2006
DOI: 10.1016/j.jenvrad.2005.10.003
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A combined method for evaluating radon and progeny in waters and its use at Guarani aquifer, São Paulo State, Brazil

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Cited by 15 publications
(6 citation statements)
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“…The Paraná sedimentary basin is intercratonic, where the sedimentary sequence covers since the Silurian-Devonian up to the Cretaceous periods [3]. The Guarani aquifer has an average thickness of 300-400m, and is composed of silty and shaly sandstones of fluviallacustrine origin and variegated quartzitic sandstones accumulated by eolian processes under desertic conditions [4].…”
Section: State Of Artmentioning
confidence: 99%
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“…The Paraná sedimentary basin is intercratonic, where the sedimentary sequence covers since the Silurian-Devonian up to the Cretaceous periods [3]. The Guarani aquifer has an average thickness of 300-400m, and is composed of silty and shaly sandstones of fluviallacustrine origin and variegated quartzitic sandstones accumulated by eolian processes under desertic conditions [4].…”
Section: State Of Artmentioning
confidence: 99%
“…The mean annual precipitation is about 1300-1400 mm, while the mean temperature in the region is 20.5ºC [5]. [3,6]. [8].…”
Section: State Of Artmentioning
confidence: 99%
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“…Po [10][11][12]. Special attention is needed when sampling and handling radon-rich water because it escapes easily.…”
Section: Po and 214mentioning
confidence: 99%