Jiashun Liu, Yang Wang, Jianping Zuo, Zuoqi Wu, Yunjiang Sun, Zhiyong Zheng
School of Civil Engineering, Liaoning Technical University, Fuxin, 123000, Liaoning, China.
School of Mechanics and Civil Engineering, China University of Mining and Technology-Beijing, Beijing, 100083, China.
Sci Rep. 2024 Jul 6;14(1):15614. doi: 10.1038/s41598-024-66622-9.
The extraction of underground coal resources induces the fracture and movement of overlying strata, leading to geological hazards such as surface deformation, cracks, and even subsidence. Utilizing the analogous hyperbola model of overlying strata movement, we conducted a mechanical analysis to examine the asymmetric fracture mechanism resulting from coal seam mining in thick loose strata. An asymmetric analogous hyperbola model was established by introducing distinct virtual half-axis lengths (b). The thickness impact of thick loose layers (H) and bedrock layer (h) on the asymmetric movement of overlying rock during mining was also discussed. Similarity model tests were conducted to research the migration characteristics and surface subsidence patterns of overburdened rock and thick loose layers at different mining stages and validate the hypothesis of asymmetric overburdened rock migration. Additionally, the discrete element numerical model for thick and loose layers mining was established by using UDEC and discussed the asymmetric analogous hyperbola behaviour of overburden movement and surface subsidence. The comparison results show that the established asymmetric hyperbolic model can effectively predict the movement law of overlying strata and surface subsidence characteristics. Therefore, the proposed model can provide valuable theoretical support for predicting the movement patterns of overburden under thick loose layers and mitigating surface subsidence disasters.
地下煤炭资源的开采会引发上覆岩层的断裂和移动,导致诸如地表变形、裂缝甚至塌陷等地质灾害。利用上覆岩层移动的类似双曲线模型,我们进行了力学分析,以研究厚松散岩层中煤层开采导致的非对称断裂机制。通过引入不同的虚拟半轴长度(b)建立了非对称类似双曲线模型。还讨论了厚松散层(H)和基岩层(h)的厚度对开采过程中上覆岩层非对称移动的影响。进行了相似模型试验,以研究不同开采阶段覆岩和厚松散层的移动特征及地表下沉模式,并验证覆岩非对称移动的假设。此外,利用UDEC建立了厚松散层开采的离散元数值模型,并讨论了覆岩移动和地表下沉的非对称类似双曲线行为。比较结果表明,所建立的非对称双曲线模型能够有效预测上覆岩层的移动规律和地表下沉特征。因此,所提出的模型可为预测厚松散层下覆岩的移动模式和减轻地表下沉灾害提供有价值的理论支持。