Ground surface uplift during subsidence trough formation due to longwall mining in the shaft protection pillar of the CSM Mine

0560454 - ÚGN 2023 RIV DE eng J - Článek v odborném periodiku
Jiránková, Eva - Lazecký, M.
Ground surface uplift during subsidence trough formation due to longwall mining in the shaft protection pillar of the CSM Mine.
Bulletin of Engineering Geology and the Environment. Roč. 81, č. 9 (2022), č. článku 389. ISSN 1435-9529. E-ISSN 1435-9537
Grant CEP: GA MŠMT LQ1602
GRANT EU: European Commission(XE) 899192 - PostMinQuake
Grant ostatní: Ministerstvo školství, mládeže a tělovýchovy - GA MŠk(CZ) LM2018140
Institucionální podpora: RVO:68145535
Klíčová slova: ground uplift * subsidence trough * longwall mining * radar interferometry
Obor OECD: Mining and mineral processing
Impakt faktor: 4.2, rok: 2022
Způsob publikování: Omezený přístup
https://link.springer.com/article/10.1007/s10064-022-02896-5

Ground surface uplift was detected at the start of longwall mining, a significant part of which is situated in the shaft protection pillar Sever of the CSM Mine in the Czech Republic. The largest uplift was found to be 23 mm, by the levelling method of surface points with height connections to non-mined areas. Due to the length of the connection to the non-influenced area, precise levelling was chosen to observe the vertical displacements and prove the displacement values using a confidence interval with 5% risk. This article aims to clarify the cause of ground surface uplift during longwall mining. Therefore, the height changes of the given area were extracted also from satellite radar interferometry (InSAR). The changes of the observed ground surface were compared with the empirical subsidence. The largest difference between the measured and empirical surface subsidence was 85 mm and occurred in the period before the ground surface uplift. Spatiotemporal evaluation of the data was used to determine the presumed cause of the occurrence of surface uplift in the overburdened strata, due to previous mining activity and the subsequent unburdening of the rock mass.
Trvalý link: https://hdl.handle.net/11104/0333398