PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Chemical diversity of groundwater in the Carboniferous-Permian aquifer in the Unisław Śląski - Sokołowsko area (the Sudetes, Poland); a geochemical modelling approach

Autorzy
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Groundwater in the Carboniferous.Permian sedimentary aquifer in the vicinity of Unisław Śląski - Sokołowsko (Intra-Sudetic Basin, the Sudetes, SW Poland) manifests spatial chemical diversity. The water chemistry varies from fresh calcium-magnesium-bicarbonate groundwater at the recharge area to calciumsodium-sulphate mineral water downwards the basin. Geochemical mass balance modelling confirms that the main chemistry features of the sulphate mineral water are controlled by dedolomitization and calcium common-ion effects. Congruent dissolution of gypsum promotes incongruent dissolution of dolomite with calcite precipitation. Cation exchange between Ca[^2+] (and Mg[^2+]) solutes and Na[^+] (and K[^+]) also takes place. The sulphate mineral water shows elevated concentrations of numerous trace elements. Iron, zinc and manganese originate from dissolution of carbonates (dolomite and/or siderite) and/or sulphides. The hydrogeological system studied should be considered as a series of individual flow systems. The results of preliminary geochemical modelling corroborate the role of mixing in the formation of the spatial pattern of the aqueous chemistry in the system. The main factor that controls groundwater chemistry is the mixing of two components: modern (tritium-bearing) fresh water and older (pre-bomb Holocene) sulphate mineral water.
Rocznik
Strony
97--112
Opis fizyczny
Bibliogr. 30 poz.,Rys., tab., wykr.,
Twórcy
Bibliografia
  • AWDANKIEWICZ, M. 1999. Volcanism in a late Variscan intramontagne trough: Carboniferous and Permian volcanic centres of the Intra-Sudetic Basin, SW Poland. Geologia Sudetica, 32, 13-47.
  • BISCHOFF, J.L., JULIA, R., SHANKS III, W.C. & ROSENBAUER, R.J. 1994. Karstification without carbonic acid: Bedrock dissolution by gypsum-driven dedolomitization. Geology, 22, 995-998.
  • BOSSOWSKI, A. (Ed.) 1996. Grzędy IG1. Profiles of deep boreholes, 83, 57 pp. Polish Geological Institute. [In Polish]
  • BOSSOWSKI, A. (Ed.) 1997. Unisław Śląski IG1. Profiles of deep boreholes, 88, 64 pp. Polish Geological Institute. [In Polish]
  • BOSSOWSKI A., CYMERMAN Z., GROCHOLSKI A. & IHNATOWICZ A. 1994. Geological Map of the Sudetes, 1:25 000, sheet Jedlina Zdrój. Wydawnictwa Geologiczne; Warszawa.
  • BOSSOWSKI, A. & IHNATOWICZ, A. 1994. Paleogeography of the uppermost Carboniferous and lowermost Permian deposits in the Intra-Sudetic Depression. Geological Quarterly, 38 (4), 709-726.
  • BUSBY, J.F., PLUMMER, L.N., LEE, R.W. & HANSHAW, B.B. 1991. Geochemical evolution of water in the Madison aquifer in parts of Montana, South Dakota, and Wyoming. U.S. Geological Survey, Professional Paper, 1273-F, pp. 1-89.
  • CLARK, I.D. & FRITZ, P. 1997. Environmental isotopes in hydrogeology. CRC Press, Boca Raton; Florida, USA.
  • DĄBROWSKI, S. & SZAFRANEK, M. 1982. Hydrogeological documentation of groundwater intake at Upper Crateceous, Triassic, and Permian deposits. Unpublished. Przedsiębiorstwo Geologiczne; Wrocław. [In Polish]
  • DOBRZYŃSKI, D. 1997. Aluminium hydrogeochemistry in areas affected by acid rains in the Intra-Sudetic Depression, SW Poland. pp. 1-149. Unpublished Ph.D. thesis, Institute of Hydrogeology and Engineering Geology, Warsaw University. [In Polish]
  • DOBRZYŃSKI, D. 2005. Conceptual geochemical models of groundwater chemistry against aquifer mineralogy (Stefanian-Autunian sedimentary rocks, the Intra-Sudetic Basin, SW Poland). Slovak Geological Magazine, 11 (4)
  • DOBRZYŃSKI, D. & MITRĘGA, J. 2002. Report on the KBN project 9 T12B 044 18: Origin of sulphate mineral waters in the Sokołowsko area (the Sudetes) on isotopic research and geochemical modelling. Unpublished. Institute of Hydrogeology and Engineering Geology, Warsaw University. [In Polish]
  • DZIEDZIC, K. & TEISSEYRE, A.K. 1990. The Hercynian molasse and younger deposits in the Intra-Sudetic Depression, SW Poland. Neues Jahrbuch für Geologie und Pallontologie, Abhandlungen, 179 (2/3), 285-305.
  • EDMUNDS, W.M., BATH, A.H., & MILES, D.L. 1982. Hydrochemical evolution of the East Midlands Triassic sandstone aquifer, England. Geochimica et Cosmochimica Acta, 46, 2069-2081.
  • GROCHOLSKI, A. 1971. Geological Map of the Sudetes, 1:25 000, sheet Mieroszów. Wydawnictwa Geologiczne; Warsaw.
  • HANOR, J.S. 2000. Barite-celestine geochemistry and environments of formation. In: C.N. ALPERS, J.L. JAMBOR & D.K. NORDSTROM (Eds), Sulfate minerals: crystallography, geochemistry, and environmental significance. Reviews in Mineralogy and Geochemistry, 40. Mineralogical Society of America; Washigton, DC, USA.
  • HANSHAW, B.B. & BACK, W. 1979. Major geochemical processes in the evolution of carbonate-aquifer systems. Journal of Hydrology, 43, 287-312.
  • ICHIKUNI, M. & MUSHA, S. 1978. Partition of strontium between gypsum and solution. Chemical Geology, 21, 359-363.
  • MAŁOSZEWSKI, P. & ZUBER, A. 1996. Lumped parameter models for the interpretation of environmental tracer data. In: Manual on Mathematical Models in Isotope Hydrology. IAEA-TECDOC-910. IAEA, Vienna, pp. 9-58.
  • MASTALERZ, K. & NEHYBA, S. 1997. Comparison of Rothliegende lacustrine depositional sequences from Intrasudetic, North-Sudetic and Boskovice basins (Central Europe). Geologia Sudetica, 30, 21-57. [In Polish, English summary]
  • NORDSTROM, D.K. 1977. Thermochemical redox equilibria of ZoBell’s solution. Geochimica et Cosmochimica Acta, 41, 1835-1841.
  • PARKHURST, D.L. & APPELO, C.A.J. 1999. User’s guide to PHREEQC (version 2) – A computer model for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. U.S. Geological Survey, WRI Report, 99-4259.
  • PLUMMER, L.N. & BACK, W. 1980. The mass balance approach: Application to interpreting the chemical evolution of hydrologic systems. American Journal of Science, 280, 130-142.
  • PLUMMER, L.N., BUSBY, J.F., LEE, R.W., & HANSHAW, B.B. 1990. Geochemical modeling of the Madison aquifer in parts of Montana, Wyoming, and South Dakota. Water Resources Research, 26, 1981-2014.
  • SACKS, L.A. & TIHANSKY, A.B. 1996. Geochemical and isotopic composition of ground water, with emphasis on sources of sulfate, in the Upper Floridan Aquifer and Intermediate Aquifer System in Southwest Florida. U.S. Geological Survey, WRI Report, 96-4146.
  • SZAFRANEK, M., RODZIEWICZ, R. & NIŻYŃSKI, S. 1986. Hydrogeological documentation of groundwater intake at Permian deposits with report on investigations at the Sokołowsko – Unisław Śląski area. Unpublished. Wałbrzyskie Przedsiębiorstwo Wodociągów i Kanalizacji, Wałbrzych, pp. 1-29. [In Polish]
  • VEIZER, J. 1983. Trace elements and isotopes in sedimentary carbonates. In: R.J. REEDER (Ed.), Carbonates: mineralogy and chemistry. Reviews in Mineralogy, 11. Mineralogical Society of America; Washigton, DC, USA.
  • WICKS, C.M. & HERMAN, J.S. 1994. The effect of a confining unit on the geochemical evolution of ground water in the Upper Floridian aquifer system. Journal of Hydrology, 153, 139-155.
  • WIŚNIEWSKA, M. 2003. Quality of groundwaters abstracted at intake in Unisław Śląski (the Sudetes) against hydrogeological conditions. Unpublished. M. Sc. thesis. Institute of Hydrogeology and Engineering Geology, Warsaw University, 184 pp. [In Polish]
  • WÓJCICKA, T. & TARKOWSKI, S. 1968. Groundwater intake in Permian and Carboniferous deposits at Unisław Śląski area. Unpublished.Wałbrzyskie Przedsiębiorstwo Wodociągów i Kanalizacji, Wałbrzych. 83 pp. [In Polish]
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-1772-6491
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.