Abstract
This study investigates surface subsidence induced by multi-slice longwall mining in the Barapukuria coal basin using FLAC3D numerical simulations. The research quantifies the progressive vertical and horizontal deformations caused by mining over multiple phases, analysing the redistribution of stress in the surrounding strata and the corresponding surface displacements. The results demonstrate a clear nonlinear escalation of vertical subsidence, with maximum displacements reaching 5.14 m after the third mining slice. Horizontal displacement similarly increased, with peak values reaching 1.91 m. The study reveals that the subsidence ratio, defined as vertical displacement relative to mining thickness, increased from 0.08 to 0.86 as mining depth progressed, while the horizontal deformation coefficient decreased. Stress redistribution analysis shows that the peak vertical stress in the overburden reached 35.50 MPa in the third phase, leading to significant compaction and fracturing of the strata, which contributed to the observed subsidence. These findings underscore the cumulative and nonlinear nature of surface deformation, emphasizing the critical need for advanced subsidence prediction models and effective mitigation strategies. In particular, the research offers practical insights into managing surface displacement in areas with dense infrastructure, such as residential, industrial, and transportation networks, as well as in environmentally sensitive regions. The study further highlights the importance of incorporating stress redistribution mechanisms to enhance subsidence management, thereby minimizing the risk of damage to local infrastructure and ensuring sustainable mining practices.