Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland
Fluvial dissolved Fe concentrations decrease upon mixing with seawater, resulting in the formation of Fe-floccules. However, a clear understanding of the fate of these floccules has yet to be established. Assessing how tidal processes affect the formation of Fe-colloids in the Leirárvogur estuary, S...
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2011
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ftumanchesterpub:oai:pure.atira.dk:publications/d32f74dc-e3c0-4071-9c3d-834d0ec5a10f 2024-09-15T18:13:25+00:00 Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland Byrne, Gemma M. Worden, Richard H. Hodgson, David M. Polya, David A. Lythgoe, Paul R. Barrie, Craig D. Boyce, Adrian J. 2011-06 https://research.manchester.ac.uk/en/publications/d32f74dc-e3c0-4071-9c3d-834d0ec5a10f https://doi.org/10.1016/j.apgeochem.2011.03.018 eng eng https://research.manchester.ac.uk/en/publications/d32f74dc-e3c0-4071-9c3d-834d0ec5a10f info:eu-repo/semantics/closedAccess Byrne , G M , Worden , R H , Hodgson , D M , Polya , D A , Lythgoe , P R , Barrie , C D & Boyce , A J 2011 , ' Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland ' , Applied Geochemistry , vol. 26 , pp. S16-S19 . https://doi.org/10.1016/j.apgeochem.2011.03.018 article 2011 ftumanchesterpub https://doi.org/10.1016/j.apgeochem.2011.03.018 2024-08-26T23:36:14Z Fluvial dissolved Fe concentrations decrease upon mixing with seawater, resulting in the formation of Fe-floccules. However, a clear understanding of the fate of these floccules has yet to be established. Assessing how tidal processes affect the formation of Fe-colloids in the Leirárvogur estuary, SW Iceland, is an important step in understanding the formation and potential deposition of estuarine Fe-rich minerals within this estuarine system. The Leirárvogur estuary drains predominately Fe-rich basalt, increasing the likelihood of detecting changes in Fe-phases. Fluvial waters and local lake waters that drain into the estuary were compared and the effects of seasonal changes were considered, in an attempt to understand how varying end-members and external factors play a role in Fe-rich mineral formation. Aqueous and colloidal Fe concentrations were found to be greater towards the head of the Leirárvogur estuary, suggesting that potential Fe-rich minerals and complexes are forming at sites of fluvial input. Increasing suspended colloidal Fe towards the estuary mouth suggests that Fe-colloids are readily transported seaward. © 2011 Elsevier Ltd. Article in Journal/Newspaper Iceland The University of Manchester: Research Explorer Applied Geochemistry 26 S16 S19 |
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The University of Manchester: Research Explorer |
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ftumanchesterpub |
language |
English |
description |
Fluvial dissolved Fe concentrations decrease upon mixing with seawater, resulting in the formation of Fe-floccules. However, a clear understanding of the fate of these floccules has yet to be established. Assessing how tidal processes affect the formation of Fe-colloids in the Leirárvogur estuary, SW Iceland, is an important step in understanding the formation and potential deposition of estuarine Fe-rich minerals within this estuarine system. The Leirárvogur estuary drains predominately Fe-rich basalt, increasing the likelihood of detecting changes in Fe-phases. Fluvial waters and local lake waters that drain into the estuary were compared and the effects of seasonal changes were considered, in an attempt to understand how varying end-members and external factors play a role in Fe-rich mineral formation. Aqueous and colloidal Fe concentrations were found to be greater towards the head of the Leirárvogur estuary, suggesting that potential Fe-rich minerals and complexes are forming at sites of fluvial input. Increasing suspended colloidal Fe towards the estuary mouth suggests that Fe-colloids are readily transported seaward. © 2011 Elsevier Ltd. |
format |
Article in Journal/Newspaper |
author |
Byrne, Gemma M. Worden, Richard H. Hodgson, David M. Polya, David A. Lythgoe, Paul R. Barrie, Craig D. Boyce, Adrian J. |
spellingShingle |
Byrne, Gemma M. Worden, Richard H. Hodgson, David M. Polya, David A. Lythgoe, Paul R. Barrie, Craig D. Boyce, Adrian J. Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
author_facet |
Byrne, Gemma M. Worden, Richard H. Hodgson, David M. Polya, David A. Lythgoe, Paul R. Barrie, Craig D. Boyce, Adrian J. |
author_sort |
Byrne, Gemma M. |
title |
Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
title_short |
Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
title_full |
Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
title_fullStr |
Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
title_full_unstemmed |
Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland |
title_sort |
understanding the fate of iron in a modern temperate estuary: leirárvogur, iceland |
publishDate |
2011 |
url |
https://research.manchester.ac.uk/en/publications/d32f74dc-e3c0-4071-9c3d-834d0ec5a10f https://doi.org/10.1016/j.apgeochem.2011.03.018 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Byrne , G M , Worden , R H , Hodgson , D M , Polya , D A , Lythgoe , P R , Barrie , C D & Boyce , A J 2011 , ' Understanding the fate of iron in a modern temperate estuary: Leirárvogur, Iceland ' , Applied Geochemistry , vol. 26 , pp. S16-S19 . https://doi.org/10.1016/j.apgeochem.2011.03.018 |
op_relation |
https://research.manchester.ac.uk/en/publications/d32f74dc-e3c0-4071-9c3d-834d0ec5a10f |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1016/j.apgeochem.2011.03.018 |
container_title |
Applied Geochemistry |
container_volume |
26 |
container_start_page |
S16 |
op_container_end_page |
S19 |
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1810451185206820864 |