{"title":"The Combined Effect of Stress Mutation and Displacement Evolution on Overlying Rock Collapse From Physical Experiment and Numerical Simulation Study","authors":"Gang Wang, Daixin Deng, Jing Liu","doi":"10.1155/gfl/7729757","DOIUrl":null,"url":null,"abstract":"<p>This study investigates the complex failure mechanisms of overlying strata deformation induced by longwall mining, with a focus on the 21221 mining face in Qianqiu mine. Combining physical similarity simulation and numerical analysis, the research analyzes the abrupt changes in stress and displacement within the overlying rock mass during mining face advancement. The results show that roof failure occurs periodically, with collapse height and area progressively increasing as the intact bearing zone shifts upward, exerting continuous pressure on the stope. Mining disturbance significantly affects the roof ~40 cm ahead of the working face, where deformation and collapse are governed by gravitational forces and rock lithology. The maximum principal stress concentrates at the goaf edges, and vertical stress mutation accurately indicates impending roof fracture locations. Critically, the failure of hard conglomerate layers triggers a strong regional mutation in the mining-induced stress field. These results provide important insights into the dynamic evolution and instability precursors of overlying strata in deep mining conditions.</p>","PeriodicalId":12512,"journal":{"name":"Geofluids","volume":"2026 1","pages":""},"PeriodicalIF":1.2000,"publicationDate":"2026-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1155/gfl/7729757","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geofluids","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1155/gfl/7729757","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
This study investigates the complex failure mechanisms of overlying strata deformation induced by longwall mining, with a focus on the 21221 mining face in Qianqiu mine. Combining physical similarity simulation and numerical analysis, the research analyzes the abrupt changes in stress and displacement within the overlying rock mass during mining face advancement. The results show that roof failure occurs periodically, with collapse height and area progressively increasing as the intact bearing zone shifts upward, exerting continuous pressure on the stope. Mining disturbance significantly affects the roof ~40 cm ahead of the working face, where deformation and collapse are governed by gravitational forces and rock lithology. The maximum principal stress concentrates at the goaf edges, and vertical stress mutation accurately indicates impending roof fracture locations. Critically, the failure of hard conglomerate layers triggers a strong regional mutation in the mining-induced stress field. These results provide important insights into the dynamic evolution and instability precursors of overlying strata in deep mining conditions.
期刊介绍:
Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines.
Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.