2004
DOI: 10.1038/nature02638
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Role of metal-reducing bacteria in arsenic release from Bengal delta sediments

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Cited by 1,056 publications
(697 citation statements)
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“…Researchers have found that As mobilization is enhanced by As(V) reduction from As-bearing minerals in the presence of As- reducing bacteria (Smeaton et al, 2012;Smith et al, 2014). As detailed by Tian et al (2015) microbial Fe(III) reduction may have two opposite consequences on the fate of associated As: mobilization (Cummings et al, 1999;Islam et al, 2004) and sequestration (Coker et al, 2006;Islam et al, 2005;Jiang et al, 2013). In anaerobic environments, the adsorption ability for As is weaker due to the reductive dissolution of Fe(III) oxides in the presence of Fe(III)-reducing bacteria; consequently, the As bioaccessibility is greatly increased.…”
Section: Arsenic Bioaccessibility In the Colon Phasementioning
confidence: 99%
“…Researchers have found that As mobilization is enhanced by As(V) reduction from As-bearing minerals in the presence of As- reducing bacteria (Smeaton et al, 2012;Smith et al, 2014). As detailed by Tian et al (2015) microbial Fe(III) reduction may have two opposite consequences on the fate of associated As: mobilization (Cummings et al, 1999;Islam et al, 2004) and sequestration (Coker et al, 2006;Islam et al, 2005;Jiang et al, 2013). In anaerobic environments, the adsorption ability for As is weaker due to the reductive dissolution of Fe(III) oxides in the presence of Fe(III)-reducing bacteria; consequently, the As bioaccessibility is greatly increased.…”
Section: Arsenic Bioaccessibility In the Colon Phasementioning
confidence: 99%
“…It is generally agreed that there are two main processes controlling the mobilization of As to the groundwaters: (1) Microbially mediated reductive dissolution of Fe oxi-hydroxides is the main process leading to the release of As under reducing conditions in young alluvial and deltaic sediments containing elevated organic carbon contents Islam et al, 2004;Roberts et al, 2010). (2) Alkali desorption of arsenate from iron-oxide surfaces occurring in oxidizing environments in arid and semi-arid climates with high pH (Nicolli et al, 2010;Nordstrom, 2002;Smedley and Kinniburgh, 2002).…”
Section: Introductionmentioning
confidence: 99%
“…Arsenic can also be released from arsenopyrite (FeSAs) under aerobic conditions and in many aquifers around the world; the lowering of the water table has been held responsible for creating an aerobic environment through introduction of atmospheric oxygen (Das et al 1994;Shreiber et al 2000;Smith et al 2000;Chakraborty et al 2003;Bhattacharjee et al 2005;Pal et al 2007b). The other school of thought (Akai et al 2004;Islam et al 2004;vanGeen et al 2004;Stute et al 2007;Sengupta et al 2008) believes that arsenic leaching which is caused by bio-mediated reductive dissolution of arsenic-bearing ferric-oxyhydroxide is mainly responsible for the problem of arsenic contamination in the Bengal delta basin. Reduction of oxyhydroxides (FeOOH) in alluvial aquifers needs organic matter (OM), the source of which may be anthropogenic (unsewered sanitation, surface soils) or authigenic.…”
Section: Occurrence and Causes Of Arsenic Contamination Of Groundwatermentioning
confidence: 99%
“…It is suggested by many researchers (Ormland et al 2002;Islam et al 2004) that rapid burial of OM along with sediments facilitates microbial activities which generate reducing conditions favourable to the formation of sulphide minerals containing arsenic. Nickson et al (2005) in their investigation on the causes of shallow groundwater (530 m deep) contamination in Muzaffargarh District of Pakistan blamed sewage, animal and human wastes (anthropogenic OM) for the reduction of hydrous ferric oxide and the release of sorbed arsenic into groundwater, though the surface source of OM in driving such reduction processes has been considered as extremely unlikely (Sengupta et al 2008).…”
Section: Occurrence and Causes Of Arsenic Contamination Of Groundwatermentioning
confidence: 99%
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