2008
DOI: 10.1016/j.gexplo.2008.01.002
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Arsenic mobilization in shallow aquifers of Datong Basin: Hydrochemical and mineralogical evidences

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Cited by 114 publications
(73 citation statements)
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References 22 publications
(22 reference statements)
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“…We evaluated information on soil characteristics including pH, salinity, texture, and so on, since soil features are factors of high As in groundwaters in south and east Asia (Smedley, 2003;Xie et al, 2008). Soil properties were complied from the "Harmonized World Soil Database" (FAO/IIASA/ISRIC/ISSCAS/JRC, 2009).…”
Section: Soil Informationmentioning
confidence: 99%
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“…We evaluated information on soil characteristics including pH, salinity, texture, and so on, since soil features are factors of high As in groundwaters in south and east Asia (Smedley, 2003;Xie et al, 2008). Soil properties were complied from the "Harmonized World Soil Database" (FAO/IIASA/ISRIC/ISSCAS/JRC, 2009).…”
Section: Soil Informationmentioning
confidence: 99%
“…We interpret that, in our study area, the high As concentrations are related to processes of reductive dissolution in reducing environments. Studies in Northern China showed that groundwaters exist in the reducing conditions and high As levels in groundwaters are enhanced by both high salinity and alkalinity in the semiarid-arid areas (Guo et al, 2008;Xie et al, 2008).…”
Section: Principal Component Analysismentioning
confidence: 99%
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“…Arsenic contamination of groundwater is a form of groundwater pollution which is often due to naturally occurring high concentrations of arsenic in deeper levels of groundwater (Wikipedia, 2017). Extensive scientific studies were investigated into the geochemical processes, resulting in high As level of concentration in groundwater almost all over the world [6][7][8][9]. During this period naturally occurring As was found to be widespread in groundwater [10].…”
Section: Introductionmentioning
confidence: 99%
“…Arsenic is released through sulfide mineral oxidation (e.g., arseno-rich pyrite, arsenopyrite), desorption (increase in pH), and reductive dissolution of arsenic-bearing Fe(III) and Mn(IV) oxyhydroxides [11][12][13]. Options to avoid potential problems related to arsenic intake from groundwater may include avoiding locating wells in high As regions, to use alternative water sources (e.g., surface water sources), and to treat groundwater contaminated with arsenic.…”
Section: Introductionmentioning
confidence: 99%