Zhao Bingchao, He Shenglin, Bai Kun, Lu Xiaoxiao, Wang Wei
Xi'an University of Science and Technology, Xi'an, 710054, Shaanxi, China.
Shaanxi Xiaobaodang Mining Company, Yulin, 719000, Shaanxi, China.
Sci Rep. 2024 Mar 25;14(1):7036. doi: 10.1038/s41598-024-57557-2.
In order to understand the development law of water-conducting fractures in overlying strata during the mining process of coal seam, an elastic wave exploration method based on key stratum theory is proposed to predict the height of water-conducting fracture zone. Taking Yushen mining area as the background, the development and evolution of fractures and the three-dimensional distribution characteristics of water-conducting fracture zone are studied by combining well-ground microseismic monitoring, high-density three-dimensional seismic exploration, borehole investigation, FLAC3D numerical simulation and similar physical simulation tests. The results indicate that the trial mining face's fracture-to-coal ratio ranges from 25.86 to 30.76, with the maximum fracture-to-coal ratio near the cutting eye at 30.76 and the minimum in the central portion of the trial mining face at 25.86. The primary characteristics of rock mass fracture distribution in the mined area are the development of fractures predominantly along high-angle and even vertical bedding planes. Within the fracture zone, fractures increase from top to bottom, with high-angle fractures developing in the lower section and high-angle and horizontal fractures developing simultaneously in the upper section. The water-conducting fracture zone undergoes a developmental process from inception to development, reaching its maximum height, and eventually stabilizing as coal seam mining progresses, overlying rock subsides, strata separation, and damage formation. The three-dimensional shape of the water-conducting fracture zone in the roof of the Yushen mining area exhibits a morphological pattern where the height of the fracture zone gradually decreases from the cutting eye towards the goaf. It also transitions from high to low along both sides and from the periphery towards the interior of the working face. In the trend and strike directions, it exhibits saddle-like characteristics. By comparing the monitoring results, the rationality of the elastic wave prospecting method for predicting the height of water-conducting fracture zones based on critical layer theory was verified. This research holds significant reference value for coal mining under similar geological conditions, especially in terms of water preservation during mining operations.
为了掌握煤层开采过程中覆岩导水裂隙的发育规律,提出一种基于关键层理论的弹性波探测方法来预测导水裂隙带高度。以榆神矿区为背景,结合地面微地震监测、高密度三维地震勘探、钻孔探测、FLAC3D数值模拟和相似物理模拟试验,研究了裂隙的发育演化及导水裂隙带的三维分布特征。结果表明,试采工作面的裂隙煤比为25.86~30.76,其中,切割眼附近的裂隙煤比最大,为30.76,试采工作面中部的裂隙煤比最小,为25.86。采空区岩体裂隙分布的主要特征是裂隙主要沿高角度甚至垂直层面发育。在裂隙带内,裂隙自上向下增多,下部发育高角度裂隙,上部高角度裂隙和水平裂隙同时发育。随着煤层开采、上覆岩层沉降、岩层离层和损伤形成,导水裂隙带经历从产生到发展、达到最大高度并最终稳定的发育过程。榆神矿区采场顶板导水裂隙带的三维形态呈现出从切割眼向采空区裂隙带高度逐渐减小的形态特征,且沿工作面两侧从高到低、从周边向内部过渡,在走向和倾向方向上呈现鞍状特征。通过对比监测结果,验证了基于关键层理论的弹性波探测方法预测导水裂隙带高度的合理性。该研究对于类似地质条件下的煤炭开采,尤其是开采过程中的保水工作具有重要的参考价值。