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Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia

Sediment processes, including resuspension and transport, affect water quality in estuaries by altering light attenuation, primary productivity, and organic matter remineralization, which then influence oxygen and nitrogen dynamics. The relative importance of these processes on oxygen and nitrogen d...

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Autores principales: Moriarty, Julia M., Friedrichs, Marjorie A. M., Harris, Courtney K.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer US 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7752872/
https://www.ncbi.nlm.nih.gov/pubmed/33380995
http://dx.doi.org/10.1007/s12237-020-00763-8
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author Moriarty, Julia M.
Friedrichs, Marjorie A. M.
Harris, Courtney K.
author_facet Moriarty, Julia M.
Friedrichs, Marjorie A. M.
Harris, Courtney K.
author_sort Moriarty, Julia M.
collection PubMed
description Sediment processes, including resuspension and transport, affect water quality in estuaries by altering light attenuation, primary productivity, and organic matter remineralization, which then influence oxygen and nitrogen dynamics. The relative importance of these processes on oxygen and nitrogen dynamics varies in space and time due to multiple factors and is difficult to measure, however, motivating a modeling approach to quantify how sediment resuspension and transport affect estuarine biogeochemistry. Results from a coupled hydrodynamic–sediment transport–biogeochemical model of the Chesapeake Bay for the summers of 2002 and 2003 showed that resuspension increased light attenuation, especially in the northernmost portion of the Bay, shifting primary production downstream. Resuspension also increased remineralization in the central Bay, which experienced larger organic matter concentrations due to the downstream shift in primary productivity and estuarine circulation. As a result, oxygen decreased and ammonium increased throughout the Bay in the bottom portion of the water column, due to reduced photosynthesis in the northernmost portion of the Bay and increased remineralization in the central Bay. Averaged over the channel, resuspension decreased oxygen by ~ 25% and increased ammonium by ~ 50% for the bottom water column. Changes due to resuspension were of the same order of magnitude as, and generally exceeded, short-term variations within individual summers, as well as interannual variability between 2002 and 2003, which were wet and dry years, respectively. Our results quantify the degree to which sediment resuspension and transport affect biogeochemistry, and provide insight into how coastal systems may respond to management efforts and environmental changes. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s12237-020-00763-8) contains supplementary material, which is available to authorized users.
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spelling pubmed-77528722020-12-28 Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia Moriarty, Julia M. Friedrichs, Marjorie A. M. Harris, Courtney K. Estuaries Coast Article Sediment processes, including resuspension and transport, affect water quality in estuaries by altering light attenuation, primary productivity, and organic matter remineralization, which then influence oxygen and nitrogen dynamics. The relative importance of these processes on oxygen and nitrogen dynamics varies in space and time due to multiple factors and is difficult to measure, however, motivating a modeling approach to quantify how sediment resuspension and transport affect estuarine biogeochemistry. Results from a coupled hydrodynamic–sediment transport–biogeochemical model of the Chesapeake Bay for the summers of 2002 and 2003 showed that resuspension increased light attenuation, especially in the northernmost portion of the Bay, shifting primary production downstream. Resuspension also increased remineralization in the central Bay, which experienced larger organic matter concentrations due to the downstream shift in primary productivity and estuarine circulation. As a result, oxygen decreased and ammonium increased throughout the Bay in the bottom portion of the water column, due to reduced photosynthesis in the northernmost portion of the Bay and increased remineralization in the central Bay. Averaged over the channel, resuspension decreased oxygen by ~ 25% and increased ammonium by ~ 50% for the bottom water column. Changes due to resuspension were of the same order of magnitude as, and generally exceeded, short-term variations within individual summers, as well as interannual variability between 2002 and 2003, which were wet and dry years, respectively. Our results quantify the degree to which sediment resuspension and transport affect biogeochemistry, and provide insight into how coastal systems may respond to management efforts and environmental changes. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s12237-020-00763-8) contains supplementary material, which is available to authorized users. Springer US 2020-06-09 2021 /pmc/articles/PMC7752872/ /pubmed/33380995 http://dx.doi.org/10.1007/s12237-020-00763-8 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
Moriarty, Julia M.
Friedrichs, Marjorie A. M.
Harris, Courtney K.
Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title_full Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title_fullStr Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title_full_unstemmed Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title_short Seabed Resuspension in the Chesapeake Bay: Implications for Biogeochemical Cycling and Hypoxia
title_sort seabed resuspension in the chesapeake bay: implications for biogeochemical cycling and hypoxia
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7752872/
https://www.ncbi.nlm.nih.gov/pubmed/33380995
http://dx.doi.org/10.1007/s12237-020-00763-8
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