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dc.contributor.authorMarschalko, Marian
dc.contributor.authorYilmaz, Isik
dc.contributor.authorKristkova, Veronika
dc.contributor.authorFuka, Matej
dc.contributor.authorBednarik, Martin
dc.contributor.authorKubecka, Karel
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T10:04:11Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T10:04:11Z
dc.date.issued2012
dc.identifier.issn0013-7952
dc.identifier.urihttps://dx.doi.org/10.1016/j.enggeo.2011.10.010
dc.identifier.urihttps://hdl.handle.net/20.500.12418/9261
dc.descriptionWOS: 000299913500013en_US
dc.description.abstractThis study deals with the determination of the actual limit angles in the long-term formed subsidence basin in the Czech part of the Upper Silesian Basin (the remaining part lays in Poland). Here there was the most extensive underground exploitation of black coal in the north-east of the Czech Republic. A limit angle is absolutely decisive in the determination of deep mining influences in relation to the current and future utilisation of this territory. The two CSM and Paskov mine localities on the edge of the subsidence basin were selected for this study, since they could not have been affected by mining in neighbouring mines. On the grounds of the long-term levelling monitoring of points on the surface which started prior to mining, the horizontal distance between the mined out area and the undisturbed ground surface was identified. The impact of limit angle on the surface was calculated by means of the horizontal distance and the established mining depth. Such identified actual limit angles reached the values of 36 degrees at the CSM Mine and 25 degrees for the Paskov Mine. The calculated values are significantly lower when compared with the currently applied empirical values of 57 degrees for the CSM Mine and 56 degrees for the Paskov Mine. This means that the extent of the undermining effects is unambiguously wider by 611 m at the CSM Mine and by 883 m at the Paskov Mine. This study thus establishes the existence of a significantly vaster area influenced by coal deep mining than previously expected. The identified facts lead to the conclusion that regular revisions and follow-up updates of the empirically determined parameters are recommended. (C) 2011 Elsevier B.V. All rights reserved.en_US
dc.description.sponsorshipEuropean Union; ERDF [1CE014P4]en_US
dc.description.sponsorshipAuthors thank the European Union (CENTRAL EUROPE Programme co-financed by the ERDF) for the support for the project (COBRAMAN - 1CE014P4) which is the base of this article. Authors are also deeply grateful to the Anonymous reviewers for their very constructive critics and suggestions which led to the improvement of the paper.en_US
dc.language.isoengen_US
dc.publisherELSEVIER SCIENCE BVen_US
dc.relation.isversionof10.1016/j.enggeo.2011.10.010en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectLimit angleen_US
dc.subjectUndermined territoryen_US
dc.subjectBlack coal deep miningen_US
dc.subjectCzech part of the Upper Silesian Basinen_US
dc.titleDetermination of actual limit angles to the surface and their comparison with the empirical values in the Upper Silesian Basin (Czech Republic)en_US
dc.typearticleen_US
dc.relation.journalENGINEERING GEOLOGYen_US
dc.contributor.department[Yilmaz, Isik] Cumhuriyet Univ, Fac Engn, Dept Geol Engn, TR-58140 Sivas, Turkey -- [Marschalko, Marian -- Kristkova, Veronika -- Fuka, Matej] Tech Univ Ostrava, Fac Min & Geol, Inst Geol Engn, Ostrava 70833, Czech Republic -- [Bednarik, Martin] Comenius Univ, Fac Nat Sci, Dept Engn Geol, Bratislava 84215, Slovakia -- [Kubecka, Karel] Tech Univ Ostrava, Fac Civil Engn, Dept Bldg Struct, Ostrava 70833, Czech Republicen_US
dc.contributor.authorIDKubecka, Karel -- 0000-0003-1562-0678; Kubecka, Karel -- 0000-0003-1562-0678;en_US
dc.identifier.volume124en_US
dc.identifier.endpage138en_US
dc.identifier.startpage130en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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