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Radon in groundwater and dose estimation for inhabitants in Spas of the Sudety Mountain area,Poland
Authors:B. KozŁowska  A. Walencik  J. Dorda  W. Zipper
Affiliation:1. Department of Organic Chemistry, Faculty of Sciences, P.O. Box 187, University of Toliara, 601 Toliara Madagascar;2. Malagasy Institute of Applied Research, Avarabohitra Itaosy lot AVB 77, P. O. BOX 3833, 102 Antananarivo Madagascar;3. Department of Organic Chemistry, Faculty of Sciences, P.O. Box 906 University of Antananarivo, 101Antananarivo, Madagascar;4. Institute of Natural Products Chemistry, National Centre for Scientific Research CNRS 91198, Gif Sur Yvette-Paris, France;5. Department of Biology, Faculty of Science, University of Kinshasa, P.O. BOX 190 Kinshasa XI, Democratic Republic of the Congo;1. Universidad de la República, Facultad de Ciencias—Sección Oceanología, Iguá 4225, Montrevideo 11400, Uruguay;2. Sección Oceanografía, Departamento de Biolog?ía Pesquera, Dirección Nacional de Recursos Acuáticos (DINARA), MGAP, Constituyente 1497, Montevideo, Uruguay;3. Instituto Oceanográfico da Universidade de São Paulo, Praça do Oceanográfico, 191, 05508-120 São Paulo, SP, Brazil;1. Dipartimento di Matematica, Università di Torino, via Carlo Alberto 10, 10123 Torino, Italy;2. University of Vienna, Faculty of Mathematics, Oskar-Morgenstern-Platz 1 A-1090 Wien, Austria;3. Dipartimento di Scienze Matematiche, Politecnico di Torino, corso Duca degli Abruzzi 24, 10129 Torino, Italy;1. Grup de Física de les Radiacions, Departament de Física, Edifici Cc, Universitat Autònoma de Barcelona, 08193 Bellaterra, Barcelona, Spain;2. Unitat de Geodinàmica Externa i d''Hidrogeologia, Departament de Geologia, Edifici Cs, Universitat Autònoma de Barcelona, 08193 Bellaterra, Barcelona, Spain
Abstract:Studies of radon isotope 222Rn activity concentration in underground water in the Sudety region were performed with the use of the liquid scintillation technique. Waters chosen for investigations were collected in 24 health resorts and towns of the Sudety area from 115 springs, wells and intakes. The 222Rn activity concentration varied within the range from 4.2±0.4 to 1703±55 Bq/l. The annual effective doses due to the consumption of 222Rn with water were calculated for 50 sources of underground spring water or tap water used for consumption. The results were within the range from 0.003 to 1.1 mSv/yr, assuming 0.5 l of tap water per day from which radon is not removed or 0.5 l of mineral spring water consumed daily. The contribution to the effective dose from the inhalation of radon during the daily usage of domestic water substantially increases its effective dose.
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