Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget
Identifieur interne : 000437 ( Istex/Corpus ); précédent : 000436; suivant : 000438Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget
Auteurs : I. D. L. Foster ; I. C. GrieveSource :
- Earth Surface Processes and Landforms [ 0197-9337 ] ; 1982-09.
English descriptors
Abstract
Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.
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DOI: 10.1002/esp.3290070503
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D. L." last="Foster">I. D. L. Foster</name><affiliation><mods:affiliation>Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB. U.K.</mods:affiliation></affiliation></author><author><name sortKey="Grieve, I C" sort="Grieve, I C" uniqKey="Grieve I" first="I. C." last="Grieve">I. C. Grieve</name><affiliation><mods:affiliation>Department of Earth and Environmental Science, University of Stirling, Stirling, FK9 4AL, U.K.</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Earth Surface Processes and Landforms</title><title level="j" type="abbrev">Earth Surf. Process. Landforms</title><idno type="ISSN">0197-9337</idno><idno type="eISSN">1096-9837</idno><imprint><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Sussex</pubPlace><date type="published" when="1982-09">1982-09</date><biblScope unit="volume">7</biblScope><biblScope unit="issue">5</biblScope><biblScope unit="page" from="417">417</biblScope><biblScope unit="page" to="425">425</biblScope></imprint><idno type="ISSN">0197-9337</idno></series><idno type="istex">9732791CAA233B8BF87ADB8617CD420DC89FE631</idno><idno type="DOI">10.1002/esp.3290070503</idno><idno type="ArticleID">ESP3290070503</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0197-9337</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Dissolved organic matter</term><term>Dry spell</term><term>Mineralization</term><term>Nutrient cycling</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>I. D. L. Foster</name><affiliations><json:string>Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB. U.K.</json:string></affiliations></json:item><json:item><name>I. C. Grieve</name><affiliations><json:string>Department of Earth and Environmental Science, University of Stirling, Stirling, FK9 4AL, U.K.</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>Dissolved organic matter</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Dry spell</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Mineralization</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Nutrient cycling</value></json:item></subject><articleId><json:string>ESP3290070503</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.</abstract><qualityIndicators><score>4.924</score><pdfVersion>1.3</pdfVersion><pdfPageSize>576 x 738 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>658</abstractCharCount><pdfWordCount>3736</pdfWordCount><pdfCharCount>20944</pdfCharCount><pdfPageCount>9</pdfPageCount><abstractWordCount>99</abstractWordCount></qualityIndicators><title>Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget</title><refBibs><json:item><author><json:item><name>R. R. Arnett</name></json:item></author><host><volume>29</volume><pages><last>179</last><first>169</first></pages><author></author><title>Zeits. für Geomorph., Suppl.</title></host><title>Regional disparities in the denudation rate of organic sediments</title></json:item><json:item><author><json:item><name>C. D. 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D. L.</forename><surname>Foster</surname></persName><affiliation>Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB. U.K.</affiliation></author><author xml:id="author-2"><persName><forename type="first">I. C.</forename><surname>Grieve</surname></persName><affiliation>Department of Earth and Environmental Science, University of Stirling, Stirling, FK9 4AL, U.K.</affiliation></author></analytic><monogr><title level="j">Earth Surface Processes and Landforms</title><title level="j" type="abbrev">Earth Surf. Process. Landforms</title><idno type="pISSN">0197-9337</idno><idno type="eISSN">1096-9837</idno><idno type="DOI">10.1002/(ISSN)1096-9837</idno><imprint><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Sussex</pubPlace><date type="published" when="1982-09"></date><biblScope unit="volume">7</biblScope><biblScope unit="issue">5</biblScope><biblScope unit="page" from="417">417</biblScope><biblScope unit="page" to="425">425</biblScope></imprint></monogr><idno type="istex">9732791CAA233B8BF87ADB8617CD420DC89FE631</idno><idno type="DOI">10.1002/esp.3290070503</idno><idno type="ArticleID">ESP3290070503</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1982</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>Dissolved organic matter</term></item><item><term>Dry spell</term></item><item><term>Mineralization</term></item><item><term>Nutrient cycling</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Article</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1980-12">Received</change><change when="1982-09">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/9732791CAA233B8BF87ADB8617CD420DC89FE631/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>John Wiley & Sons, Ltd</publisherName><publisherLoc>Sussex</publisherLoc></publisherInfo><doi registered="yes">10.1002/(ISSN)1096-9837</doi><issn type="print">0197-9337</issn><issn type="electronic">1096-9837</issn><idGroup><id type="product" value="ESP"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="EARTH SURFACE PROCESSES AND LANDFORMS">Earth Surface Processes and Landforms</title><title type="short">Earth Surf. 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D. L.</givenNames><familyName>Foster</familyName></personName></creator><creator xml:id="au2" creatorRole="author" affiliationRef="#af2"><personName><givenNames>I. C.</givenNames><familyName>Grieve</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="GB" type="organization"><unparsedAffiliation>Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB. U.K.</unparsedAffiliation></affiliation><affiliation xml:id="af2" countryCode="GB" type="organization"><unparsedAffiliation>Department of Earth and Environmental Science, University of Stirling, Stirling, FK9 4AL, U.K.</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en" type="author"><keyword xml:id="kwd1">Dissolved organic matter</keyword><keyword xml:id="kwd2">Dry spell</keyword><keyword xml:id="kwd3">Mineralization</keyword><keyword xml:id="kwd4">Nutrient cycling</keyword></keywordGroup><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>DISSOLVED ORGANIC MATTER FLUCTUATIONS</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget</title></titleInfo><name type="personal"><namePart type="given">I. D. L.</namePart><namePart type="family">Foster</namePart><affiliation>Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB. U.K.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">I. C.</namePart><namePart type="family">Grieve</namePart><affiliation>Department of Earth and Environmental Science, University of Stirling, Stirling, FK9 4AL, U.K.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd</publisher><place><placeTerm type="text">Sussex</placeTerm></place><dateIssued encoding="w3cdtf">1982-09</dateIssued><dateCaptured encoding="w3cdtf">1980-12</dateCaptured><copyrightDate encoding="w3cdtf">1982</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">4</extent><extent unit="tables">2</extent><extent unit="references">21</extent></physicalDescription><abstract lang="en">Dissolved organic matter (DOM) concentrations in throughfall, throughflow, and runoff were recorded in a small (95 ha) woodland catchment in North Warwickshire for a period of eight weeks following a prolonged dry spell. DOM is shown to be positively related to stream discharge over the sampling period, although distinctive flushing effects were identified. The net contribution of DOM to total dissolved solids load carried in the river was only 2.4 per cent, and represented significantly less than published carbon losses by mineralization of soil organic matter. Throughfall inputs were some 100 times higher than streamflow outputs from the catchment.</abstract><subject lang="en"><genre>keywords</genre><topic>Dissolved organic matter</topic><topic>Dry spell</topic><topic>Mineralization</topic><topic>Nutrient cycling</topic></subject><relatedItem type="host"><titleInfo><title>Earth Surface Processes and Landforms</title></titleInfo><titleInfo type="abbreviated"><title>Earth Surf. Process. 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|texte= Short term fluctuations in dissolved organic matter concentrations in streamflow draining a forested watershed and their relation to the catchment budget
}}
| This area was generated with Dilib version V0.6.27. |  |