Treatise on Geochemistry 2014
DOI: 10.1016/b978-0-08-095975-7.00906-2
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Radioactivity, Geochemistry, and Health

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Cited by 10 publications
(6 citation statements)
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References 450 publications
(558 reference statements)
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“…The water-soluble fraction of Sr was higher than that of other trace metals except Mn in all soils. Although Sr can be released from the weathering of sulfate minerals and ion-exchange reactions with clay minerals (Siegel and Bryan 2014 ), aeolian dust input can be a major Sr source in arid regions (Coble et al 2015 ). The Mo content in the control soil was less than the EILs (40 mg/kg) but nearly 10 times higher than the EILs in the PHC-contaminated soils.…”
Section: Resultsmentioning
confidence: 99%
“…The water-soluble fraction of Sr was higher than that of other trace metals except Mn in all soils. Although Sr can be released from the weathering of sulfate minerals and ion-exchange reactions with clay minerals (Siegel and Bryan 2014 ), aeolian dust input can be a major Sr source in arid regions (Coble et al 2015 ). The Mo content in the control soil was less than the EILs (40 mg/kg) but nearly 10 times higher than the EILs in the PHC-contaminated soils.…”
Section: Resultsmentioning
confidence: 99%
“…Going on, the content of 226 Ra in aquifers is not only related to the abundance of its parent radionuclides [ 22 ], but also it is controlled by sorption, desorption, and ion exchange processes [ 23 ]. In particular, factors related to geology and climate that affect the acidity, redox potential, degree of mineralization, and composition of groundwater, as well as their potential residence time, can also affect sorption and, thereby, the distribution pattern of Ra-isotopes [ 23 ].…”
Section: Resultsmentioning
confidence: 99%
“…Going on, the content of 226 Ra in aquifers is not only related to the abundance of its parent radionuclides [ 22 ], but also it is controlled by sorption, desorption, and ion exchange processes [ 23 ]. In particular, factors related to geology and climate that affect the acidity, redox potential, degree of mineralization, and composition of groundwater, as well as their potential residence time, can also affect sorption and, thereby, the distribution pattern of Ra-isotopes [ 23 ]. Moreover, it is worth noting is that the investigated area falls within the Aspromonte Massifs, a geological segment of the Calabrian Arc, which consists of a series of Palaeozoic plutonic–metamorphic nappes, locally overlain by a Mesozoic–Cenozoic sedimentary cover.…”
Section: Resultsmentioning
confidence: 99%
“…Upon release to the environment, they may pose a severe threat. Their fate, behavior, and activity (emission of ionizing or non-ionizing radiation) are mainly controlled by their chemistry and the nature of their host environment (Siegel & Bryan, 2014).…”
Section: Naturally Occurring Radioactive Materials (Norms)mentioning
confidence: 99%