2016
DOI: 10.1016/j.jenvrad.2015.10.019
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Radon in spring waters in the south of Catalonia

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Cited by 78 publications
(36 citation statements)
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“…The high variability of the Rn-222 activity concentrations can be explained by their different origins and the lithology of the aquifer host rocks (LLERENA et al, 2013). Larger values are found in groundwater, based on the geology of the studied site (FONOLLOSA et al, 2016). If we compare the results of this work with those from survey data of many other countries and different sources, such as wells, non-bottled mineral water, springs, and underground, surface, and drinking water, the Rn-222 activity concentrations found in the Matinha stream present no anomalous readings.…”
Section: Discussionmentioning
confidence: 92%
“…The high variability of the Rn-222 activity concentrations can be explained by their different origins and the lithology of the aquifer host rocks (LLERENA et al, 2013). Larger values are found in groundwater, based on the geology of the studied site (FONOLLOSA et al, 2016). If we compare the results of this work with those from survey data of many other countries and different sources, such as wells, non-bottled mineral water, springs, and underground, surface, and drinking water, the Rn-222 activity concentrations found in the Matinha stream present no anomalous readings.…”
Section: Discussionmentioning
confidence: 92%
“…Nevinsky, Tsvetkova and Nevinskaya () reported radon levels of well waters from Western Caucasus (Russia) as range from 0.4 to 86.7 Bq/L. In Catalonia spring waters, radon concentration levels were found between 1.4 and 104.9 Bq/L (Fonollosa, Penalver, Borrull, & Aguilar, ). Generally, radon concentration levels in well water of Bodrum Peninsula are higher than the levels given by literature.…”
Section: Resultsmentioning
confidence: 99%
“…Radon ( 222 Rn) is an endogenous natural radioactive noble gas, and is a product of the decay chain of Uranium ( 238 U). 222 Rn (half-life of 3.82 days) is the most commonly occurring radon isotope in nature, produced by α-decay from Radium ( 226 Ra), it is soluble in water, and its behavior and concentration in groundwater is strongly influenced by the geological nature of substratum, and by the occurrence of Rn parent elements [1,2]. Moreover, the concentration of Rn in soil depends on chemical, physical, and geological factors, such as geochemical mobility of Rn precursors, grain size, distribution of sediments, porosity, permeability, and seasonal variations, including temperature and atmospheric pressure [3][4][5].…”
Section: Introductionmentioning
confidence: 99%