Unique documentation,analysis of origin and development of an undrained depression in a subsidence basin caused by underground coal mining (Kozinec,Czech Republic) |
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Authors: | Marian Marschalko Işık Yilmaz David Lamich Marián Drusa Darja Kubečková Tomáš Peňaz Tereza Burkotová Vladimír Slivka Martin Bednárik David Krčmář Miloš Duraj Alena Sochorková |
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Affiliation: | 1. Faculty of Mining and Geology, Institute of Geological Engineering, V?B-Technical University of Ostrava, 17. listopadu 15, 708 33, Ostrava, Czech Republic 2. Department of Geological Engineering, Faculty of Engineering, Cumhuriyet University, 58140, Sivas, Turkey 3. Department of Geotechnics, Faculty of Civil Engineering, University of Zilina, Zilina, Slovak Republic 4. Department of Building Construction, Faculty of Civil Engineering, V?B-Technical University of Ostrava, L. Podé?tě 1875, 708 33, Ostrava, Czech Republic 5. Department of Engineering Geology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, 842 15, Bratislava, Slovak Republic 6. Department of Hydrogeology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, 842 15, Bratislava, Slovak Republic
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Abstract: | This article aims to explain and demonstrate the origin and development of a subsidence basin caused by coal mining as well as to point out important aspects of this phenomenon in engineering geology. Engineering geology needs to deal with a number of issues related to the origin and development of subsidence basins in areas affected by deep coal mining. An interesting case study from the Upper-Silesian Basin in the northeast of the Czech Republic near the Polish border is presented in this paper. There is a clear time chronological succession in the ground surface changes manifested by a ground subsidence gradation, both in their absolute values as well as in their spatial distribution. The phenomenon is documented by aerial photo time series, which optimally depict the origin and development of the subsidence. In the study area, there are changes in the landscape elements and it is essential to be considered in future land use plans. The marginal conditions of the Quaternary geological structure and hydrogeological conditions are responsible for an unconfined aquifer which manifests there as a water body in an undrained depression in the course of the ground subsidence. |
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