W. Ciezkowski et Ta. Przylibski, RADON IN WATERS FROM HEALTH RESORTS OF THE SUDETY MOUNTAINS (SW POLAND), Applied radiation and isotopes, 48(6), 1997, pp. 855-856
Citations number
9
Categorie Soggetti
Nuclear Sciences & Tecnology","Radiology,Nuclear Medicine & Medical Imaging","Chemistry Inorganic & Nuclear
This paper discusses the geological background related to the presence
of selected radon waters in the Sudety Mountains. Special attention i
s paid to radon waters whose chemical composition is formed within met
amorphic rocks (mainly gneisses). The physical, chemical, and isotopic
characteristics of the waters of Ladek Zdroj, Czerniawa Zdroj and Swi
eradow Zdroj are presented. The rocks at these locations are briefly c
haracterized by their U, Th, and Ra contents. It was found that the ba
sic role in enrichment of these waters with radon is played by the 100
m deep near-surface zone. This is related to the increased emanation
coefficient in this zone as a consequence of weathering processes. It
is also shown that the residence time of water in the rocks is not imp
ortant for radon genesis. (C) 1997 Elsevier Science Ltd.