2007
DOI: 10.1016/j.scitotenv.2007.02.037
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Arsenic in the environment: Biology and Chemistry

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Cited by 508 publications
(167 citation statements)
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References 84 publications
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“…As(III) exists as H 3 AsO 3 when the pH is below 8.0. At pH values above 8.0, As(III) is gradually negatively charged, changing from H 2 AsO 3 − to HAsO 3 2− and finally to AsO 3 3− . 64 Because As(III) is gradually negatively charged when the pH is above 8.0, it is reasonable that the adsorption capacity decreases considerably for pH values above 11.0.…”
Section: Acs Applied Materials and Interfacesmentioning
confidence: 99%
“…As(III) exists as H 3 AsO 3 when the pH is below 8.0. At pH values above 8.0, As(III) is gradually negatively charged, changing from H 2 AsO 3 − to HAsO 3 2− and finally to AsO 3 3− . 64 Because As(III) is gradually negatively charged when the pH is above 8.0, it is reasonable that the adsorption capacity decreases considerably for pH values above 11.0.…”
Section: Acs Applied Materials and Interfacesmentioning
confidence: 99%
“…As(V) predominates in surface waters, while groundwater may also contain relevant concentrations of As(III) that are more mobile and toxic than As(V) [2]. Elevated concentrations of arsenic in groundwaters of China are the result of biogeochemical processes [3] or anthropogenic activities such as agriculture (the extensive use of herbicides and insecticides) and irregular disposal of hazardous waste from heavy industry [4][5].…”
mentioning
confidence: 99%
“…Arsenic may be found in soil as inorganic species as well as binding to organic compounds; however, it exists predominantly as inorganic species in soil. Inorganic As compounds may undergo methylation by microorganisms, producing, under oxidizing conditions, monomethylarsonic acid, dimethylarsinic acid, and trimethylarsine oxide [2,45,46]. Principle factors affecting the level of As in soils include the parent rock, climate, organic and inorganic components of the soil, and redox potential status [41,47].…”
Section: Occurrence Of Arsenic In Soilmentioning
confidence: 99%
“…enter air, water, and surface environments through wind-blown dust and runoff [1][2][3]. The primary source of As is natural, derived mainly from the interactions between groundwater and aquifer sediments and hard rocks of minerals, particularly pyrite (FeS 2 ), arsenopyrite (FeAsS), and other unspecified sulfide minerals [4][5][6], as well as secondary As-bearing minerals or mineral coatings, whereas industrial uses, agricultural activities, coal and oil exploitation and combustion, and mining of metal ores are anthropogenic sources that release As into groundwaters [7,8].…”
mentioning
confidence: 99%