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Nitrogen retention, removal, and saturation in lotic ecosystems
Increased nitrogen (N) loading to lotic ecosystems may cause fundamental changes in the ability of streams and rivers to retain or remove N due to the potential for N saturation. Lotic ecosystems will saturate with sustained increases in the N load, but it is unclear at what point saturation will oc...
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Published in: | Ecosystems (New York) 2005-06, Vol.8 (4), p.442-453 |
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creator | Bernot, M.J Dodds, W.K |
description | Increased nitrogen (N) loading to lotic ecosystems may cause fundamental changes in the ability of streams and rivers to retain or remove N due to the potential for N saturation. Lotic ecosystems will saturate with sustained increases in the N load, but it is unclear at what point saturation will occur. Rates of N transformation in lotic ecosystems will vary depending on the total N load and whether it is an acute or chronic N load. Nitrogen saturation may not occur with only pulsed or short-term increases in N. Overall, saturation of microbial uptake will occur prior to saturation of denitrification of N and denitrification will become saturated prior to nitrification, exacerbating increases in nitrate concentrations and in N export downstream. The rate of N export to downstream ecosystems will increase proportionally to the N load once saturation occurs. Long term data sets showed that smaller lotic ecosystems have a greater capacity to remove in-stream N loads, relative to larger systems. Thus, denitrification is likely to become less important as a N loss mechanism as the stream size increases. There is a great need for long-term studies of N additions in lotic ecosystems and clear distinctions need to be made between ecosystem responses to short-term or periodic increases in N loading and alterations in ecosystem functions due to chronic N loading.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1007/s10021-003-0143-y |
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Lotic ecosystems will saturate with sustained increases in the N load, but it is unclear at what point saturation will occur. Rates of N transformation in lotic ecosystems will vary depending on the total N load and whether it is an acute or chronic N load. Nitrogen saturation may not occur with only pulsed or short-term increases in N. Overall, saturation of microbial uptake will occur prior to saturation of denitrification of N and denitrification will become saturated prior to nitrification, exacerbating increases in nitrate concentrations and in N export downstream. The rate of N export to downstream ecosystems will increase proportionally to the N load once saturation occurs. Long term data sets showed that smaller lotic ecosystems have a greater capacity to remove in-stream N loads, relative to larger systems. Thus, denitrification is likely to become less important as a N loss mechanism as the stream size increases. There is a great need for long-term studies of N additions in lotic ecosystems and clear distinctions need to be made between ecosystem responses to short-term or periodic increases in N loading and alterations in ecosystem functions due to chronic N loading.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1432-9840</identifier><identifier>EISSN: 1435-0629</identifier><identifier>DOI: 10.1007/s10021-003-0143-y</identifier><language>eng</language><publisher>New York, NY: Springer</publisher><subject>adsorption ; Animal and plant ecology ; Animal, plant and microbial ecology ; biogeochemical cycles ; Biological and medical sciences ; Denitrification ; denitrifying microorganisms ; Downstream ; Ecological function ; Ecosystems ; Fresh water ecosystems ; Fundamental and applied biological sciences. 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Lotic ecosystems will saturate with sustained increases in the N load, but it is unclear at what point saturation will occur. Rates of N transformation in lotic ecosystems will vary depending on the total N load and whether it is an acute or chronic N load. Nitrogen saturation may not occur with only pulsed or short-term increases in N. Overall, saturation of microbial uptake will occur prior to saturation of denitrification of N and denitrification will become saturated prior to nitrification, exacerbating increases in nitrate concentrations and in N export downstream. The rate of N export to downstream ecosystems will increase proportionally to the N load once saturation occurs. Long term data sets showed that smaller lotic ecosystems have a greater capacity to remove in-stream N loads, relative to larger systems. Thus, denitrification is likely to become less important as a N loss mechanism as the stream size increases. There is a great need for long-term studies of N additions in lotic ecosystems and clear distinctions need to be made between ecosystem responses to short-term or periodic increases in N loading and alterations in ecosystem functions due to chronic N loading.[PUBLICATION ABSTRACT]</description><subject>adsorption</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>biogeochemical cycles</subject><subject>Biological and medical sciences</subject><subject>Denitrification</subject><subject>denitrifying microorganisms</subject><subject>Downstream</subject><subject>Ecological function</subject><subject>Ecosystems</subject><subject>Fresh water ecosystems</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General aspects</subject><subject>limnology</subject><subject>Load</subject><subject>Load distribution</subject><subject>Nitrification</subject><subject>Nitrogen</subject><subject>nutrient uptake</subject><subject>pollution load</subject><subject>rivers</subject><subject>Saturation</subject><subject>streams</subject><subject>Synecology</subject><subject>water pollution</subject><issn>1432-9840</issn><issn>1435-0629</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNpdkE1Lw0AQhoMoWKs_wJNB0FOjsx_Jbk8ixS8oetCel8l2t6Qk2bqbCPn3bo0geJkZmOd9mXmT5JzADQEQtyFWSjIAlgHhLBsOkknseQYFnR_-zDSbSw7HyUkIWwCSS84nyd1r1Xm3MW3qTWfarnLtLI6N-8J6lmK7TgN2vcf9Iq3atHZdpVOjXRhCZ5pwmhxZrIM5--3TZPX48LF4zpZvTy-L-2WmWS66THK7LuncAuU55BIZIlkzSYsCpBCWCc6sLJGWnGqUuYB8zjkvheSSCiiRTZPr0Xfn3WdvQqeaKmhT19ga1wdFBJOEcRLBy3_g1vW-jbcpwRgUQgoZITJC2rsQvLFq56sG_aAIqH2easxTxTzVPk81RM3VrzEGjbX12Ooq_AkFyCKeELmLkbPoFG58ZFbvFAgDEr8vWMG-AUN2fLw</recordid><startdate>20050601</startdate><enddate>20050601</enddate><creator>Bernot, M.J</creator><creator>Dodds, W.K</creator><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>HCIFZ</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7U6</scope></search><sort><creationdate>20050601</creationdate><title>Nitrogen retention, removal, and saturation in lotic ecosystems</title><author>Bernot, M.J ; Dodds, W.K</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c357t-84fdb29f0245058a3aa1d382660877f3743f8ba2b42ca857059444b7848270ba3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>adsorption</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>biogeochemical cycles</topic><topic>Biological and medical sciences</topic><topic>Denitrification</topic><topic>denitrifying microorganisms</topic><topic>Downstream</topic><topic>Ecological function</topic><topic>Ecosystems</topic><topic>Fresh water ecosystems</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General aspects</topic><topic>limnology</topic><topic>Load</topic><topic>Load distribution</topic><topic>Nitrification</topic><topic>Nitrogen</topic><topic>nutrient uptake</topic><topic>pollution load</topic><topic>rivers</topic><topic>Saturation</topic><topic>streams</topic><topic>Synecology</topic><topic>water pollution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bernot, M.J</creatorcontrib><creatorcontrib>Dodds, W.K</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Research Library</collection><collection>ProQuest Science Journals</collection><collection>Research Library (Corporate)</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><jtitle>Ecosystems (New York)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bernot, M.J</au><au>Dodds, W.K</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nitrogen retention, removal, and saturation in lotic ecosystems</atitle><jtitle>Ecosystems (New York)</jtitle><date>2005-06-01</date><risdate>2005</risdate><volume>8</volume><issue>4</issue><spage>442</spage><epage>453</epage><pages>442-453</pages><issn>1432-9840</issn><eissn>1435-0629</eissn><abstract>Increased nitrogen (N) loading to lotic ecosystems may cause fundamental changes in the ability of streams and rivers to retain or remove N due to the potential for N saturation. Lotic ecosystems will saturate with sustained increases in the N load, but it is unclear at what point saturation will occur. Rates of N transformation in lotic ecosystems will vary depending on the total N load and whether it is an acute or chronic N load. Nitrogen saturation may not occur with only pulsed or short-term increases in N. Overall, saturation of microbial uptake will occur prior to saturation of denitrification of N and denitrification will become saturated prior to nitrification, exacerbating increases in nitrate concentrations and in N export downstream. The rate of N export to downstream ecosystems will increase proportionally to the N load once saturation occurs. Long term data sets showed that smaller lotic ecosystems have a greater capacity to remove in-stream N loads, relative to larger systems. Thus, denitrification is likely to become less important as a N loss mechanism as the stream size increases. There is a great need for long-term studies of N additions in lotic ecosystems and clear distinctions need to be made between ecosystem responses to short-term or periodic increases in N loading and alterations in ecosystem functions due to chronic N loading.[PUBLICATION ABSTRACT]</abstract><cop>New York, NY</cop><pub>Springer</pub><doi>10.1007/s10021-003-0143-y</doi><tpages>12</tpages></addata></record> |
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subjects | adsorption Animal and plant ecology Animal, plant and microbial ecology biogeochemical cycles Biological and medical sciences Denitrification denitrifying microorganisms Downstream Ecological function Ecosystems Fresh water ecosystems Fundamental and applied biological sciences. Psychology General aspects limnology Load Load distribution Nitrification Nitrogen nutrient uptake pollution load rivers Saturation streams Synecology water pollution |
title | Nitrogen retention, removal, and saturation in lotic ecosystems |
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