College of Energy and Mining Engineering, Shandong University of Science and Technology, Qingdao, 266590, Shandong, China.
State Key Laboratory of Mining Disaster Prevention and Control Co-Founded By Shandong Province and the Ministry of Science and Technology, Shandong University of Science and Technology, Qingdao, 266590, Shandong, China.
Sci Rep. 2023 Mar 14;13(1):4232. doi: 10.1038/s41598-023-31158-x.
Coal mining inevitably results in the movement of overlying strata, with the upward formation of the strata leading to surface subsidence, causing irreversible impact on the buildings, land, and ecological environment. The movement and deformation of the strata are controlled by the bearing structure in the overlying strata, whose failure results in the deformation and breakage of the overlying strata simultaneously. While studies have been conducted on the arch structure in unconsolidated layers (ASUL), its bearing performance has not been addressed. Therefore, this study develops a bearing mechanics model based on the morphological characteristics of the ASUL. The analytical expressions of the axial force, bending moment, and shear force of the cross-sectional area were determined using theoretical derivations. The model analysed the internal forces and showed the influence laws of the overlying load, horizontal pressure coefficient, and rise-to-span ratio of the ASUL. The failure criterion of the bearing was also further determined. The results indicated that with overlying and horizontal loads, the axial force and bending moment are symmetrically distributed, whereas the shear force is asymmetrically distributed. In addition, the axial force gradually increases from the dome to the base of the ASUL. Compared to the axial force and bending moment, the shear force has a lower impact on the stability of the ASUL. Most of the axial force and overlying load is received through the axial compression of the cross-section to maintain stability and play a bearing role on the overlying unconsolidated layers. As the overlying load, horizontal pressure coefficient, and rise-to-span ratio increase, the axial force, bending moment, and shearing force also increase gradually. This effect is more apparent at the dome, spandrel, and base of the ASUL. The stability of the dome and spandrel is key to the overall structural stability. Therefore, the failure criterion for the ASUL was determined based on the compression failure at the dome and spandrel. During the mining process of the working face, the ASUL served as load-bearing control for the overlying unconsolidated layers. Further, increasing width of the working face damages and shifts the base of the ASUL, resulting in compression failure at the dome and spandrel, further inducing dome lift and causing overall failure of the ASUL. Considering the aforementioned factors, a control method that reinforces the surface subsidence of the ASUL by 'one-time, upward, staged, and multiple-ground-drilling' compaction grouting has been proposed. During the mining process of the working face, the arch bead-like structure, combined with the ASUL, serves as the load-bearing control on the overlying strata and ground surface, reducing ASUL deformation in the unconsolidated layers, overlying strata, and ground surface. This process enables the controlling of ground subsidence of coal mining in thick unconsolidated layers.
煤炭开采必然导致覆岩移动,覆岩向上移动导致地表沉降,对建筑物、土地和生态环境造成不可逆转的影响。覆岩的移动和变形受上覆岩层承载结构的控制,其破坏导致上覆岩层同时变形和断裂。虽然已经对松散层中的拱结构(ASUL)进行了研究,但尚未涉及到其承载性能。因此,本研究基于 ASUL 的形态特征,建立了一种承载力学模型。通过理论推导,确定了横截面积的轴向力、弯矩和剪力的解析表达式。该模型分析了内力,并展示了上覆荷载、水平压力系数和 ASUL 升跨比的影响规律。进一步确定了承载的破坏准则。结果表明,在承受上覆和水平荷载时,轴向力和弯矩呈对称分布,而剪力呈非对称分布。此外,轴向力从拱顶逐渐增加到 ASUL 的底部。与轴向力和弯矩相比,剪力对 ASUL 的稳定性影响较小。大部分轴向力和上覆荷载通过横截面对轴向压缩来接收,以保持稳定性,并对上覆松散层发挥承载作用。随着上覆荷载、水平压力系数和升跨比的增加,轴向力、弯矩和剪力也逐渐增加。这种影响在 ASUL 的拱顶、拱肩和底部更为明显。拱顶和拱肩的稳定性是整体结构稳定性的关键。因此,根据拱顶和拱肩的压缩破坏确定了 ASUL 的破坏准则。在工作面开采过程中,ASUL 作为上覆松散层的承载控制。此外,增加工作面的宽度会损坏和移动 ASUL 的底部,导致拱顶和拱肩的压缩破坏,进一步引起拱顶抬升,并导致 ASUL 的整体破坏。考虑到上述因素,提出了一种通过“一次、向上、分阶段、多次地面钻孔”压实注浆加固 ASUL 表面沉降的控制方法。在工作面开采过程中,拱肋状结构与 ASUL 结合,对上覆地层和地表起到承载控制作用,减少了松散层、上覆地层和地表的 ASUL 变形。这一过程实现了对厚松散层中采煤地面沉降的控制。