Treatise on Geochemistry 2014
DOI: 10.1016/b978-0-08-095975-7.00906-2
|View full text |Cite
|
Sign up to set email alerts
|

Radioactivity, Geochemistry, and Health

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1

Citation Types

0
4
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
4
2

Relationship

0
6

Authors

Journals

citations
Cited by 8 publications
(4 citation statements)
references
References 450 publications
(558 reference statements)
0
4
0
Order By: Relevance
“…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%
“…Inherently, coals, coal combustion residuals (CCRs), and soils commonly possess naturally occurring radioactive materials (NORMs) including Th and U actinide series and their progenies, along with other radionuclide, e.g., 40 K (Habib et al 2019a, b;Chen et al 2011Chen et al , 2017aOrem and Finkelman 2014;Arbuzov et al 2011) (Table 24.14). The degree of gamma radiation is directly related to the radioactivity concentrations of NORMs (Siegel and Bryan 2014). Considering the abundances of NORMs ( 226 Ra, 232 Th, 238 U, and 40 K), the evaluation of radiological risks owing to the environmental radioactivity is more important compared to merely studying the hazardous radioactive wastes (Dragović et al 2008(Dragović et al , 2013Vuković et al 1996).…”
Section: Radionuclidesmentioning
confidence: 99%