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Tytuł artykułu

Hydrogeological conditions of the Cracow sandstone series in Upper Silesian Coal Basin influenced by mining activity

Treść / Zawartość
Identyfikatory
Warianty tytułu
Konferencja
Groundwater quality sustainability : XXXVIII IAH Congress in Kraków
Języki publikacji
EN
Abstrakty
EN
The Cracow Sandstone Series (CSS), consisting mainly of coarse-grained clastic rocks (>75%), form upper lithostratigraphic series of the coal-bearing Carboniferous formations in the Upper Silesian Coal Basin (USCB). CSS covers the area of 1,500 km2. Thicknes of a formation varies from tens to 1,140 m. Exploitation of coal deposits on industrial scale of production has started since the turn of the XVIII and XIX century. Intensity of water inflows to individual mines ranging from 4.3 to 52.8 m3/min, depends on morphological, geogenic and mining factors. Within the CSS hydrogeological complex typical for sedimentary basins hydrodynamic and hydrogeochemical vertical zoning occurs. Hydrochemical as well as isotope research revealed appearance of varied zones of infiltration, mixed waters and relict brines. Prevailing significance in hydrodynamic conditions forming within the CSS have hydrodynamic barriers: overlying isolating Miocene aquitard and increasing with depth diagenesis of the Carboniferous formation. The mining activity increases the rock permeability and causes the disturbance of the natural hydrodynamic field and hydrogeochemical conditions of the CSS.
Rocznik
Strony
131--137
Opis fizyczny
Bibliogr. 19 poz., rys., wykr.
Twórcy
  • University of Silesia, Faculty of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
  • AGH University of Science and Technology, Faculty of Mining and Geoengineering, al. Mickiewicza 30, 30-059 Kraków, Poland
Bibliografia
  • 1. BUKOWSKI P., 1999 - Carboniferous rock massif water storage capacity and its influence on the process of the coal mines self-flooding. PhD thesis . Arch. Główn. Inst. Górn., Katowice in Polish.
  • 2. JANSON E., 2007 - The impact of the pumped out waters from the liquidated coal mines on the the Przemsza River water quality. PhD thesis . Arch. Wydz. Górn. i Geoinż. AGH, Kraków in Polish.
  • 3. KLECZKOWSKI A.S., WILK Z., 1968 - The influence of the geological structure on the groundwater environment in the south-eastern part of the Upper Silesian Coal Basin. 3, 2/3: 83–202 in Polish.
  • 4. KLECZKOWSKI A.S., WITCZAK S., 1967 - Permeability and porosity of Carboniferous sandstones as related to depth (East Upper Silesian)., 1, 1: 23 –31.
  • 5. KOTAS A., 1985 - Structural evolution of the Upper Silesia Coal Basin (Poland). X Congress Int. Strat. Geol. Carb. Compt. Rend., 3: 459–469. Madrid.
  • 6. PLUTA I., 2005 - Mine waters of the Upper Silesian Coal Basin – origin, pollutants and purification., : 169 in Polish.
  • 7. ROGOŻ M., POSYŁEK E., 2000 - Hydrogeological problems of the Polish coal mines. Wyd. GIG, Katowice in Polish.
  • 8. RÓŻKOWSKI A., 1998 - Origin of mine waters based on isotopic composition (Upper Silesian Coal Basin, Poland). Symp. On mine water and environmental impacts. Proc. IMWA, 1: 53–68. Johannesburg.
  • 9. RÓŻKOWSKI A., 2003 - Upper Silesian Coal Basin. Geological and hydrogeological conditions.: Hydrogeology of the Polish mineral deposits and mining water problems. 1: Upper Silesian Coal Basin: 42–145. Wyd. Nauk.-Dyd. AGH, Kraków in Polish.
  • 10. RÓŻKOWSKI A. (ed.), 2004 - Hydrogeochemical environment of Carboniferous coal-bearing formations of the Upper Silesian Coal Basin. Wyd. U l., Katowice in Polish.
  • 11. RÓŻKOWSKI A., RÓŻKOWSKI K., 2003 - Hydrogeological environment of the Cracow Sandstone Series in the Upper Silesian Coal Basin.: Współczesne problemy hydrogeologii, 11, 1: 177–193. Gdańsk in Polish.
  • 12. RÓŻKOWSKI A., SOŁTYSIAK M., 2005 - Proposition of the hydrochemical regionalization of the mining areas in the Upper Silesian Coal Basin.: Współczesne problemy hydrogeologii, 12: 617–622 . Wyd. Uniw. Mikołaja Kopernika, Toruń in Polish.
  • 13. RÓŻKOWSKI K., 2004 - Groundwater chemistry of the coal-bearing Carboniferous – groundwater complex of the Cracow Sandstone Series.: Hydrogeochemical environment of the Upper Carboniferous: 75–78. Wyd. U l., Katowice in Polish.
  • 14. RÓŻKOWSKI K., WITKOWSKI A., 2004 - Hydrogeological properties of the Upper Carboniferous groundwater complexes.: 30–34.
  • 15. TOTH J., 1995 - Hydraulic continuity in large sedimentary basins., 3, 4: 4–16.
  • 16. WAGNER J., 1998 - Hydrogeological characteristics of the Upper Carboniferous in the main syncline of the Upper Silesian Coal Basin.., 33: 55–96 in Polish .
  • 17. WILK Z., 1965 - Size, depth and water inflow into the coal mines in the eastern part of the Upper Silesian Coal Basin. Wyd. Geol., Warszawa in Polish .
  • 18. WILK Z. (ed.), 2003 - Hydrogeology of the Polish mineral deposits and water mining problems. AGH, Kraków in Polish.
  • 19. WITKOWSKI A., 1982 - Variety of the porosity, drainage capacity and permeability of the Upper Carboniferous rocks in the Pszczyna–Strumień region in Upper Silesian Coal Basin (based on the laboratory studies). PhD thesis . Arch. Kat. Hydrogeol. i Geol. Inż. U l., Katowice in Polish.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-94319edc-cee7-407d-821f-0aee8170052a
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