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Investigation of the Radon Levels in Groundwater and Thermal Springs of Pamukkale Region

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dc.creator Kulali, F.
dc.creator Akkurt, I.
dc.creator Ozgur, N.
dc.date 2016-06-30T21:00:00Z
dc.date.accessioned 2020-10-06T09:39:23Z
dc.date.available 2020-10-06T09:39:23Z
dc.identifier 304b56db-4b2d-4e82-891f-e32512612d10
dc.identifier 10.12693/aphyspola.130.496
dc.identifier https://avesis.sdu.edu.tr/publication/details/304b56db-4b2d-4e82-891f-e32512612d10/oai
dc.identifier.uri http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/56694
dc.description Radon, which is the largest source of natural ionizing radiation, reaches surface as gas form or solvated in the ground water. Emanation of radon can has a profile which is disposed to increase or decrease depending on the effects of meteorological events or crust movements. Pamukkale, which was involved previously in the world heritage list of UNESCO, and the surrounding area have many groundwater and thermal springs that carry dissolved radon to surface. The aim of this study was to investigate the variations of radon in the water samples of the region.
dc.language eng
dc.rights info:eu-repo/semantics/closedAccess
dc.title Investigation of the Radon Levels in Groundwater and Thermal Springs of Pamukkale Region
dc.type info:eu-repo/semantics/article


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