1991
DOI: 10.1007/bf00282890
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Effects of acidification and natural organic materials on the mobility of arsenic in the environment

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Cited by 172 publications
(80 citation statements)
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“…Much work has been devoted to the study of arsenate adsorption on individual soil minerals, for example on iron oxides (Pierce and Moore, 1982;Fendorf et al, 1997), aluminium oxides (Anderson et al, 1975;Xu et al, 1991), manganese oxides (Oscarson et al, 1983), phyllosilicate clay minerals (Frost and Griffin, 1977;Goldberg and Glaubig, 1988), and on calcium carbonate (Goldberg and Glaubig, 1988). However, although there are some studies of arsenate adsorption on intact soils (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Much work has been devoted to the study of arsenate adsorption on individual soil minerals, for example on iron oxides (Pierce and Moore, 1982;Fendorf et al, 1997), aluminium oxides (Anderson et al, 1975;Xu et al, 1991), manganese oxides (Oscarson et al, 1983), phyllosilicate clay minerals (Frost and Griffin, 1977;Goldberg and Glaubig, 1988), and on calcium carbonate (Goldberg and Glaubig, 1988). However, although there are some studies of arsenate adsorption on intact soils (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Both dissolved silicate (Luxton et al, 2008) and organic matter (Grafe et al, 2001(Grafe et al, , 2002 can also competitively limit arsenic adsorption or promote desorption, with concentrations common to soils and sediments having an appreciable impact on dissolved arsenic concentrations. Carbonate can also compete with arsenic for adsorption sites on mineral surfaces ( Van Geen et al, 1994;Kim et al, 2000;Villalobos and Leckie, 2001;Appelo et al, 2002;Lee and Nriagu, 2003 ), and natural organic matter may also compete with As and inhibit arsenic adsorption onto iron (hydr)oxides due to competitive adsorption (Xu et al, 1991;Redman et al, 2002). Other anions, such as Cl -, SO 4 2-, and NO 3 -, have minimal impact on As desorption, yet these ions can contribute to ionic strength and salinization effects on As retention in soils and sediments (Gupta and Chen, 1978;Smith et al, 1998) that are potentially important in the desorption of arsenite.…”
Section: Ion Displacementmentioning
confidence: 99%
“…In natural conditions, As speciation is controlled by chemical properties such as pH and redox conditions, along with absorption, desorption, and ion exchange reactions (Ferguson and Gavis 1972;Sadiq 1997). As adsorption is high at low pH and decreases with increasing pH (Xu et al 1991). At all pH values, arsenate bonds more easily than arsenite and therefore, arsenite is also more mobile than arsenate (Kim et al 2012).…”
Section: Introductionmentioning
confidence: 99%