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Environmental tracers in thermal waters of Podhale Basin
Języki publikacji
Abstrakty
Tritium and stable isotope data delta exp.18 O and delta exp.2H) for wells near the recharge area of the thermal system of the Podhale Basin indicate the presence of modern waters recharged at the lowest altitudes of the outcrops of water bearing formations. In turn, delta exp.18O and delta exp.2H values obtained for deep part of the basin may be interpreted as either the result of a high altitude recharge or a cold climate. Helium contents are in general unusually high but can not be interpreted quantitatively at the present stage of the study. The noble gas temperatures (NGT) values obtained from Ne and Ar data disagree with temperatures deduced from the known dependence of air temperature on altitude and altitudes of recharge areas found from the stable isotope data. High concentrations ofHe (ca. 10-4 cm3STP/g), and low NGT deduced from Ne and Ar concentrations suggest the presence of pre-Holocene water in the northeastern part of the basin, which means slow movement of water. Stable isotope and exp.14C data indicate the presence of much younger Holocene waters in the western part of the basin.
Czasopismo
Rocznik
Tom
Strony
685--693
Opis fizyczny
–693, bibliogr. 26 poz., rys., tab., wykr.
Twórcy
autor
autor
autor
autor
autor
autor
- Państwowy Instytut Geologiczny, Oddział Karpacki, ul. Skrzatów 1, 31-560 Kraków, jozef.chowaniec@pgi.gov.pl
Bibliografia
- AESCHBACH-HERTIG W., PETER F., BEYERLE U. & KIPFER R. 1999 - Interpretation of dissolved atmosheric noble gases in natural waters. Water Resour. Res., 35(9): 2779-2792.
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- COOK P.G. & HERCZEG A.I. (eds.) 2000 - Environmental tracers in subsurface hydrology. Kluwer Acad. Publ., Boston.
- KHARAKA Y.K. & CAROTHERS W.W. 1986 - Oxygen and hydrogen isotope geochemistry of deep basin brines. [In:] Fritz P. & Fontes J.C. (eds.) Handbook of environmental isotope geochemistry, vol. 2: The terrestrial environment. Elsevier, Amsterdam: 305-360.
- KON_EK M. & ORLICZ M. 1974-Teplotne pomery. [W:] Kon_ek M. i in. Klima Tatier. Slovenska Akademia Vied. Bratislava.
- LASA J., MOCHALSKI P. & ŁOKAS E. 2002 - Determination of argon in air and water. Analytical Chem. (Warsaw), 47: 839-845.
- LASA J., MOCHALSKI P. & PUSZ J. 2004 - Evaluation of a pulse- discharge helium detector for the determination of neon concentrations by gas chromatography. J. Chrom. A, 1035: 261-264.
- MAŁECKA D. & NOWICKI Z. 2002 - Skład izotopowy wód podziemnych Tatr i Podhala. Biul. Państw. Inst. Geol., 404, Hydrogeologia IV: 67-83.
- MAŁOSZEWSKI P. & ZUBER A. 1996 - Lumped parameter models for the interpretation of environmental tracer data. [W:] Manual on Mathematical Models in Isotope Hydrology. IAEA-TECDOC-910, IAEA, Vienna: 9-58.
- MANNING A.H. & SOLOMON D.K. 2003 - Using noble gases to investigate mountain-front recharge. J. Hydrol., 275(3-4): 194-207.
- MAZOR E. 1972 - Paleotemperatures and other hydrological parameters deduced from noble gases dissolved in groundwaters, Jordan Rift Valley, Israel. Geochim. Cosmochim. Acta, 36: 1321-1336.
- MOCHALSKI P., LASA J. & OELIWKA I. 2006 - Simultaneous determination of Ne, Ar, and N2 in groundwater by gas chromatography. Chem. Anal. (Warsaw), 51: 825.
- PORCELLI D., BALLENTINE C.J. & WIELER R. (eds.) 2002 - Noble gases in geochemistry and cosmochemistry. Reviews in mineralogy and geochemistry, 47. Geochemical Society; Washington, DC.
- PUSZ J., LASA J. & OELIWKA I. 2007 - Metoda chromatografii gazowej w pomiarach stężenia helu w wodach podziemnych. [W:] Szczepański A., Kmiecik E. & Żurek A. (red.) Współczesne problemy hydrogeologii, T. XIII, cz. 2. AGH, Kraków: 303-311.
- SOLOMON D.K., HUNT A. & POREDA J. 1996 - Source of radiogenic helium 4 in shallow aquifers: implications for dating young groundwater. Water Resour. Res., 32: 1805-1813.
- TORGERSEN T. & CLARKE W.B. 1985 - Groundwater dating with helium isotopes, I. An evaluation of sources and the continental flux of crustal 4He in the Great Artesian Basin, Australia. Geochim. Cosmochim. Acta, 49: 1211-1218.
- TORGERSEN T. & IVEY G.N. 1985 - Helium accumulation in groundwater II: A model for the crustal 4He degassing flux. Geochim. Cosmochim. Acta, 49: 2425-2452.
- ZUBER A., MAŁECKI J.J. & DULIŃSKI M. 2008 - Groundwater ages and altitudes of recharge areas in the Polish Tatras Mts. As determined from 3H, Δ18 O and Δ2H data. Geol. Quart., 52 (1): 71-80.
- ZUBER A., OSENBRÜCK K., WEISE S.M., KOWALCZYK A. & RUBIN K. 2005 - Rezultaty badań gazów szlachetnych w GZWP-327, Lubliniec-Myszków. [W:] Kowalczyk A. & Różkowski A. (red.) Hydrogeologia obszarów zurbanizowanych i uprzemysłowionych, t. 2. Pr. Wydz. Nauk o Ziemi UŚ, 37: 189-196.
- ZUBER A., WEISE S.M., MOTYKA J., OSENBRÜCK K. & RÓŻAŃSKI K. 2004 - Age and flow pattern of groundwater in a Jurassic limestone aquifer and related Tertiary sands derived from isotope, noble gas and chemical data. J. Hydrol., 286 (1-4): 87-112.
- ZUBER A., WEISE S.M., OSENBRÜCK K., GRABCZAK J. & CIĘŻKOWSKI W. 1995 - Age and recharge area of thermal waters in Lądek Spa (Sudeten, Poland) deduced from environmental isotope and noble gas data. J. Hydrol., 167: 327-349.
- ZUBER A., WEISE S.M., OSENBRÜCK K. & MATEŃKO T. 1997 - Origin and age of saline waters in Busko Spa (southern Poland) determined by isotope, noble gas, and hydrochemical methods: Evidence of interglacial and pre-Quaternary recharge. Appl. Geochem., 12: 643-660.
- ZUBER A., WEISE S.M., OSENBRÜCK K., PAJNOWSKA H. & GRABCZAK J. 2000 - Age and recharge pattern of the Mazovian basin (Poland) as indicated by environmental tracers. J. Hydrol., 233: 174-188.
- ZUBER A., RÓŻAŃSKI K. & CIĘŻKOWSKI W. (red.) 2007 - Metody znacznikowe w hydrogeologii - poradnik metodyczny. Wyd. Politechniki Wrocławskiej, Wrocław.
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Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS6-0018-0004