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Seismic activity and flooding of hard coal mines in the Ostrava-Karvina Coalfield

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The termination of mining activities often results in post-mining problems and risks. One of these issues is the flooding of mines. Long-term mining in the Ostrava and Petrvald sub-basins in the Upper Silesian Coal Basin finished in 1994. Tens of coal seams were mined here, and the depth of mining reached more than 1000 m below the surface. Flooding of the Ostrava sub-basin started in 1994. The Ostrava and Petrvald sub-basins were flooded from one half only to prevent water from flooding into the Karvina sub-basin, where mining continued. The continual pumping of water has been carried out ever since. Only low-energy seismic events (up to 103 J) were recorded during the periods of flooding and water pumping. Only one high-energy seismic event was recorded here (108 J, magnitude of 3.5, 12 December 2017). This study presents the natural and mining conditions regarding the process of mine flooding; and the induced seismicity registered during the flooding of mines and the preservation of water at the stated level. Analysis of the flooding of mines in connection to the registered seismicity is presented. Probable reasons for the low seismic activity during the flooding of mines are also discussed.
Rocznik
Strony
249--260
Opis fizyczny
Bibliogr. 18 poz.
Twórcy
autor
  • Institute of Geonics of the Czech Academy of Sciences, Czech Republic
  • Institute of Geonics of the Czech Academy of Sciences, Czech Republic
  • Institute of Geonics of the Czech Academy of Sciences, Czech Republic
  • Green Gas DPB, Inc., Czech Republic
  • DIAMO, s.p., ODRA, o.z., Czech Republic
  • Institute of Geonics of the Czech Academy of Sciences, Czech Republic
Bibliografia
  • [1] Caro Cuenca M, Hooper AJ, Hanssen RF. Surface deformation induced by water influx in the abandoned coal mines in Limburg, The Netherlands observed by satellite radar interferometry. J Appl Geophys 2013;88.
  • [2] Samsonov S, d'Oreye N, Smets B. Ground deformation associated with post-mining activity at the French-German border revealed by novel InSAR time series method. Int J Appl Earth Obs Geoinf 2013;23(1).
  • [3] Kessler T, Mugova E, Jasnowski-Peters H, Rinder T, Stemke M, Wolkersdorfer C, et al. Groundwater in former German coal mining areas - a scientific perspective on mine floodings. Grundwasser 2020;25(4).
  • [4] Devleeschouwer X, Declercq P-Y, Flamion B, Brixko J, Timmermans A, Vanneste J. Uplift revealed by radar interferometry around Liège (Belgium): a relation with rising mining groundwater. In: Proceedings of the post-mining symposium; 2008.
  • [5] Matrullo E, Contrucci I, Dominique P, Bernard P, Aochi H, Bennani M. Induced micro-seismicity by flooding of the abandoned Gardanne coal basin (Provence, France): analysis and interpretation. In: HAL Id: ineris-01862559 [Internet]. rench-Japanese symposium an earthquakes & triggered hazards; 2015. p. 79-81. Available from: https://hal-ineris.archives-ouvertes.fr/ineris-01862559/document.
  • [6] Rische M, Fischer KD, Allgaier F, Friederich W. Induced micro seismicity due to raising mine water level in former coal mines in the eastern Ruhr area (Germany). EGU General Assembly 2021 [Internet]. EGU21-13040; 2021. Available from: https://meetingorganizer.copernicus.org/EGU21/EGU21-13040.html.
  • [7] Vervoort A. The time duration of the effects of total extraction mining methods on surface movement. Energies 2020 Aug 8;13(16):4107. Available from: https://www.mdpi.com/1996-1073/13/16/4107.
  • [8] Kandarachevová J, Sedláčková L, Hýlová L, Jirásek J, Sivek M. Lateral development of coalification in the Czech part of the Upper Silesian Coal Basin and its connection with gas deposits. Int J Coal Geol 2009;78(3).
  • [9] Dopita M. Geology of the Czech part of the upper silesian basin. Prague: Ministry of the Environment of the Czech Republic; 1997. p. 278.
  • [10] Grygar R, Vavro M. Evolution of Lugosilesian orocline (north-eastern periphery of the Bohemian Massif): kinematics of Variscan deformation. J Czech Geol Soc 1995;40(1-2).
  • [11] Dvorský J. Hydrogeological summary of the solution to the problem of flooding the Ostrava sub-basin. Paskov, OKD, DPB; 1996.
  • [12] Malucha P, Šmolka M, Hotárek V, Říčná M. Solution of hydrogeological conditions after the closure of active mines OKD, a.s. - case study. Paskov, Green Gas DPB; 2015.
  • [13] Malucha P. Influence of the hydrosphere by deep mining of a coal deposit during and after the period of active mining activity with a focus on OKC. PhD thesis. VSB - Technical University of Ostrava; 2013.
  • [14] Younger PL, Banwart SA, Hedin RS. Mine water hydrology, pollution, remediation. Mine Wastes; 2007.
  • [15] Ptacek J, Konicek P, Holecko J, Przeczek A, Waclawik P, Pavelek Z, et al. Rockbursts in ostrava-karvina coalfield. Ostrava: Institute of Geonics of the Czech Academy of Sciences; 2017. p. 1-147.
  • [16] Konicek P, Schreiber J, Nazarova L. Volumetric changes in focal areas of seismic events correspond to destress blasting. Journal of Mining Science and Technology 2019;29(4):541-7. https://doi.org/10.1016/j.ijmst.2019.06.004.
  • [17] Folprecht J. The concept of pumping mine water in the Ostrava sub-basin. Ostrava: Archív Dolu Odra; 1995.
  • [18] Hrubcová P, Šílený J, Zedník J. Earthquake in the hlučín region. Vesmír 97 [Internet]. 2018. Available from: https://vesmir.cz/cz/casopis/archiv-casopisu/2018/cislo-3/zemetreseni-hlucinsku.html.
Uwagi
PL
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-072400d9-8f73-4612-b0fd-ac1dd46309f5
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