Solubility of iron in the Southern Ocean
International audience Iron solubility (cFe S) ranged from 0.4 to 1.5 nmol L -1, decreasing from south to north in three different Southern Ocean zones (the Coastal Zone, the Antarctic Zone, and the Polar Frontal Zone plus the Subantarctic Zone). This decrease was at times correlated with an increas...
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Online Access: | https://doi.org/10.4319/lo.2012.57.3.0684 https://hal.univ-brest.fr/hal-00710163 |
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fttriple:oai:gotriple.eu:10670/1.p64d2o 2023-05-15T14:03:00+02:00 Solubility of iron in the Southern Ocean Schlosser, C. De La Rocha, Christina, Streu, P. Croot, Peter Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR) National Oceanography Centre Southampton (NOC) University of Southampton Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Plymouth Marine Laboratory (PML) Plymouth Marine Laboratory 2012-03-15 https://doi.org/10.4319/lo.2012.57.3.0684 https://hal.univ-brest.fr/hal-00710163 en eng HAL CCSD Association for the Sciences of Limnology and Oceanography hal-00710163 doi:10.4319/lo.2012.57.3.0684 10670/1.p64d2o https://hal.univ-brest.fr/hal-00710163 undefined Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0024-3590 EISSN: 1939-5590 Limnology and Oceanography Limnology and Oceanography, Association for the Sciences of Limnology and Oceanography, 2012, 57 (3), pp.684-697. ⟨10.4319/lo.2012.57.3.0684⟩ geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2012 fttriple https://doi.org/10.4319/lo.2012.57.3.0684 2023-01-22T18:51:21Z International audience Iron solubility (cFe S) ranged from 0.4 to 1.5 nmol L -1, decreasing from south to north in three different Southern Ocean zones (the Coastal Zone, the Antarctic Zone, and the Polar Frontal Zone plus the Subantarctic Zone). This decrease was at times correlated with an increase in temperature. Organic Fe solubility (cFe S,org), which was obtained by subtracting from total measured Fe solubility the solubility of inorganic species of iron (Fe) at the measurement temperature (20°C), ranged from 0.3 to 1.3 nmol L -1, representing an average of 32 ± 14% of the concentration of ligands in the dissolved size fraction as determined via competitive ligand exchange- absorptive cathodic stripping voltammetry (barring a handful of extremely high values from a transect run to the east of Prydz Bay). Values of cFe S were mainly lower than the predicted value for inorganic Fe solubility at the in situ temperature. Total in situ Fe solubility (cFe S,adj) was therefore estimated by adjusting for inorganic Fe solubility at in situ temperatures (between -2°C and +18°C). Because in situ temperatures in the Antarctic Circumpolar Current were mostly lower than +3°C, such cFe S,adj values, ranging from 0.5 to 1.8 nmol L -1, were roughly twice as large as cFe S,org. The adjustment relies heavily on model calculations of inorganic Fe solubility but, if correct, indicates that the bulk of the solubility of Fe in the cold waters of the Southern Ocean is tied to the solubility of inorganic Fe rather than to Fe ligands in the soluble size fraction. Article in Journal/Newspaper Antarc* Antarctic Prydz Bay Southern Ocean Unknown Antarctic Prydz Bay Southern Ocean The Antarctic Limnology and Oceanography 57 3 684 697 |
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geo envir |
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geo envir Schlosser, C. De La Rocha, Christina, Streu, P. Croot, Peter Solubility of iron in the Southern Ocean |
topic_facet |
geo envir |
description |
International audience Iron solubility (cFe S) ranged from 0.4 to 1.5 nmol L -1, decreasing from south to north in three different Southern Ocean zones (the Coastal Zone, the Antarctic Zone, and the Polar Frontal Zone plus the Subantarctic Zone). This decrease was at times correlated with an increase in temperature. Organic Fe solubility (cFe S,org), which was obtained by subtracting from total measured Fe solubility the solubility of inorganic species of iron (Fe) at the measurement temperature (20°C), ranged from 0.3 to 1.3 nmol L -1, representing an average of 32 ± 14% of the concentration of ligands in the dissolved size fraction as determined via competitive ligand exchange- absorptive cathodic stripping voltammetry (barring a handful of extremely high values from a transect run to the east of Prydz Bay). Values of cFe S were mainly lower than the predicted value for inorganic Fe solubility at the in situ temperature. Total in situ Fe solubility (cFe S,adj) was therefore estimated by adjusting for inorganic Fe solubility at in situ temperatures (between -2°C and +18°C). Because in situ temperatures in the Antarctic Circumpolar Current were mostly lower than +3°C, such cFe S,adj values, ranging from 0.5 to 1.8 nmol L -1, were roughly twice as large as cFe S,org. The adjustment relies heavily on model calculations of inorganic Fe solubility but, if correct, indicates that the bulk of the solubility of Fe in the cold waters of the Southern Ocean is tied to the solubility of inorganic Fe rather than to Fe ligands in the soluble size fraction. |
author2 |
Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR) National Oceanography Centre Southampton (NOC) University of Southampton Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Plymouth Marine Laboratory (PML) Plymouth Marine Laboratory |
format |
Article in Journal/Newspaper |
author |
Schlosser, C. De La Rocha, Christina, Streu, P. Croot, Peter |
author_facet |
Schlosser, C. De La Rocha, Christina, Streu, P. Croot, Peter |
author_sort |
Schlosser, C. |
title |
Solubility of iron in the Southern Ocean |
title_short |
Solubility of iron in the Southern Ocean |
title_full |
Solubility of iron in the Southern Ocean |
title_fullStr |
Solubility of iron in the Southern Ocean |
title_full_unstemmed |
Solubility of iron in the Southern Ocean |
title_sort |
solubility of iron in the southern ocean |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://doi.org/10.4319/lo.2012.57.3.0684 https://hal.univ-brest.fr/hal-00710163 |
geographic |
Antarctic Prydz Bay Southern Ocean The Antarctic |
geographic_facet |
Antarctic Prydz Bay Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Prydz Bay Southern Ocean |
genre_facet |
Antarc* Antarctic Prydz Bay Southern Ocean |
op_source |
Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0024-3590 EISSN: 1939-5590 Limnology and Oceanography Limnology and Oceanography, Association for the Sciences of Limnology and Oceanography, 2012, 57 (3), pp.684-697. ⟨10.4319/lo.2012.57.3.0684⟩ |
op_relation |
hal-00710163 doi:10.4319/lo.2012.57.3.0684 10670/1.p64d2o https://hal.univ-brest.fr/hal-00710163 |
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https://doi.org/10.4319/lo.2012.57.3.0684 |
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Limnology and Oceanography |
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57 |
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684 |
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