The bioavailability of particulate nitrogen in eroded sediment: Catchment sources and processes

Purpose Anthropogenic land use change has caused an increase in particulate nutrient loads from catchments draining to the Great Barrier Reef (GBR). The research in GBR catchments has indicated that particulate nutrients are bioavailable to both freshwater and marine phytoplankton, but relative impo...

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Veröffentlicht in:Journal of soils and sediments 2024-03, Vol.24 (3), p.1402-1419
Hauptverfasser: Garzon-Garcia, Alexandra, Burton, Joanne M., Ellis, Rob, Askildsen, Maria, Bloesch, Philip, De Hayr, Rob, Moody, Phil
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container_end_page 1419
container_issue 3
container_start_page 1402
container_title Journal of soils and sediments
container_volume 24
creator Garzon-Garcia, Alexandra
Burton, Joanne M.
Ellis, Rob
Askildsen, Maria
Bloesch, Philip
De Hayr, Rob
Moody, Phil
description Purpose Anthropogenic land use change has caused an increase in particulate nutrient loads from catchments draining to the Great Barrier Reef (GBR). The research in GBR catchments has indicated that particulate nutrients are bioavailable to both freshwater and marine phytoplankton, but relative importance of this source of nutrients to the GBR is unknown. We quantified the contribution of this source of bioavailable nitrogen in a dry-tropics grazing and a wet-tropics fertilized mixed land use catchment of the GBR. Materials and methods The different bioavailable nitrogen pools and associated processes through which dissolved inorganic nitrogen (DIN) is generated from eroded sediment (mass of DIN generated per mass of sediment) were identified. These pools and processes were quantified from a range of representative sediment sources (e.g. surface and subsurface soil and different land uses). We collected 17 sediment source samples in the wet tropics and 41 in the dry tropics. We combined the N pool concentration data with spatial and hydrological fine sediment modelling to estimate the contribution from different sources and processes/pools to the end-of-catchment DIN load. Results and discussion The modelled load of DIN generated from sediment accounted for all the monitored DIN load in the grazing-dominated catchment but was insignificant in the fertilized mixed land use catchment. Sediment from surface erosion (hillslope erosion) and some soil types contributed disproportionally to the modelled DIN generation. Fast solubilisation of DIN was the main process in the catchments studied. The importance of mineralisation of the organic fraction increased with the time the sediment was in suspension. Conclusion Particulate nutrients in sediment are a significant source of bioavailable nitrogen in eroding grazing catchments. The processes that drive this bioavailability are complex, vary with sediment source and operate at different timeframes and spatial scales.
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The research in GBR catchments has indicated that particulate nutrients are bioavailable to both freshwater and marine phytoplankton, but relative importance of this source of nutrients to the GBR is unknown. We quantified the contribution of this source of bioavailable nitrogen in a dry-tropics grazing and a wet-tropics fertilized mixed land use catchment of the GBR. Materials and methods The different bioavailable nitrogen pools and associated processes through which dissolved inorganic nitrogen (DIN) is generated from eroded sediment (mass of DIN generated per mass of sediment) were identified. These pools and processes were quantified from a range of representative sediment sources (e.g. surface and subsurface soil and different land uses). We collected 17 sediment source samples in the wet tropics and 41 in the dry tropics. We combined the N pool concentration data with spatial and hydrological fine sediment modelling to estimate the contribution from different sources and processes/pools to the end-of-catchment DIN load. Results and discussion The modelled load of DIN generated from sediment accounted for all the monitored DIN load in the grazing-dominated catchment but was insignificant in the fertilized mixed land use catchment. Sediment from surface erosion (hillslope erosion) and some soil types contributed disproportionally to the modelled DIN generation. Fast solubilisation of DIN was the main process in the catchments studied. The importance of mineralisation of the organic fraction increased with the time the sediment was in suspension. Conclusion Particulate nutrients in sediment are a significant source of bioavailable nitrogen in eroding grazing catchments. The processes that drive this bioavailability are complex, vary with sediment source and operate at different timeframes and spatial scales.</description><identifier>ISSN: 1439-0108</identifier><identifier>EISSN: 1614-7480</identifier><identifier>DOI: 10.1007/s11368-024-03740-x</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Ammonium nitrogen ; Anthropogenic factors ; Barrier reefs ; Bioavailability ; Catchment area ; Catchments ; Earth and Environmental Science ; Environment ; Environmental Physics ; Freshwater ; Grazing ; Inland water environment ; Land use ; Mineralization ; Nitrogen ; Nutrient loading ; Nutrients ; Phytoplankton ; Sec 2 • Physical and Biogeochemical Processes • Research Article ; Sediment ; Sediment load ; Sediment samples ; Sediment sources ; Sediments ; Soil erosion ; Soil Science &amp; Conservation ; Soil types ; Soils ; Solubilization ; Tropical environments</subject><ispartof>Journal of soils and sediments, 2024-03, Vol.24 (3), p.1402-1419</ispartof><rights>The Author(s) 2024</rights><rights>The Author(s) 2024. 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The research in GBR catchments has indicated that particulate nutrients are bioavailable to both freshwater and marine phytoplankton, but relative importance of this source of nutrients to the GBR is unknown. We quantified the contribution of this source of bioavailable nitrogen in a dry-tropics grazing and a wet-tropics fertilized mixed land use catchment of the GBR. Materials and methods The different bioavailable nitrogen pools and associated processes through which dissolved inorganic nitrogen (DIN) is generated from eroded sediment (mass of DIN generated per mass of sediment) were identified. These pools and processes were quantified from a range of representative sediment sources (e.g. surface and subsurface soil and different land uses). We collected 17 sediment source samples in the wet tropics and 41 in the dry tropics. We combined the N pool concentration data with spatial and hydrological fine sediment modelling to estimate the contribution from different sources and processes/pools to the end-of-catchment DIN load. Results and discussion The modelled load of DIN generated from sediment accounted for all the monitored DIN load in the grazing-dominated catchment but was insignificant in the fertilized mixed land use catchment. Sediment from surface erosion (hillslope erosion) and some soil types contributed disproportionally to the modelled DIN generation. Fast solubilisation of DIN was the main process in the catchments studied. The importance of mineralisation of the organic fraction increased with the time the sediment was in suspension. Conclusion Particulate nutrients in sediment are a significant source of bioavailable nitrogen in eroding grazing catchments. 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Conservation</topic><topic>Soil types</topic><topic>Soils</topic><topic>Solubilization</topic><topic>Tropical environments</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Garzon-Garcia, Alexandra</creatorcontrib><creatorcontrib>Burton, Joanne M.</creatorcontrib><creatorcontrib>Ellis, Rob</creatorcontrib><creatorcontrib>Askildsen, Maria</creatorcontrib><creatorcontrib>Bloesch, Philip</creatorcontrib><creatorcontrib>De Hayr, Rob</creatorcontrib><creatorcontrib>Moody, Phil</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>Environment 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of soils and sediments</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Garzon-Garcia, Alexandra</au><au>Burton, Joanne M.</au><au>Ellis, Rob</au><au>Askildsen, Maria</au><au>Bloesch, Philip</au><au>De Hayr, Rob</au><au>Moody, Phil</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The bioavailability of particulate nitrogen in eroded sediment: Catchment sources and processes</atitle><jtitle>Journal of soils and sediments</jtitle><stitle>J Soils Sediments</stitle><date>2024-03-01</date><risdate>2024</risdate><volume>24</volume><issue>3</issue><spage>1402</spage><epage>1419</epage><pages>1402-1419</pages><issn>1439-0108</issn><eissn>1614-7480</eissn><abstract>Purpose Anthropogenic land use change has caused an increase in particulate nutrient loads from catchments draining to the Great Barrier Reef (GBR). The research in GBR catchments has indicated that particulate nutrients are bioavailable to both freshwater and marine phytoplankton, but relative importance of this source of nutrients to the GBR is unknown. We quantified the contribution of this source of bioavailable nitrogen in a dry-tropics grazing and a wet-tropics fertilized mixed land use catchment of the GBR. Materials and methods The different bioavailable nitrogen pools and associated processes through which dissolved inorganic nitrogen (DIN) is generated from eroded sediment (mass of DIN generated per mass of sediment) were identified. These pools and processes were quantified from a range of representative sediment sources (e.g. surface and subsurface soil and different land uses). We collected 17 sediment source samples in the wet tropics and 41 in the dry tropics. We combined the N pool concentration data with spatial and hydrological fine sediment modelling to estimate the contribution from different sources and processes/pools to the end-of-catchment DIN load. Results and discussion The modelled load of DIN generated from sediment accounted for all the monitored DIN load in the grazing-dominated catchment but was insignificant in the fertilized mixed land use catchment. Sediment from surface erosion (hillslope erosion) and some soil types contributed disproportionally to the modelled DIN generation. Fast solubilisation of DIN was the main process in the catchments studied. The importance of mineralisation of the organic fraction increased with the time the sediment was in suspension. Conclusion Particulate nutrients in sediment are a significant source of bioavailable nitrogen in eroding grazing catchments. 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subjects Ammonium nitrogen
Anthropogenic factors
Barrier reefs
Bioavailability
Catchment area
Catchments
Earth and Environmental Science
Environment
Environmental Physics
Freshwater
Grazing
Inland water environment
Land use
Mineralization
Nitrogen
Nutrient loading
Nutrients
Phytoplankton
Sec 2 • Physical and Biogeochemical Processes • Research Article
Sediment
Sediment load
Sediment samples
Sediment sources
Sediments
Soil erosion
Soil Science & Conservation
Soil types
Soils
Solubilization
Tropical environments
title The bioavailability of particulate nitrogen in eroded sediment: Catchment sources and processes
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