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The synergistic effect of calcium on organic carbon sequestration to ferrihydrite
Sequestration of organic carbon (OC) in environmental systems is critical to mitigating climate change. Organo-mineral associations, especially those with iron (Fe) oxides, drive the chemistry of OC sequestration and stability in soils. Short-range-ordered Fe oxides, such as ferrihydrite, demonstrat...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer International Publishing
2018
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5797485/ https://www.ncbi.nlm.nih.gov/pubmed/29397451 http://dx.doi.org/10.1186/s12932-018-0049-4 |
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author | Sowers, Tyler D. Stuckey, Jason W. Sparks, Donald L. |
author_facet | Sowers, Tyler D. Stuckey, Jason W. Sparks, Donald L. |
author_sort | Sowers, Tyler D. |
collection | PubMed |
description | Sequestration of organic carbon (OC) in environmental systems is critical to mitigating climate change. Organo-mineral associations, especially those with iron (Fe) oxides, drive the chemistry of OC sequestration and stability in soils. Short-range-ordered Fe oxides, such as ferrihydrite, demonstrate a high affinity for OC in binary systems. Calcium commonly co-associates with OC and Fe oxides in soils, though the bonding mechanism (e.g., cation bridging) and implications of the co-association for OC sequestration remain unresolved. We explored the effect of calcium (Ca(2+)) on the sorption of dissolved OC to 2-line ferrihydrite. Sorption experiments were conducted between leaf litter-extractable OC and ferrihydrite at pH 4 to 9 with different initial C/Fe molar ratios and Ca(2+) concentrations. The extent of OC sorption to ferrihydrite in the presence of Ca(2+) increased across all tested pH values, especially at pH ≥ 7. Sorbed OC concentration at pH 9 increased from 8.72 ± 0.16 to 13.3 ± 0.20 mmol OC g(−1) ferrihydrite between treatments of no added Ca(2+) and 30 mM Ca(2+) addition. Batch experiments were paired with spectroscopic studies to probe the speciation of sorbed OC and elucidate the sorption mechanism. ATR-FTIR spectroscopy analysis revealed that carboxylic functional moieties were the primary sorbed OC species that were preferentially bound to ferrihydrite and suggested an increase in Fe-carboxylate ligand exchange in the presence of Ca at pH 9. Results from batch to spectroscopic experiments provide significant evidence for the enhancement of dissolved OC sequestration to 2-line ferrihydrite and suggest the formation of Fe–Ca-OC ternary complexes. Findings of this research will inform modeling of environmental C cycling and have the potential to influence strategies for managing land to minimize OM stabilization. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s12932-018-0049-4) contains supplementary material, which is available to authorized users. |
format | Online Article Text |
id | pubmed-5797485 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2018 |
publisher | Springer International Publishing |
record_format | MEDLINE/PubMed |
spelling | pubmed-57974852018-02-09 The synergistic effect of calcium on organic carbon sequestration to ferrihydrite Sowers, Tyler D. Stuckey, Jason W. Sparks, Donald L. Geochem Trans Research Article Sequestration of organic carbon (OC) in environmental systems is critical to mitigating climate change. Organo-mineral associations, especially those with iron (Fe) oxides, drive the chemistry of OC sequestration and stability in soils. Short-range-ordered Fe oxides, such as ferrihydrite, demonstrate a high affinity for OC in binary systems. Calcium commonly co-associates with OC and Fe oxides in soils, though the bonding mechanism (e.g., cation bridging) and implications of the co-association for OC sequestration remain unresolved. We explored the effect of calcium (Ca(2+)) on the sorption of dissolved OC to 2-line ferrihydrite. Sorption experiments were conducted between leaf litter-extractable OC and ferrihydrite at pH 4 to 9 with different initial C/Fe molar ratios and Ca(2+) concentrations. The extent of OC sorption to ferrihydrite in the presence of Ca(2+) increased across all tested pH values, especially at pH ≥ 7. Sorbed OC concentration at pH 9 increased from 8.72 ± 0.16 to 13.3 ± 0.20 mmol OC g(−1) ferrihydrite between treatments of no added Ca(2+) and 30 mM Ca(2+) addition. Batch experiments were paired with spectroscopic studies to probe the speciation of sorbed OC and elucidate the sorption mechanism. ATR-FTIR spectroscopy analysis revealed that carboxylic functional moieties were the primary sorbed OC species that were preferentially bound to ferrihydrite and suggested an increase in Fe-carboxylate ligand exchange in the presence of Ca at pH 9. Results from batch to spectroscopic experiments provide significant evidence for the enhancement of dissolved OC sequestration to 2-line ferrihydrite and suggest the formation of Fe–Ca-OC ternary complexes. Findings of this research will inform modeling of environmental C cycling and have the potential to influence strategies for managing land to minimize OM stabilization. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s12932-018-0049-4) contains supplementary material, which is available to authorized users. Springer International Publishing 2018-02-03 /pmc/articles/PMC5797485/ /pubmed/29397451 http://dx.doi.org/10.1186/s12932-018-0049-4 Text en © The Author(s) 2018 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 Sowers, Tyler D. Stuckey, Jason W. Sparks, Donald L. The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title | The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title_full | The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title_fullStr | The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title_full_unstemmed | The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title_short | The synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
title_sort | synergistic effect of calcium on organic carbon sequestration to ferrihydrite |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5797485/ https://www.ncbi.nlm.nih.gov/pubmed/29397451 http://dx.doi.org/10.1186/s12932-018-0049-4 |
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