Hydrologic Versus Biogeochemical Control of Nutrient Dynamics in a Shallow Hypersaline Coastal Lagoon: Insight From a Coupled Hydrodynamic‐Water Quality Model
Shallow coastal lagoons with restricted connection to the ocean are often productive but can also be sensitive to nutrient enrichment and hydrologic changes. Resolving nutrient dynamics is important for their sustainable management, yet being able to accurately resolve nutrient budgets has remained...
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creator | Huang, Peisheng Mosley, Luke Brookes, Justin D. Sims, Claire Waycott, Michelle Paraska, Daniel Zhai, Sherry Y. Hipsey, Matthew R. |
description | Shallow coastal lagoons with restricted connection to the ocean are often productive but can also be sensitive to nutrient enrichment and hydrologic changes. Resolving nutrient dynamics is important for their sustainable management, yet being able to accurately resolve nutrient budgets has remained a challenge due to their complex hydrological regimes and habitat heterogeneity. In this study, we undertake a systematic nutrient budget of a large shallow hypersaline lagoon (Coorong, South Australia), with assistance of a high‐resolution coupled hydrodynamic‐biogeochemical model, to demonstrate the conditions that lead to nutrient retention. Under current conditions, high rates of evapo‐concentration and limited water connectivity have led to a persistent accumulation of nutrients and poor water quality in substantial areas of the lagoon. The interplay between hydrological drivers and biogeochemical processes was quantified using an adjusted Damköhler number, comparing the timescales of nutrient flushing versus processing. This showed a general transition from hydrologic control to biogeochemical control with increasing distance from the main ocean connection, modified by episodes of increased flows and external loads. Whilst water age was a useful indicator of the factors controlling rates of nutrient retention, interannual variability in retention between areas of the lagoon was explained based on river flows and changes in mean sea level. As the system has been affected by reduced flows over past decades, the results provide evidence that increasing river flow to the lagoon would reduce the nutrient retention, and we discuss the potential for net nutrient export to the ocean under sustained high flows.
Plain Language Summary
Nutrient loads to coastal waters have increased worldwide as a direct consequence of the growing human population and increased development, with the end result being degraded water quality. Coastal lagoons with topographically restricted connection to the ocean are particularly sensitive relative to other coastal ecosystems since poor flushing and evaporation promotes nutrient retention. Resolving processes and factors that “control” nutrient concentrations is therefore important for guiding water quality management and ecosystem restoration. We studied nutrient dynamics in the Coorong, a shallow hypersaline coastal lagoon located in South Australia, using a high‐resolution coupled hydrodynamic‐water quality model. We showed that redu |
doi_str_mv | 10.1029/2023JG007497 |
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Plain Language Summary
Nutrient loads to coastal waters have increased worldwide as a direct consequence of the growing human population and increased development, with the end result being degraded water quality. Coastal lagoons with topographically restricted connection to the ocean are particularly sensitive relative to other coastal ecosystems since poor flushing and evaporation promotes nutrient retention. Resolving processes and factors that “control” nutrient concentrations is therefore important for guiding water quality management and ecosystem restoration. We studied nutrient dynamics in the Coorong, a shallow hypersaline coastal lagoon located in South Australia, using a high‐resolution coupled hydrodynamic‐water quality model. We showed that reducing flows to the system, and low mean sea level anomalies, encourage increased nutrient recycling and retention within the lagoon, resulting in persistent accumulation of nutrients in the south lagoon where water quality has become degraded. Based on the results, we conclude that potential restoration measures must focus on increasing hydrologic control through managing flow volumes and/or ocean flushing in order to optimize nutrient export.
Key Points
An adjusted Damköhler number was developed to quantitatively compare hydrologic versus biogeochemical controls on nutrient dynamics
A transition from hydrologic control to biogeochemical control with increasing water retention time led to higher nutrient retention rates
Annual nutrient retention rates were co‐modulated by catchment inflows and mean sea levels</description><identifier>ISSN: 2169-8953</identifier><identifier>EISSN: 2169-8961</identifier><identifier>DOI: 10.1029/2023JG007497</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Accumulation ; Biogeochemistry ; Budgets ; Coastal ecology ; Coastal ecosystems ; Coastal lagoons ; Coastal management ; Coastal plains ; Coastal processes ; Coastal waters ; Control systems ; Ecosystem management ; Ecosystem restoration ; Environmental degradation ; Environmental restoration ; eutrophication ; Evaporation ; Evaporation rate ; Flushing ; Flushing (water) ; Heterogeneity ; High flow ; Human populations ; Hydrodynamics ; Hydrologic regime ; Hydrology ; hypersaline ; Lagoons ; Marine ecosystems ; Mean sea level ; Nutrient concentrations ; Nutrient dynamics ; Nutrient enrichment ; Nutrient flow ; Nutrient loading ; Nutrient retention ; Nutrients ; Quality management ; Retention ; River flow ; Rivers ; Sea level ; Sustainability management ; Water quality ; Water quality management</subject><ispartof>Journal of geophysical research. Biogeosciences, 2024-07, Vol.129 (7), p.n/a</ispartof><rights>2024 The Author(s).</rights><rights>2024. This article is published under http://creativecommons.org/licenses/by-nc/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c2323-e15cdd0fd0e4b0aa636b565dc294b13084f6e15ec88cec432e52964dccb736583</cites><orcidid>0000-0001-8408-9142 ; 0000-0001-8386-4354 ; 0009-0003-2717-0739 ; 0000-0002-8347-7175</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2023JG007497$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2023JG007497$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,1416,27915,27916,45565,45566</link.rule.ids></links><search><creatorcontrib>Huang, Peisheng</creatorcontrib><creatorcontrib>Mosley, Luke</creatorcontrib><creatorcontrib>Brookes, Justin D.</creatorcontrib><creatorcontrib>Sims, Claire</creatorcontrib><creatorcontrib>Waycott, Michelle</creatorcontrib><creatorcontrib>Paraska, Daniel</creatorcontrib><creatorcontrib>Zhai, Sherry Y.</creatorcontrib><creatorcontrib>Hipsey, Matthew R.</creatorcontrib><title>Hydrologic Versus Biogeochemical Control of Nutrient Dynamics in a Shallow Hypersaline Coastal Lagoon: Insight From a Coupled Hydrodynamic‐Water Quality Model</title><title>Journal of geophysical research. Biogeosciences</title><description>Shallow coastal lagoons with restricted connection to the ocean are often productive but can also be sensitive to nutrient enrichment and hydrologic changes. Resolving nutrient dynamics is important for their sustainable management, yet being able to accurately resolve nutrient budgets has remained a challenge due to their complex hydrological regimes and habitat heterogeneity. In this study, we undertake a systematic nutrient budget of a large shallow hypersaline lagoon (Coorong, South Australia), with assistance of a high‐resolution coupled hydrodynamic‐biogeochemical model, to demonstrate the conditions that lead to nutrient retention. Under current conditions, high rates of evapo‐concentration and limited water connectivity have led to a persistent accumulation of nutrients and poor water quality in substantial areas of the lagoon. The interplay between hydrological drivers and biogeochemical processes was quantified using an adjusted Damköhler number, comparing the timescales of nutrient flushing versus processing. This showed a general transition from hydrologic control to biogeochemical control with increasing distance from the main ocean connection, modified by episodes of increased flows and external loads. Whilst water age was a useful indicator of the factors controlling rates of nutrient retention, interannual variability in retention between areas of the lagoon was explained based on river flows and changes in mean sea level. As the system has been affected by reduced flows over past decades, the results provide evidence that increasing river flow to the lagoon would reduce the nutrient retention, and we discuss the potential for net nutrient export to the ocean under sustained high flows.
Plain Language Summary
Nutrient loads to coastal waters have increased worldwide as a direct consequence of the growing human population and increased development, with the end result being degraded water quality. Coastal lagoons with topographically restricted connection to the ocean are particularly sensitive relative to other coastal ecosystems since poor flushing and evaporation promotes nutrient retention. Resolving processes and factors that “control” nutrient concentrations is therefore important for guiding water quality management and ecosystem restoration. We studied nutrient dynamics in the Coorong, a shallow hypersaline coastal lagoon located in South Australia, using a high‐resolution coupled hydrodynamic‐water quality model. We showed that reducing flows to the system, and low mean sea level anomalies, encourage increased nutrient recycling and retention within the lagoon, resulting in persistent accumulation of nutrients in the south lagoon where water quality has become degraded. Based on the results, we conclude that potential restoration measures must focus on increasing hydrologic control through managing flow volumes and/or ocean flushing in order to optimize nutrient export.
Key Points
An adjusted Damköhler number was developed to quantitatively compare hydrologic versus biogeochemical controls on nutrient dynamics
A transition from hydrologic control to biogeochemical control with increasing water retention time led to higher nutrient retention rates
Annual nutrient retention rates were co‐modulated by catchment inflows and mean sea levels</description><subject>Accumulation</subject><subject>Biogeochemistry</subject><subject>Budgets</subject><subject>Coastal ecology</subject><subject>Coastal ecosystems</subject><subject>Coastal lagoons</subject><subject>Coastal management</subject><subject>Coastal plains</subject><subject>Coastal processes</subject><subject>Coastal waters</subject><subject>Control systems</subject><subject>Ecosystem management</subject><subject>Ecosystem restoration</subject><subject>Environmental degradation</subject><subject>Environmental restoration</subject><subject>eutrophication</subject><subject>Evaporation</subject><subject>Evaporation rate</subject><subject>Flushing</subject><subject>Flushing (water)</subject><subject>Heterogeneity</subject><subject>High flow</subject><subject>Human populations</subject><subject>Hydrodynamics</subject><subject>Hydrologic regime</subject><subject>Hydrology</subject><subject>hypersaline</subject><subject>Lagoons</subject><subject>Marine ecosystems</subject><subject>Mean sea level</subject><subject>Nutrient concentrations</subject><subject>Nutrient dynamics</subject><subject>Nutrient enrichment</subject><subject>Nutrient flow</subject><subject>Nutrient loading</subject><subject>Nutrient retention</subject><subject>Nutrients</subject><subject>Quality management</subject><subject>Retention</subject><subject>River flow</subject><subject>Rivers</subject><subject>Sea level</subject><subject>Sustainability management</subject><subject>Water quality</subject><subject>Water quality management</subject><issn>2169-8953</issn><issn>2169-8961</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><sourceid>WIN</sourceid><recordid>eNp9kUtOwzAQhiMEEhV0xwEssaXgR57soNCXCoj3MnLtSevKjYOdqMqOI3AEzsZJMBQhVsxmRjPf__-LCYIDgo8JptkJxZRNhhgnYZZsBR1K4qyXZjHZ_p0jtht0nVtiX6lfEdIJ3kettEabuRLoCaxrHDpXZg5GLGClBNeob8raE8gU6LqprYKyRhdtyf3VIVUiju4XXGuzRqO28g5cqxK8irvaq6d8bkx5isalU_NFjQbWrLykb5pKg0Tf6XLj9vH69sxrsOi28R51i66MBL0f7BRcO-j-9L3gcXD50B_1pjfDcf9s2hOUUdYDEgkpcSExhDPMecziWRRHUtAsnBGG07CIPQMiTQWIkFGIaBaHUohZwuIoZXvB4ca3sualAVfnS9PY0kfmXh0xlkYJ9tTRhhLWOGehyCurVty2OcH51xvyv2_wONvga6Wh_ZfNJ8O7IaVJytgnTqGMNw</recordid><startdate>202407</startdate><enddate>202407</enddate><creator>Huang, Peisheng</creator><creator>Mosley, Luke</creator><creator>Brookes, Justin D.</creator><creator>Sims, Claire</creator><creator>Waycott, Michelle</creator><creator>Paraska, Daniel</creator><creator>Zhai, Sherry Y.</creator><creator>Hipsey, Matthew R.</creator><general>Blackwell Publishing Ltd</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0001-8408-9142</orcidid><orcidid>https://orcid.org/0000-0001-8386-4354</orcidid><orcidid>https://orcid.org/0009-0003-2717-0739</orcidid><orcidid>https://orcid.org/0000-0002-8347-7175</orcidid></search><sort><creationdate>202407</creationdate><title>Hydrologic Versus Biogeochemical Control of Nutrient Dynamics in a Shallow Hypersaline Coastal Lagoon: Insight From a Coupled Hydrodynamic‐Water Quality Model</title><author>Huang, Peisheng ; Mosley, Luke ; Brookes, Justin D. ; Sims, Claire ; Waycott, Michelle ; Paraska, Daniel ; Zhai, Sherry Y. ; Hipsey, Matthew R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2323-e15cdd0fd0e4b0aa636b565dc294b13084f6e15ec88cec432e52964dccb736583</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Accumulation</topic><topic>Biogeochemistry</topic><topic>Budgets</topic><topic>Coastal ecology</topic><topic>Coastal ecosystems</topic><topic>Coastal lagoons</topic><topic>Coastal management</topic><topic>Coastal plains</topic><topic>Coastal processes</topic><topic>Coastal waters</topic><topic>Control systems</topic><topic>Ecosystem management</topic><topic>Ecosystem restoration</topic><topic>Environmental degradation</topic><topic>Environmental restoration</topic><topic>eutrophication</topic><topic>Evaporation</topic><topic>Evaporation rate</topic><topic>Flushing</topic><topic>Flushing (water)</topic><topic>Heterogeneity</topic><topic>High flow</topic><topic>Human populations</topic><topic>Hydrodynamics</topic><topic>Hydrologic regime</topic><topic>Hydrology</topic><topic>hypersaline</topic><topic>Lagoons</topic><topic>Marine ecosystems</topic><topic>Mean sea level</topic><topic>Nutrient concentrations</topic><topic>Nutrient dynamics</topic><topic>Nutrient enrichment</topic><topic>Nutrient flow</topic><topic>Nutrient loading</topic><topic>Nutrient retention</topic><topic>Nutrients</topic><topic>Quality management</topic><topic>Retention</topic><topic>River flow</topic><topic>Rivers</topic><topic>Sea level</topic><topic>Sustainability management</topic><topic>Water quality</topic><topic>Water quality management</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Huang, Peisheng</creatorcontrib><creatorcontrib>Mosley, Luke</creatorcontrib><creatorcontrib>Brookes, Justin D.</creatorcontrib><creatorcontrib>Sims, Claire</creatorcontrib><creatorcontrib>Waycott, Michelle</creatorcontrib><creatorcontrib>Paraska, Daniel</creatorcontrib><creatorcontrib>Zhai, Sherry Y.</creatorcontrib><creatorcontrib>Hipsey, Matthew R.</creatorcontrib><collection>Wiley-Blackwell Open Access Titles</collection><collection>Wiley Free Content</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of geophysical research. Biogeosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Huang, Peisheng</au><au>Mosley, Luke</au><au>Brookes, Justin D.</au><au>Sims, Claire</au><au>Waycott, Michelle</au><au>Paraska, Daniel</au><au>Zhai, Sherry Y.</au><au>Hipsey, Matthew R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrologic Versus Biogeochemical Control of Nutrient Dynamics in a Shallow Hypersaline Coastal Lagoon: Insight From a Coupled Hydrodynamic‐Water Quality Model</atitle><jtitle>Journal of geophysical research. Biogeosciences</jtitle><date>2024-07</date><risdate>2024</risdate><volume>129</volume><issue>7</issue><epage>n/a</epage><issn>2169-8953</issn><eissn>2169-8961</eissn><abstract>Shallow coastal lagoons with restricted connection to the ocean are often productive but can also be sensitive to nutrient enrichment and hydrologic changes. Resolving nutrient dynamics is important for their sustainable management, yet being able to accurately resolve nutrient budgets has remained a challenge due to their complex hydrological regimes and habitat heterogeneity. In this study, we undertake a systematic nutrient budget of a large shallow hypersaline lagoon (Coorong, South Australia), with assistance of a high‐resolution coupled hydrodynamic‐biogeochemical model, to demonstrate the conditions that lead to nutrient retention. Under current conditions, high rates of evapo‐concentration and limited water connectivity have led to a persistent accumulation of nutrients and poor water quality in substantial areas of the lagoon. The interplay between hydrological drivers and biogeochemical processes was quantified using an adjusted Damköhler number, comparing the timescales of nutrient flushing versus processing. This showed a general transition from hydrologic control to biogeochemical control with increasing distance from the main ocean connection, modified by episodes of increased flows and external loads. Whilst water age was a useful indicator of the factors controlling rates of nutrient retention, interannual variability in retention between areas of the lagoon was explained based on river flows and changes in mean sea level. As the system has been affected by reduced flows over past decades, the results provide evidence that increasing river flow to the lagoon would reduce the nutrient retention, and we discuss the potential for net nutrient export to the ocean under sustained high flows.
Plain Language Summary
Nutrient loads to coastal waters have increased worldwide as a direct consequence of the growing human population and increased development, with the end result being degraded water quality. Coastal lagoons with topographically restricted connection to the ocean are particularly sensitive relative to other coastal ecosystems since poor flushing and evaporation promotes nutrient retention. Resolving processes and factors that “control” nutrient concentrations is therefore important for guiding water quality management and ecosystem restoration. We studied nutrient dynamics in the Coorong, a shallow hypersaline coastal lagoon located in South Australia, using a high‐resolution coupled hydrodynamic‐water quality model. We showed that reducing flows to the system, and low mean sea level anomalies, encourage increased nutrient recycling and retention within the lagoon, resulting in persistent accumulation of nutrients in the south lagoon where water quality has become degraded. Based on the results, we conclude that potential restoration measures must focus on increasing hydrologic control through managing flow volumes and/or ocean flushing in order to optimize nutrient export.
Key Points
An adjusted Damköhler number was developed to quantitatively compare hydrologic versus biogeochemical controls on nutrient dynamics
A transition from hydrologic control to biogeochemical control with increasing water retention time led to higher nutrient retention rates
Annual nutrient retention rates were co‐modulated by catchment inflows and mean sea levels</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2023JG007497</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0001-8408-9142</orcidid><orcidid>https://orcid.org/0000-0001-8386-4354</orcidid><orcidid>https://orcid.org/0009-0003-2717-0739</orcidid><orcidid>https://orcid.org/0000-0002-8347-7175</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Accumulation Biogeochemistry Budgets Coastal ecology Coastal ecosystems Coastal lagoons Coastal management Coastal plains Coastal processes Coastal waters Control systems Ecosystem management Ecosystem restoration Environmental degradation Environmental restoration eutrophication Evaporation Evaporation rate Flushing Flushing (water) Heterogeneity High flow Human populations Hydrodynamics Hydrologic regime Hydrology hypersaline Lagoons Marine ecosystems Mean sea level Nutrient concentrations Nutrient dynamics Nutrient enrichment Nutrient flow Nutrient loading Nutrient retention Nutrients Quality management Retention River flow Rivers Sea level Sustainability management Water quality Water quality management |
title | Hydrologic Versus Biogeochemical Control of Nutrient Dynamics in a Shallow Hypersaline Coastal Lagoon: Insight From a Coupled Hydrodynamic‐Water Quality Model |
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