Nutrient loading and macrophyte growth in Wilson Inlet, a bar-built southwestern Australian estuary
Identifieur interne : 000E39 ( Istex/Corpus ); précédent : 000E38; suivant : 000E40Nutrient loading and macrophyte growth in Wilson Inlet, a bar-built southwestern Australian estuary
Auteurs : R. J. Lukatelich ; N. J. Schofield ; A. J. MccombSource :
- Estuarine, Coastal and Shelf Science [ 0272-7714 ] ; 1987.
Abstract
Wilson Inlet is a ‘bar-built’ estuary, open to the ocean only when a sandbar has been breached after river flow. estimates are presented of phosphorus and nitrogen loadings from rivers, losses to the ocean, and amounts present in estuarine components during a particular year. Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%). Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of Ruppia megacarpa Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass. Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. These are in higher rainfall areas, have high drainage densities, large proportions of sandy soils and are subjected to phosphatic fertilizer application.
Url:
DOI: 10.1016/0272-7714(87)90062-X
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Lukatelich</name><affiliation><mods:affiliation>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</mods:affiliation></affiliation></author><author><name sortKey="Schofield, N J" sort="Schofield, N J" uniqKey="Schofield N" first="N. J." last="Schofield">N. J. Schofield</name><affiliation><mods:affiliation>Hydrology Branch, Water Authority of Western Australia, Leederville, Western Australia 6007 Australia</mods:affiliation></affiliation></author><author><name sortKey="Mccomb, A J" sort="Mccomb, A J" uniqKey="Mccomb A" first="A. J." last="Mccomb">A. J. Mccomb</name><affiliation><mods:affiliation>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Estuarine, Coastal and Shelf Science</title><title level="j" type="abbrev">YECSS</title><idno type="ISSN">0272-7714</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1987">1987</date><biblScope unit="volume">24</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="141">141</biblScope><biblScope unit="page" to="165">165</biblScope></imprint><idno type="ISSN">0272-7714</idno></series><idno type="istex">3858AF1B7FB2803157224C05A0C3524E1DF57D15</idno><idno type="DOI">10.1016/0272-7714(87)90062-X</idno><idno type="PII">0272-7714(87)90062-X</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0272-7714</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Wilson Inlet is a ‘bar-built’ estuary, open to the ocean only when a sandbar has been breached after river flow. estimates are presented of phosphorus and nitrogen loadings from rivers, losses to the ocean, and amounts present in estuarine components during a particular year. Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%). Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of Ruppia megacarpa Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass. Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. These are in higher rainfall areas, have high drainage densities, large proportions of sandy soils and are subjected to phosphatic fertilizer application.</div></front></TEI><istex><corpusName>elsevier</corpusName><author><json:item><name>R.J. Lukatelich</name><affiliations><json:string>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</json:string></affiliations></json:item><json:item><name>N.J. Schofield</name><affiliations><json:string>Hydrology Branch, Water Authority of Western Australia, Leederville, Western Australia 6007 Australia</json:string></affiliations></json:item><json:item><name>A.J. 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Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%). Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of Ruppia megacarpa Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass. Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. 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Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%). Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of Ruppia megacarpa Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass. Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. These are in higher rainfall areas, have high drainage densities, large proportions of sandy soils and are subjected to phosphatic fertilizer application.</p></abstract><textClass><keywords scheme="keyword"><list><head>Keywords</head><item><term>estuaries</term></item><item><term>eutrophication</term></item><item><term>nitrogen</term></item><item><term>phosphorus</term></item><item><term>river discharges</term></item><item><term>seagrasses</term></item><item><term>Western Australia</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1986-02-05">Modified</change><change when="1987">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/3858AF1B7FB2803157224C05A0C3524E1DF57D15/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>YECSS</jid><aid>8790062X</aid><ce:pii>0272-7714(87)90062-X</ce:pii><ce:doi>10.1016/0272-7714(87)90062-X</ce:doi><ce:copyright type="unknown" year="1987"></ce:copyright></item-info><head><ce:title>Nutrient loading and macrophyte growth in Wilson Inlet, a bar-built southwestern Australian estuary</ce:title><ce:author-group><ce:author><ce:given-name>R.J.</ce:given-name><ce:surname>Lukatelich</ce:surname><ce:cross-ref refid="AFF1"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>N.J.</ce:given-name><ce:surname>Schofield</ce:surname><ce:cross-ref refid="AFF2"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>A.J.</ce:given-name><ce:surname>McComb</ce:surname><ce:cross-ref refid="AFF1"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="AFF1"><ce:label>a</ce:label><ce:textfn>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</ce:textfn></ce:affiliation><ce:affiliation id="AFF2"><ce:label>b</ce:label><ce:textfn>Hydrology Branch, Water Authority of Western Australia, Leederville, Western Australia 6007 Australia</ce:textfn></ce:affiliation></ce:author-group><ce:date-received day="21" month="6" year="1984"></ce:date-received><ce:date-revised day="5" month="2" year="1986"></ce:date-revised><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Wilson Inlet is a ‘bar-built’ estuary, open to the ocean only when a sandbar has been breached after river flow. estimates are presented of phosphorus and nitrogen loadings from rivers, losses to the ocean, and amounts present in estuarine components during a particular year. Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%).</ce:simple-para><ce:simple-para>Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of <ce:italic>Ruppia megacarpa</ce:italic> Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass.</ce:simple-para><ce:simple-para>Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. These are in higher rainfall areas, have high drainage densities, large proportions of sandy soils and are subjected to phosphatic fertilizer application.</ce:simple-para></ce:abstract-sec></ce:abstract><ce:keywords><ce:section-title>Keywords</ce:section-title><ce:keyword><ce:text>estuaries</ce:text></ce:keyword><ce:keyword><ce:text>eutrophication</ce:text></ce:keyword><ce:keyword><ce:text>nitrogen</ce:text></ce:keyword><ce:keyword><ce:text>phosphorus</ce:text></ce:keyword><ce:keyword><ce:text>river discharges</ce:text></ce:keyword><ce:keyword><ce:text>seagrasses</ce:text></ce:keyword><ce:keyword><ce:text>Western Australia</ce:text></ce:keyword></ce:keywords></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Nutrient loading and macrophyte growth in Wilson Inlet, a bar-built southwestern Australian estuary</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Nutrient loading and macrophyte growth in Wilson Inlet, a bar-built southwestern Australian estuary</title></titleInfo><name type="personal"><namePart type="given">R.J.</namePart><namePart type="family">Lukatelich</namePart><affiliation>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">N.J.</namePart><namePart type="family">Schofield</namePart><affiliation>Hydrology Branch, Water Authority of Western Australia, Leederville, Western Australia 6007 Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A.J.</namePart><namePart type="family">McComb</namePart><affiliation>Centre for Water Research, University of Western Australia, Nedlands, Western Australia 6009 Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article"></genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1987</dateIssued><dateModified encoding="w3cdtf">1986-02-05</dateModified><copyrightDate encoding="w3cdtf">1987</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Wilson Inlet is a ‘bar-built’ estuary, open to the ocean only when a sandbar has been breached after river flow. estimates are presented of phosphorus and nitrogen loadings from rivers, losses to the ocean, and amounts present in estuarine components during a particular year. Following bar opening, a volume of water equivalent to 35% of estuarine volume at the time was lost, providing a major loss of dissolved nutrients from the estuary. While the bar was open (51 days) water was displaced through river flow, but there was little tidal exchange. There was net retention of phosphorus (about 60% of river input) and some loss of nitrogen (less than 15%). Much of the nutrient held in the estuary was in surface sediments, but concentrations have shown little change with time and are similar to other southwestern estuaries. In contrast there have been massive increases in the biomass of Ruppia megacarpa Mason in recent years; this constitutes more than 90% of plant biomass. The nutrient bank in this plant is large compared to the water column, and amounts recycled through plant material greatly exceeded riverine loading in the year of the study. Tissue N concentrations were relatively high and constant, tissue P relatively low and seasonally variable, suggesting P limitation of plant biomass. Estimates of nutrient loading from streams showed relatively higher nutrient inputs from catchments cleared for agriculture. These are in higher rainfall areas, have high drainage densities, large proportions of sandy soils and are subjected to phosphatic fertilizer application.</abstract><subject><genre>Keywords</genre><topic>estuaries</topic><topic>eutrophication</topic><topic>nitrogen</topic><topic>phosphorus</topic><topic>river discharges</topic><topic>seagrasses</topic><topic>Western Australia</topic></subject><relatedItem type="host"><titleInfo><title>Estuarine, Coastal and Shelf Science</title></titleInfo><titleInfo type="abbreviated"><title>YECSS</title></titleInfo><genre type="journal">journal</genre><originInfo><dateIssued encoding="w3cdtf">198702</dateIssued></originInfo><identifier type="ISSN">0272-7714</identifier><identifier type="PII">S0272-7714(00)X0213-2</identifier><part><date>198702</date><detail type="volume"><number>24</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="issue pages"><start>141</start><end>288</end></extent><extent unit="pages"><start>141</start><end>165</end></extent></part></relatedItem><identifier type="istex">3858AF1B7FB2803157224C05A0C3524E1DF57D15</identifier><identifier type="DOI">10.1016/0272-7714(87)90062-X</identifier><identifier type="PII">0272-7714(87)90062-X</identifier><recordInfo><recordContentSource>ELSEVIER</recordContentSource></recordInfo></mods></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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