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Theme 3-8-Arsenic in groundwater and redox conditions in the Bengal delta – Possible in situ remediation

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dc.contributor.author Jacks, G.
dc.contributor.author Bhattacharya, Prosun
dc.contributor.author Ahmed, K. Matin
dc.contributor.author Chatterjee, D.
dc.date.accessioned 2019-10-10T10:37:01Z
dc.date.available 2019-10-10T10:37:01Z
dc.date.issued 2000
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/3697
dc.description.abstract Widespread arsenic contamination in groundwater in the Bengal Delta seems to be largely natural depending on reducing conditions in the aquifers. Reduction of ferric hydroxides with adsorbed arsenic species occurs at intermediate depth. In situ remediation might be achieved by artificial recharge stabilising the ferric hydroxides. It might however be problematic to keep the aquifer oxic. Sulphate levels are generally low and sulphur deficiency for crops common. The low sulphate levels favour methane fermentation over sulphate reduction. Application of gypsum to the surface soils might favour immobilisation of the arsenic in the form of sulphides. en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.subject Arsenic in groundwater en_US
dc.subject Bengal Delta en_US
dc.title Theme 3-8-Arsenic in groundwater and redox conditions in the Bengal delta – Possible in situ remediation en_US
dc.type Technical Report en_US


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