120采空区,沿采空区走向方向的氧化带监测范围约为- 45 ~ 14 m,而模拟范围为- 48 ~ 13 m。随着留煤柱破坏程度的增加,裂缝连通性和等效渗透率增加,促进了邻近采空区氧气穿透深度加深,氧化带逐渐扩大,而31119活动采空区三带分布变化不大。这些结果表明,对残余煤柱的破坏主要控制邻近采空区氧可及氧化条件的再激活。所提出的方法为识别潜在的自燃易发区域以及在采空区侧巷道驱动盘中采取有针对性的泄漏密封、气体监测和防火措施提供了基础。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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