dc.contributor.author | Marschalko, Marian | |
dc.contributor.author | Yilmaz, Işık | |
dc.contributor.author | Lamich, David | |
dc.contributor.author | Heviánková, Silvie | |
dc.contributor.author | Kyncl, Miroslav | |
dc.contributor.author | Dirner, Vojtech | |
dc.contributor.author | Andráš, Peter | |
dc.date.accessioned | 2014-09-12T13:35:44Z | |
dc.date.available | 2014-09-12T13:35:44Z | |
dc.date.issued | 2014 | |
dc.identifier.citation | Carpathian Journal of Earth and Environmental Sciences. 2014, vol. 9, issue 2, p. 187-197. | cs |
dc.identifier.issn | 1842-4090 | |
dc.identifier.issn | 1844-489X | |
dc.identifier.uri | http://hdl.handle.net/10084/105789 | |
dc.description | Článek je přístupný po bezplatné registraci na webu vydavatele. | |
dc.description.abstract | The study area has been greatly affected by mining activities and other anthropogenic activities since it falls within the so-called Ostrava-Karvina Coal District. Morphological variations in time by temporal variations in subsidence basins by underground mining activities in the Moravia-Silesian Region in the north-east of the Czech Republic was investigated in this article. Subsidence was observed in the four time intervals of 1983-1990, 1983-1995, 1983-2000, and 1983-2005. Relationships between estimated subsidence during time period of 2003-2010 and municipality land use plans were identified by overlay analyses. There is a clear impact on the land use plans caused by varying thoroughness of the urban planners. As the result of the observations in these periods, underground mining activities considerably had a negative impact on the current built-up area. Despite this, the built-up area erected on the most affected subsidence interval of “500-1200 cm” during the last time period of 1983-2005 is only 1%. According to the Land Use Plan Categorization, development planned for the most impacted subsidence interval of “500-1200 cm” is in the U_V_0 category of Unspecified Production Zone and also in the U_DL_2 zone of mining interest. This development area covers 1.54% of the overall planned development. Analyses related with slope deformation in the study area imply that there are three active areal shaped slide areas, one so-called other areal shaped slide area (55.6 ha) and three active very small slide areas. A possible risk is posed by the active areal shaped slide areas which have an overall surface area of 12.05 ha. As the main results of this study; it was found that the subsidence distribution implies trends which confirm that the area unaffected by subsidence impacts decreased over time due to the expansion of the subsidence basin, and thus a re-distribution of impacts occurred in the study area. These impacts were caused by black coal mining in the Karvina Mine, the CSA Plant and in allotments of Karvina-Doly I, Doubrava and Darkov. As another result; the analyses showed that impacts of subsidence in the area had not properly considered in the planning of future development. | cs |
dc.language.iso | en | cs |
dc.publisher | North University of Baia Mare, Faculty of Mineral Resources and Environment | cs |
dc.relation.ispartofseries | Carpathian Journal of Earth and Environmental Sciences | cs |
dc.relation.uri | http://www.ubm.ro/sites/CJEES/viewTopic.php?topicId=433 | cs |
dc.rights | (c) 2007 - 2014 - North University of Baia Mare, Faculty of Mineral Resources and Environment | cs |
dc.title | Morphological variations in subsidence basin and importance for land use planning: undermined Karvina region (Czech Republic) | cs |
dc.type | article | cs |
dc.type.status | Peer-reviewed | cs |
dc.description.source | Web of Science | cs |
dc.description.volume | 9 | cs |
dc.description.issue | 2 | cs |
dc.description.lastpage | 197 | cs |
dc.description.firstpage | 187 | cs |
dc.identifier.wos | 000334903200019 | |