Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions

The potentially toxic Fe-CN complexes ferricyanide, [FeIII(CN)6]3−, and ferrocyanide, [FeII(CN)6]4−, undergo a variety of redox processes in soil, which affect their mobility. We carried out microcosm experiments with suspensions of a humic topsoil (pH 5.3; Corg...

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Main Authors: Thilo Rennert, Tim Mansfeldt
Format: Article
Language:English
Published: Hindawi Limited 2009-01-01
Series:Applied and Environmental Soil Science
Online Access:http://dx.doi.org/10.1155/2009/857640
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spelling doaj-174d3a35fed7455ba6433df5bfbda9322020-11-24T21:24:35ZengHindawi LimitedApplied and Environmental Soil Science1687-76671687-76752009-01-01200910.1155/2009/857640857640Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox ConditionsThilo Rennert0Tim Mansfeldt1Institut für Geowissenschaften, Friedrich-Schiller-Universität Jena, Burgweg 11, 07749 Jena, GermanyGeographisches Institut, Universität zu Köln, Albertus-Magnus-Platz, 50923 Köln, GermanyThe potentially toxic Fe-CN complexes ferricyanide, [FeIII(CN)6]3−, and ferrocyanide, [FeII(CN)6]4−, undergo a variety of redox processes in soil, which affect their mobility. We carried out microcosm experiments with suspensions of a humic topsoil (pH 5.3; Corg 107 g kg-1) to which we added ferricyanide (20 mg l-1). We varied the redox potential (EH) from −280 to 580 mV by using O2, N2 and glucose. The decrease of EH led to decreasing concentrations of Fe-CN complexes and partial reductive dissolution of (hydrous) Fe and Mn oxides. The dynamics of aqueous Fe-CN concentrations was characterized by decreasing concentrations when the pH rose and the EH dropped. We attribute these dependencies to adsorption on organic surfaces, for which such a pH/EH behavior has been shown previously. Adsorption was reversible, because when the pH and EH changed into the opposite direction, desorption occurred. This study demonstrates the possible impact of soil organic matter on the fate of Fe-CN complexes in soil.http://dx.doi.org/10.1155/2009/857640
collection DOAJ
language English
format Article
sources DOAJ
author Thilo Rennert
Tim Mansfeldt
spellingShingle Thilo Rennert
Tim Mansfeldt
Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
Applied and Environmental Soil Science
author_facet Thilo Rennert
Tim Mansfeldt
author_sort Thilo Rennert
title Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
title_short Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
title_full Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
title_fullStr Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
title_full_unstemmed Mobility of Iron-Cyanide Complexes in a Humic Topsoil under Varying Redox Conditions
title_sort mobility of iron-cyanide complexes in a humic topsoil under varying redox conditions
publisher Hindawi Limited
series Applied and Environmental Soil Science
issn 1687-7667
1687-7675
publishDate 2009-01-01
description The potentially toxic Fe-CN complexes ferricyanide, [FeIII(CN)6]3−, and ferrocyanide, [FeII(CN)6]4−, undergo a variety of redox processes in soil, which affect their mobility. We carried out microcosm experiments with suspensions of a humic topsoil (pH 5.3; Corg 107 g kg-1) to which we added ferricyanide (20 mg l-1). We varied the redox potential (EH) from −280 to 580 mV by using O2, N2 and glucose. The decrease of EH led to decreasing concentrations of Fe-CN complexes and partial reductive dissolution of (hydrous) Fe and Mn oxides. The dynamics of aqueous Fe-CN concentrations was characterized by decreasing concentrations when the pH rose and the EH dropped. We attribute these dependencies to adsorption on organic surfaces, for which such a pH/EH behavior has been shown previously. Adsorption was reversible, because when the pH and EH changed into the opposite direction, desorption occurred. This study demonstrates the possible impact of soil organic matter on the fate of Fe-CN complexes in soil.
url http://dx.doi.org/10.1155/2009/857640
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