Sorption and catalytic oxidation of Fe(II) at the surface of calcite

International audience The effect of sorption and coprecipitation of Fe(II) with calcite on the kinetics of Fe(II) oxidation was investigated. The interaction of Fe(II) with calcite was studied experimentally in the absence and presence of oxygen. The sorption of Fe(II) on calcite occurred in two di...

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Published in:Geochimica et Cosmochimica Acta
Main Authors: Mettler, Suzanne, Wolthers, Mariette, Charlet, Laurent, von Gunten, Urs
Other Authors: Swiss Federal Insitute of Aquatic Science and Technology Dübendorf (EAWAG), Laboratoire de Géophysique Interne et Tectonophysique (LGIT), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Faculty of Geosciences, UCEL, Universiteit Utrecht / Utrecht University Utrecht, funding by KTI, partial funding by RECOSY, partial funding by ANDRA and VENI grant #016.071.018 of NWO, ANR-05-PCO2-0009,Geocarbone-CARBONATATION, Bio Minéralisation du carbone: de la caractérisation expérimentale à la modélisation(2005)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://insu.hal.science/insu-00447473
https://doi.org/10.1016/j.gca.2009.01.003
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description International audience The effect of sorption and coprecipitation of Fe(II) with calcite on the kinetics of Fe(II) oxidation was investigated. The interaction of Fe(II) with calcite was studied experimentally in the absence and presence of oxygen. The sorption of Fe(II) on calcite occurred in two distinguishable steps: (a) a rapid adsorption step (seconds–minutes) was followed by (b) a slower incorporation (hours–weeks). The incorporated Fe(II) could not be remobilized by a strong complexing agent (phenanthroline or ferrozine) but the dissolution of the outmost calcite layers with carbonic acid allowed its recovery. Based on results of the latter dissolution experiments, a stoichiometry of 0.4 mol% Fe:Ca and a mixed carbonate layer thickness of 25 nm (after 168 h equilibration) were estimated. Fe(II) sorption on calcite could be successfully described by a surface adsorption and precipitation model (Comans & Middelburg, GCA 51 (1987), 2587) and surface complexation modeling (Van Cappellen et al., GCA 57 (1993), 3505; Pokrovsky et al., Langmuir 16 (2000), 2677). The surface complex model required the consideration of two adsorbed Fe(II) surface species, >CO3Fe + and >CO 3FeCO3H 0. For the formation of the latter species, a stability constant is being suggested. The oxidation kinetics of Fe(II) in the presence of calcite depended on the equilibration time of aqueous Fe(II) with the mineral prior to the introduction of oxygen. If pre-equilibrated for >15 h, the oxidation kinetics was comparable to a calcite-free system (t1/2 = 145 ± 15 min). Conversely, if Fe(II) was added to an aerated calcite suspension, the rate of oxidation was higher than in the absence of calcite (t1/2 = 41 ± 1 min and t1/2 = 100 ± 15 min, respectively). This catalysis was due to the greater reactivity of the adsorbed Fe(II) species, >CO3FeCO3H 0, for which the species specific rate constant was estimated
author2 Swiss Federal Insitute of Aquatic Science and Technology Dübendorf (EAWAG)
Laboratoire de Géophysique Interne et Tectonophysique (LGIT)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)
Faculty of Geosciences, UCEL
Universiteit Utrecht / Utrecht University Utrecht
funding by KTI, partial funding by RECOSY, partial funding by ANDRA and VENI grant #016.071.018 of NWO
ANR-05-PCO2-0009,Geocarbone-CARBONATATION, Bio Minéralisation du carbone: de la caractérisation expérimentale à la modélisation(2005)
format Article in Journal/Newspaper
author Mettler, Suzanne
Wolthers, Mariette
Charlet, Laurent
von Gunten, Urs
spellingShingle Mettler, Suzanne
Wolthers, Mariette
Charlet, Laurent
von Gunten, Urs
Sorption and catalytic oxidation of Fe(II) at the surface of calcite
author_facet Mettler, Suzanne
Wolthers, Mariette
Charlet, Laurent
von Gunten, Urs
author_sort Mettler, Suzanne
title Sorption and catalytic oxidation of Fe(II) at the surface of calcite
title_short Sorption and catalytic oxidation of Fe(II) at the surface of calcite
title_full Sorption and catalytic oxidation of Fe(II) at the surface of calcite
title_fullStr Sorption and catalytic oxidation of Fe(II) at the surface of calcite
title_full_unstemmed Sorption and catalytic oxidation of Fe(II) at the surface of calcite
title_sort sorption and catalytic oxidation of fe(ii) at the surface of calcite
publisher HAL CCSD
publishDate 2009
url https://insu.hal.science/insu-00447473
https://doi.org/10.1016/j.gca.2009.01.003
genre Carbonic acid
genre_facet Carbonic acid
op_source ISSN: 0016-7037
EISSN: 0016-7037
Geochimica et Cosmochimica Acta
https://insu.hal.science/insu-00447473
Geochimica et Cosmochimica Acta, 2009, 73 (7), pp.1826-1840. ⟨10.1016/j.gca.2009.01.003⟩
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container_title Geochimica et Cosmochimica Acta
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container_issue 7
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spelling ftunivsavoie:oai:HAL:insu-00447473v1 2024-04-21T07:59:35+00:00 Sorption and catalytic oxidation of Fe(II) at the surface of calcite Mettler, Suzanne Wolthers, Mariette Charlet, Laurent von Gunten, Urs Swiss Federal Insitute of Aquatic Science and Technology Dübendorf (EAWAG) Laboratoire de Géophysique Interne et Tectonophysique (LGIT) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Central des Ponts et Chaussées (LCPC)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) Faculty of Geosciences, UCEL Universiteit Utrecht / Utrecht University Utrecht funding by KTI, partial funding by RECOSY, partial funding by ANDRA and VENI grant #016.071.018 of NWO ANR-05-PCO2-0009,Geocarbone-CARBONATATION, Bio Minéralisation du carbone: de la caractérisation expérimentale à la modélisation(2005) 2009-04-01 https://insu.hal.science/insu-00447473 https://doi.org/10.1016/j.gca.2009.01.003 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gca.2009.01.003 insu-00447473 https://insu.hal.science/insu-00447473 doi:10.1016/j.gca.2009.01.003 ISSN: 0016-7037 EISSN: 0016-7037 Geochimica et Cosmochimica Acta https://insu.hal.science/insu-00447473 Geochimica et Cosmochimica Acta, 2009, 73 (7), pp.1826-1840. ⟨10.1016/j.gca.2009.01.003⟩ info:eu-repo/semantics/article Journal articles 2009 ftunivsavoie https://doi.org/10.1016/j.gca.2009.01.003 2024-04-11T00:24:45Z International audience The effect of sorption and coprecipitation of Fe(II) with calcite on the kinetics of Fe(II) oxidation was investigated. The interaction of Fe(II) with calcite was studied experimentally in the absence and presence of oxygen. The sorption of Fe(II) on calcite occurred in two distinguishable steps: (a) a rapid adsorption step (seconds–minutes) was followed by (b) a slower incorporation (hours–weeks). The incorporated Fe(II) could not be remobilized by a strong complexing agent (phenanthroline or ferrozine) but the dissolution of the outmost calcite layers with carbonic acid allowed its recovery. Based on results of the latter dissolution experiments, a stoichiometry of 0.4 mol% Fe:Ca and a mixed carbonate layer thickness of 25 nm (after 168 h equilibration) were estimated. Fe(II) sorption on calcite could be successfully described by a surface adsorption and precipitation model (Comans & Middelburg, GCA 51 (1987), 2587) and surface complexation modeling (Van Cappellen et al., GCA 57 (1993), 3505; Pokrovsky et al., Langmuir 16 (2000), 2677). The surface complex model required the consideration of two adsorbed Fe(II) surface species, >CO3Fe + and >CO 3FeCO3H 0. For the formation of the latter species, a stability constant is being suggested. The oxidation kinetics of Fe(II) in the presence of calcite depended on the equilibration time of aqueous Fe(II) with the mineral prior to the introduction of oxygen. If pre-equilibrated for >15 h, the oxidation kinetics was comparable to a calcite-free system (t1/2 = 145 ± 15 min). Conversely, if Fe(II) was added to an aerated calcite suspension, the rate of oxidation was higher than in the absence of calcite (t1/2 = 41 ± 1 min and t1/2 = 100 ± 15 min, respectively). This catalysis was due to the greater reactivity of the adsorbed Fe(II) species, >CO3FeCO3H 0, for which the species specific rate constant was estimated Article in Journal/Newspaper Carbonic acid Université Savoie Mont Blanc: HAL Geochimica et Cosmochimica Acta 73 7 1826 1840