Abstract:
:Activity concentrations of dissolved (222)Rn and (226)Ra were measured in several underground aquifers, which are candidates for repositories or for the study of analogue natural escapes of CO2. The concentration of both radionuclides in water was determined using liquid scintillation counting. The values obtained for the (222)Rn concentrations varied from 0 to 150 Bq l(-1), while the levels of (226)Ra were in general very low. This indicates that (222)Rn is coming from the decay of the undissolved (226)Ra existing in the rocks and deep layers of the aquifers, being later transported by diffusion in water.
journal_name
Radiat Prot Dosimetryjournal_title
Radiation protection dosimetryauthors
Martín Sánchez A,Ruano Sánchez AB,de la Torre Pérez J,Jurado Vargas Mdoi
10.1093/rpd/ncv232subject
Has Abstractpub_date
2015-11-01 00:00:00pages
143-6issue
1-3eissn
0144-8420issn
1742-3406pii
ncv232journal_volume
167pub_type
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