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Interactions between magnetite and humic substances: redox reactions and dissolution processes
Humic substances (HS) are redox-active compounds that are ubiquitous in the environment and can serve as electron shuttles during microbial Fe(III) reduction thus reducing a variety of Fe(III) minerals. However, not much is known about redox reactions between HS and the mixed-valent mineral magnetit...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer International Publishing
2017
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5648731/ https://www.ncbi.nlm.nih.gov/pubmed/29086818 http://dx.doi.org/10.1186/s12932-017-0044-1 |
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author | Sundman, Anneli Byrne, James M. Bauer, Iris Menguy, Nicolas Kappler, Andreas |
author_facet | Sundman, Anneli Byrne, James M. Bauer, Iris Menguy, Nicolas Kappler, Andreas |
author_sort | Sundman, Anneli |
collection | PubMed |
description | Humic substances (HS) are redox-active compounds that are ubiquitous in the environment and can serve as electron shuttles during microbial Fe(III) reduction thus reducing a variety of Fe(III) minerals. However, not much is known about redox reactions between HS and the mixed-valent mineral magnetite (Fe(3)O(4)) that can potentially lead to changes in Fe(II)/Fe(III) stoichiometry and even dissolve the magnetite. To address this knowledge gap, we incubated non-reduced (native) and reduced HS with four types of magnetite that varied in particle size and solid-phase Fe(II)/Fe(III) stoichiometry. We followed dissolved and solid-phase Fe(II) and Fe(III) concentrations over time to quantify redox reactions between HS and magnetite. Magnetite redox reactions and dissolution processes with HS varied depending on the initial magnetite and HS properties. The interaction between biogenic magnetite and reduced HS resulted in dissolution of the solid magnetite mineral, as well as an overall reduction of the magnetite. In contrast, a slight oxidation and no dissolution was observed when native and reduced HS interacted with 500 nm magnetite. This variability in the solubility and electron accepting and donating capacity of the different types of magnetite is likely an effect of differences in their reduction potential that is correlated to the magnetite Fe(II)/Fe(III) stoichiometry, particle size, and crystallinity. Our study suggests that redox-active HS play an important role for Fe redox speciation within minerals such as magnetite and thereby influence the reactivity of these Fe minerals and their role in biogeochemical Fe cycling. Furthermore, such processes are also likely to have an effect on the fate of other elements bound to the surface of Fe minerals. [Image: see text] ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12932-017-0044-1) contains supplementary material, which is available to authorized users. |
format | Online Article Text |
id | pubmed-5648731 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2017 |
publisher | Springer International Publishing |
record_format | MEDLINE/PubMed |
spelling | pubmed-56487312017-11-02 Interactions between magnetite and humic substances: redox reactions and dissolution processes Sundman, Anneli Byrne, James M. Bauer, Iris Menguy, Nicolas Kappler, Andreas Geochem Trans Research Article Humic substances (HS) are redox-active compounds that are ubiquitous in the environment and can serve as electron shuttles during microbial Fe(III) reduction thus reducing a variety of Fe(III) minerals. However, not much is known about redox reactions between HS and the mixed-valent mineral magnetite (Fe(3)O(4)) that can potentially lead to changes in Fe(II)/Fe(III) stoichiometry and even dissolve the magnetite. To address this knowledge gap, we incubated non-reduced (native) and reduced HS with four types of magnetite that varied in particle size and solid-phase Fe(II)/Fe(III) stoichiometry. We followed dissolved and solid-phase Fe(II) and Fe(III) concentrations over time to quantify redox reactions between HS and magnetite. Magnetite redox reactions and dissolution processes with HS varied depending on the initial magnetite and HS properties. The interaction between biogenic magnetite and reduced HS resulted in dissolution of the solid magnetite mineral, as well as an overall reduction of the magnetite. In contrast, a slight oxidation and no dissolution was observed when native and reduced HS interacted with 500 nm magnetite. This variability in the solubility and electron accepting and donating capacity of the different types of magnetite is likely an effect of differences in their reduction potential that is correlated to the magnetite Fe(II)/Fe(III) stoichiometry, particle size, and crystallinity. Our study suggests that redox-active HS play an important role for Fe redox speciation within minerals such as magnetite and thereby influence the reactivity of these Fe minerals and their role in biogeochemical Fe cycling. Furthermore, such processes are also likely to have an effect on the fate of other elements bound to the surface of Fe minerals. [Image: see text] ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12932-017-0044-1) contains supplementary material, which is available to authorized users. Springer International Publishing 2017-10-19 /pmc/articles/PMC5648731/ /pubmed/29086818 http://dx.doi.org/10.1186/s12932-017-0044-1 Text en © The Author(s) 2017 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated. |
spellingShingle | Research Article Sundman, Anneli Byrne, James M. Bauer, Iris Menguy, Nicolas Kappler, Andreas Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title | Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title_full | Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title_fullStr | Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title_full_unstemmed | Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title_short | Interactions between magnetite and humic substances: redox reactions and dissolution processes |
title_sort | interactions between magnetite and humic substances: redox reactions and dissolution processes |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5648731/ https://www.ncbi.nlm.nih.gov/pubmed/29086818 http://dx.doi.org/10.1186/s12932-017-0044-1 |
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