Removal of Fe(II) from groundwater via aqueous portlandite carbonation and calcite-solution interactions

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Removal of Fe(II) from groundwater via aqueous portlandite carbonation and calcite-solution interactions

Fresh groundwater is sometimes enriched with dissolved ferrous iron (Fe(II)) that restricts its consumption as potable water because it forms colloidal red matter (mainly ferric oxyhydroxides) under oxic conditions at near neutral pH (>6) conditions. As already demonstrated, natural or synthetic...

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Bibliographic Details
Main Authors:	Hamdouni, A., Montes-Hernandez, G., Tlili, M., Findling, N., Renard, F., Putnis, Christine
Format:	Journal Article
Published:	Elsevier BV 2016
Online Access:	http://hdl.handle.net/20.500.11937/11423

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