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 |
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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. |
doi_str_mv | 10.1007/s11368-024-03740-x |
format | Article |
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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.</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 & 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. This work is published under http://creativecommons.org/licenses/by/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-c314t-4115aa658085d9d1e2a1e70b9bf1fbcfbf534de44bf2dc913fa5fafd93a8eacf3</cites><orcidid>0000-0002-6804-8890</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11368-024-03740-x$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11368-024-03740-x$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><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><title>The bioavailability of particulate nitrogen in eroded sediment: Catchment sources and processes</title><title>Journal of soils and sediments</title><addtitle>J Soils Sediments</addtitle><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.</description><subject>Ammonium nitrogen</subject><subject>Anthropogenic factors</subject><subject>Barrier reefs</subject><subject>Bioavailability</subject><subject>Catchment area</subject><subject>Catchments</subject><subject>Earth and Environmental Science</subject><subject>Environment</subject><subject>Environmental Physics</subject><subject>Freshwater</subject><subject>Grazing</subject><subject>Inland water environment</subject><subject>Land use</subject><subject>Mineralization</subject><subject>Nitrogen</subject><subject>Nutrient loading</subject><subject>Nutrients</subject><subject>Phytoplankton</subject><subject>Sec 2 • Physical and Biogeochemical Processes • Research Article</subject><subject>Sediment</subject><subject>Sediment load</subject><subject>Sediment samples</subject><subject>Sediment sources</subject><subject>Sediments</subject><subject>Soil erosion</subject><subject>Soil Science & Conservation</subject><subject>Soil types</subject><subject>Soils</subject><subject>Solubilization</subject><subject>Tropical environments</subject><issn>1439-0108</issn><issn>1614-7480</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kE9LAzEQxYMoWKtfwFPAczTZZHcTb1L8BwUv9RyyyaRNaXdrkkr99qau4M3TPJjfezM8hK4ZvWWUtneJMd5IQitBKG8FJYcTNGENE6QVkp4WLbgilFF5ji5SWtNClfUE6cUKcBcG82nCxnRhE_IXHjzemZiD3W9MBtyHHIcl9Dj0GOLgwOEELmyhz_d4ZrJdHSVOwz5aSNj0Du_iUGSCdInOvNkkuPqdU_T-9LiYvZD52_Pr7GFOLGciE8FYbUxTSyprpxyDyjBoaac6z3xnfedrLhwI0fnKWcW4N7U33iluJBjr-RTdjLnl8sceUtbr8k5fTupK1Y1qlJRNoaqRsnFIKYLXuxi2Jn5pRvWxSD0WqUuR-qdIfSgmPppSgfslxL_of1zfPex5iw</recordid><startdate>20240301</startdate><enddate>20240301</enddate><creator>Garzon-Garcia, Alexandra</creator><creator>Burton, Joanne M.</creator><creator>Ellis, Rob</creator><creator>Askildsen, Maria</creator><creator>Bloesch, Philip</creator><creator>De Hayr, Rob</creator><creator>Moody, Phil</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>H97</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-6804-8890</orcidid></search><sort><creationdate>20240301</creationdate><title>The bioavailability of particulate nitrogen in eroded sediment: Catchment sources and processes</title><author>Garzon-Garcia, Alexandra ; Burton, Joanne M. ; Ellis, Rob ; Askildsen, Maria ; Bloesch, Philip ; De Hayr, Rob ; Moody, Phil</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c314t-4115aa658085d9d1e2a1e70b9bf1fbcfbf534de44bf2dc913fa5fafd93a8eacf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Ammonium nitrogen</topic><topic>Anthropogenic factors</topic><topic>Barrier reefs</topic><topic>Bioavailability</topic><topic>Catchment area</topic><topic>Catchments</topic><topic>Earth and Environmental Science</topic><topic>Environment</topic><topic>Environmental Physics</topic><topic>Freshwater</topic><topic>Grazing</topic><topic>Inland water environment</topic><topic>Land use</topic><topic>Mineralization</topic><topic>Nitrogen</topic><topic>Nutrient loading</topic><topic>Nutrients</topic><topic>Phytoplankton</topic><topic>Sec 2 • Physical and Biogeochemical Processes • Research Article</topic><topic>Sediment</topic><topic>Sediment load</topic><topic>Sediment samples</topic><topic>Sediment sources</topic><topic>Sediments</topic><topic>Soil erosion</topic><topic>Soil Science & 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 & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & 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. The processes that drive this bioavailability are complex, vary with sediment source and operate at different timeframes and spatial scales.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11368-024-03740-x</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-6804-8890</orcidid><oa>free_for_read</oa></addata></record> |
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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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