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Proceedings of the International Conference "Radon in Environment" 10-14 May 2009, Zakopane Poland
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Abstrakty
Natural radioactive isotopes were studied in nine different types of brines from four locations in Poland. Investigated brines are exploited from various geological structures composed of the rocks of different chemical and mineral composition as well as different age and depth. All investigated brines are used in balneotherapy (i.e. baths, inhalations, showers). The main goal of this study was to obtain some basic knowledge on the activity range of natural elements such as uranium, radium and radon in different brine types in Poland and their variability depending on their location in certain geological structures. Activities of 234,238U, 226,228Ra and 222Rn isotopes were measured with the use of two nuclear spectrometry techniques: liquid scintillation and alpha spectrometry. The activity concentrations of 222Rn vary from below 1 to 76.1 plus or minus 3.7 Bq/l, for the 226Ra isotope from 0.19 plus or minus 0.01 to 85.5 plus or minus 0.4 Bq/l and for 228Ra from below 0.03 to 2.17 plus or minus 0.09 Bq/l. For uranium isotopes, the concentrations are in the range from below 0.5 to 5.1 plus or minus 0.4 mBq/l for 238U and from 1.6 plus or minus 0.4 to 45.6 plus or minus 2.0 mBq/l for 234U. The obtained results indicate high radium activity concentrations corresponding to high mineralization of waters.
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Tom
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519--522
Opis fizyczny
Bibliogr. 14 poz., rys.
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- Department of Nuclear Physics and Its Applications, Institute of Physics, University of Silesia, 4 Uniwersytecka Str., 40-007 Katowice, Poland, Tel.: +48 32 359 1308, Fax: +48 32 258 8431, beata.kozlowska@us.edu.pl
Bibliografia
- 1. Bateman H (1910) Solution of a system of differential equations occurring in the theory of radioactive transformations. Proc of the Cambridge Philosophical Society. Mathematical and Physical Sciences 15:423–427
- 2. Chau ND, Michalec B (2009) Natural radioactivity in bottled natural, spring, mineral and therapeutic waters in Poland. J Radioanal Nucl Chem 278;1:121–129
- 3. Curie LA (1968) Limits for qualitative detection and quantitative determination. Anal Chem 40;3:586–592
- 4. Kozłowska B (2009) Natural radioactivity of spring waters in spas of southern Poland. Wydawnictwo Uniwersytetu Śląskiego, Katowice (in Polish)
- 5. Kozłowska B, Walencik A, Dorda J, Przylibski TA (2007) Uranium, radium and 40K isotopes in bottled mineral waters from Outer Carpathians, Poland. Radiat Meas 42:1380–1386
- 6. Paczyński B, Sadurski A (2007) Regional hydrogeology of Poland. T. II. Państwowy Instytut Geologiczny, Warszawa (in Polish)
- 7. Pluta I, Zuber A (1995) Origin of brines in the Upper Silesian Coal Basin (Poland) inferred from stable isotope and chemical data. Appl Geochem 10:447–460
- 8. Polish Norm PN-89/ZN-70072 (1989) Radium isotopes determination in water with LSC method. Wydawnictwa Normalizacyjne Alfa, Warszawa (in Polish)
- 9. Przylibski TA (2005) Radon. Specific component of medicinal waters in the Sudety Mountains. Oficyna Wydawnicza Politechniki Wrocławskiej, Wrocław (in Polish)
- 10. Przylibski TA, Dorda J, Kozłowska B (2002) The occurrence of 226Ra and 228Ra in groundwaters of the Polish Sudety Mountains. Nukleonika 47;2:59–64
- 11. Sill CW (1987) Precipitation of actinides as fluorides or hydroxides for high resolution alpha spectrometry. Nucl Chem Waste Mgmt 7:201–215
- 12. Suomela J (1993) Method for determination of radon-222 in water by liquid scintillation counting. SSI Report 93-13, ISO Norm: ISO/TC147/SC3/WG6 Work, Swedish Radiation Protection Institute, Stockholm
- 13. Suomela J (1993) Method for determination of U-isotopes in water. Swedish Radiation Institute, Stockholm
- 14.Walencik A, Kozłowska B, Dorda J, Zipper W (2009) Natural radioactivity in underground water from the Outer Carpathians in Poland with the use of nuclear spectrometry techniques. Appl Radiat Isot, doi:10.1016/j. Apradiso.2009.09.056
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ7-0014-0082