Zhang Yuan, Xu Mengtang, Kong Dezhong, Zuo Yujun, Wu Guiyi, Chen Fi, Zhou Yang
College of Mining, Guizhou University, Guiyang, 550025, China.
Institute of Ming Engineering, Guizhou Institute of Technology, Guiyang, 550003, China.
Sci Rep. 2025 Sep 12;15(1):32517. doi: 10.1038/s41598-025-17438-8.
Coal mines located in southwestern China are generally faced with the complex situation of repeated mining of coal seams in areas with dense karst caves. In view of the problems brought about by overburden fracture transport-induced karst cave instability during repeated mining of karst mines, this paper takes the repeated mining under the karst mines of Qinglong Coal Mine in Guizhou, China, as a background for the study.Using a combination of theoretical analyses, physical experiments and numerical simulations, the influence of karst caves on the transport of the overlying rock layers and the height of the development of water-conducting fissure zones was analysed from the conditions of repeated mining in karst mines.The results show that the existence of repeated mining karst caves accelerates the overburden fracture fissure penetration into the upper coal seam air-mining zone, and at the same time, the analysis of the stress distribution of the caves obtains the judgement basis for the instability of the caves.The DIC digital scatter monitoring system found that the displacement of the overlying rock layer of the cave model at the monitoring point was significantly larger than the displacement of the overlying rock layer of the no-cave model as the working face progressed.The displacement rate of the cavern model is obviously larger under repeated mining, but the cavern plays a key role in controlling the fracture of the overburden rock when the working face advances to the bottom of the cavern, and the cavern is re-stabilised after instability, and it still has a certain supporting effect on the overburden rock above.In order to verify the above analysis using 3DEC numerical simulation to verify it again, it was found that the results are still shifted more at the karst cave, and showed asymmetric subsidence after the cave was perturbed to return to the steady state, which is highly similar to the results of the physical experiments.Therefore, before the coal seam is mined to the vicinity of the karst hole, the roof of the working face can be grouted and reinforced in advance, and the working face can be pushed through the vicinity of the karst hole quickly, and the results of the above research provide certain reference for the safe mining in karst mines.
位于中国西南部的煤矿通常面临着岩溶洞穴密集区域煤层重复开采的复杂情况。针对岩溶矿山重复开采过程中覆岩裂隙运移导致岩溶洞穴失稳所带来的问题,本文以中国贵州青龙煤矿岩溶矿井下重复开采为研究背景。采用理论分析、物理实验和数值模拟相结合的方法,从岩溶矿井重复开采条件出发,分析了岩溶洞穴对上覆岩层运移及导水裂隙带发育高度的影响。结果表明,重复开采岩溶洞穴的存在加速了覆岩裂隙向上煤层采空区的贯通,同时,通过对洞穴应力分布的分析得到了洞穴失稳的判断依据。DIC数字散斑监测系统发现,随着工作面推进,洞穴模型监测点处覆岩位移明显大于无洞穴模型覆岩位移。重复开采条件下洞穴模型位移速率明显增大,但当工作面推进到洞穴底部时洞穴对上覆岩层断裂起到关键控制作用,洞穴失稳后重新稳定,对上方覆岩仍有一定支撑作用。为验证上述分析,利用3DEC数值模拟再次进行验证,发现岩溶洞穴处结果仍有较大偏移,洞穴扰动恢复稳态后呈现非对称沉降,与物理实验结果高度相似。因此,在煤层开采至岩溶洞穴附近前,可提前对工作面顶板进行注浆加固,并快速推过岩溶洞穴附近,上述研究成果为岩溶矿井安全开采提供了一定参考。