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Analysis of the spatial variability of the concentrations of Na+ and K+ ions in the groundwater sourced in Southern Poland

Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Differences in the spatial variability of Na+ and K+ ion concentrations in the groundwater sourced in Southern Poland have been analysed. The study was based on selected hydrogeological environments differing in the lithology and geometry of aquifer rock voids. The hydrogeochemical background for Na+ and K+ ions was determined for various hydrogeological environments as well. The hydroge-ochemical background ranges obtained do not deviate significantly from the background ranges for groundwater observed in other areas of Poland. The analyses conducted indicate the presence of anomalous concentrations of Na+ and K+ ions in all hydrogeological environments often accompanied with significantly elevated concentrations of Cl- and SO42– ions. Owing to the fact that the data analysed exhibit a distribution deviating considerably from a normal one, non-parametric methods of statistical inference were used. The results obtained indicate statistically significant differences between the variabilities of Na+ and K+ ion concentrations in various hydrogeological environments. The factors responsible for such differences are lithological variability and different groundwater circulation systems.
Rocznik
Strony
5--18
Opis fizyczny
Bibliogr. 10 poz., tab., rys.
Twórcy
autor
  • University of Agriculture in Cracow, Department of Sanitary Engineering and Water Management, Environmental Engineering and Land Surveying, ul. Mickiewicza 24/28, 30-059 Cracow, Poland
autor
  • University of Agriculture in Cracow, Department of Sanitary Engineering and Water Management, Environmental Engineering and Land Surveying, ul. Mickiewicza 24/28, 30-059 Cracow, Poland
Bibliografia
  • [1] SHALLENBERGER R.S., Taste Chemistry, Blackie Academic and Professional, an imprint of Chapman and Hall, Glasgow 1993.
  • [2] HEM J.D., Study and interpretation of the chemical characteristic of natural water, U.S. Geol. Surv. Wat. Supp. Pap. 2254, 1989.
  • [3] BACK W., HANSHAW B.B., Chemical geohydrology, Adv. Hydrosci., 1965, 2, 49.
  • [4] REIMANN C., FILZMOSER P., Normal and lognormal data distribution in geochemistry: death of a myth. Consequences for the statistical treatment of geochemical and environmental data, Environ. Geol., 2000, 39 (9), 1001.
  • [5] MATSCHULLAT J., OTTENSTEIN R., REIMANN C., Geochemical background – can we calculate it?, Environ. Geol., 2000, 39 (9), 990.
  • [6] MACIOSZCZYK A., The hydrochemical background of groundwaters sourced in Poland. The groundwater protection in Poland: the present state and direction of research. A Central Program of the Basic Research Papers (CPBP), SGGW-AR, Warsaw 1991 (in Polish).
  • [7] PŁOCHNIEWSKI Z., BIDZIŃSKA W., The occurrence of potassium ions in the groundwaters in Poland, Geol. Quart., 1970, 14, 2 (in Polish).
  • [8] SPRUILL T.B., SHOWERS W.J., HOWE S.S., Application of classification-tree methods to identify nitrate sources in groundwater, J. Environ. Qual., 2002, 31, 1538.
  • [9] SZYMAŃSKA-PULIKOWSKA A., Sodium and potassium in the groundwater in areas near the Maślice municipal refuse dump in Wrocław, J. Elem., 2008, 13 (4), 665.
  • [10] KANGJOO K., SEONG-TAEK Y., Buffering of sodium concentration by cation exchange in the ground-water system of a sandy aquifer, Geochem. J., 2005, 39, 273.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-3abee895-6a7f-49ba-8eed-7eeeb2c1d457
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