A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications
Identifieur interne : 000174 ( Istex/Corpus ); précédent : 000173; suivant : 000175A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications
Auteurs : Changsheng Li ; Steve Frolking ; Tod A. FrolkingSource :
- Journal of Geophysical Research: Atmospheres [ 0148-0227 ] ; 1992-06-20.
Abstract
Simulations of nitrous oxide (N2O) and carbon dioxide (CO2) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). Model simulations were compared with five field studies: a 1‐month denitrification study of a fertilized grassland in England; a 2‐month study of N2O emissions from a native and fertilized grassland in Colorado; a 1‐year study of N2O emissions from agricultural fields on drained, organic soils in Florida; a 1‐year study of CO2 emissions from a grassland in Germany; and a 1‐year study of CO2 emissions from a cultivated agricultural site in Missouri. The trends and magnitude of simulated N2O (or N2O + N2) and CO2 emissions were consistent with the results obtained in field experiments. The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.
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DOI: 10.1029/92JD00510
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Frolking</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:032CD2F7FC2F129552744712598FC027F2775A26</idno><date when="1992" year="1992">1992</date><idno type="doi">10.1029/92JD00510</idno><idno type="url">https://api.istex.fr/document/032CD2F7FC2F129552744712598FC027F2775A26/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000174</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000174</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications</title><author wicri:is="90%"><name sortKey="Li, Changsheng" sort="Li, Changsheng" uniqKey="Li C" first="Changsheng" last="Li">Changsheng Li</name></author><author wicri:is="90%"><name sortKey="Frolking, Steve" sort="Frolking, Steve" uniqKey="Frolking S" first="Steve" last="Frolking">Steve Frolking</name></author><author wicri:is="90%"><name sortKey="Frolking, Tod A" sort="Frolking, Tod A" uniqKey="Frolking T" first="Tod A." last="Frolking">Tod A. Frolking</name></author></analytic><monogr></monogr><series><title level="j">Journal of Geophysical Research: Atmospheres</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="ISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="1992-06-20">1992-06-20</date><biblScope unit="volume">97</biblScope><biblScope unit="issue">D9</biblScope><biblScope unit="page" from="9777">9777</biblScope><biblScope unit="page" to="9783">9783</biblScope></imprint><idno type="ISSN">0148-0227</idno></series><idno type="istex">032CD2F7FC2F129552744712598FC027F2775A26</idno><idno type="DOI">10.1029/92JD00510</idno><idno type="ArticleID">92JD00510</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Simulations of nitrous oxide (N2O) and carbon dioxide (CO2) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). Model simulations were compared with five field studies: a 1‐month denitrification study of a fertilized grassland in England; a 2‐month study of N2O emissions from a native and fertilized grassland in Colorado; a 1‐year study of N2O emissions from agricultural fields on drained, organic soils in Florida; a 1‐year study of CO2 emissions from a grassland in Germany; and a 1‐year study of CO2 emissions from a cultivated agricultural site in Missouri. The trends and magnitude of simulated N2O (or N2O + N2) and CO2 emissions were consistent with the results obtained in field experiments. The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Changsheng Li</name></json:item><json:item><name>Steve Frolking</name></json:item><json:item><name>Tod A. Frolking</name></json:item></author><articleId><json:string>92JD00510</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Simulations of nitrous oxide (N2O) and carbon dioxide (CO2) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). 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The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.</abstract><qualityIndicators><score>4.676</score><pdfVersion>1.2</pdfVersion><pdfPageSize>601 x 815 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1054</abstractCharCount><pdfWordCount>2660</pdfWordCount><pdfCharCount>25556</pdfCharCount><pdfPageCount>7</pdfPageCount><abstractWordCount>168</abstractWordCount></qualityIndicators><title>A model of nitrous oxide evolution from soil driven by rainfall events: 2. 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Res.</title><idno type="pISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><idno type="DOI">10.1002/(ISSN)2156-2202d</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="1992-06-20"></date><biblScope unit="volume">97</biblScope><biblScope unit="issue">D9</biblScope><biblScope unit="page" from="9777">9777</biblScope><biblScope unit="page" to="9783">9783</biblScope></imprint></monogr><idno type="istex">032CD2F7FC2F129552744712598FC027F2775A26</idno><idno type="DOI">10.1029/92JD00510</idno><idno type="ArticleID">92JD00510</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1992</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>Simulations of nitrous oxide (N2O) and carbon dioxide (CO2) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). Model simulations were compared with five field studies: a 1‐month denitrification study of a fertilized grassland in England; a 2‐month study of N2O emissions from a native and fertilized grassland in Colorado; a 1‐year study of N2O emissions from agricultural fields on drained, organic soils in Florida; a 1‐year study of CO2 emissions from a grassland in Germany; and a 1‐year study of CO2 emissions from a cultivated agricultural site in Missouri. The trends and magnitude of simulated N2O (or N2O + N2) and CO2 emissions were consistent with the results obtained in field experiments. The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>ATMOSPHERIC COMPOSITION AND STRUCTURE</term></item><item><term>Biosphere/atmosphere interactions</term></item><item><term>Geochemical cycles</term></item><item><term>BIOGEOSCIENCES</term></item><item><term>Biosphere/atmosphere interactions</term></item><item><term>GEOCHEMISTRY</term></item><item><term>Geochemical cycles</term></item><item><term>GLOBAL CHANGE</term></item><item><term>Atmosphere</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1991-07-16">Received</change><change when="1992-02-27">Registration</change><change when="1992-06-20">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/032CD2F7FC2F129552744712598FC027F2775A26/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 type="serialArticle" version="2.0" xml:lang="en" xml:id="jgrd2245"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2156-2202d</doi><issn type="print">0148-0227</issn><issn type="electronic">2156-2202</issn><idGroup><id type="product" value="JGRD"></id><id type="coden" value="JGREA2"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES">Journal of Geophysical Research: Atmospheres</title><title type="short">J. 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A.</givenNames> <familyName>Frolking</familyName></author> (<pubYear year="1992">1992</pubYear>), <articleTitle>A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications</articleTitle>, <journalTitle>J. Geophys. Res.</journalTitle>, <vol>97</vol>(<issue>D9</issue>), <pageFirst>9777</pageFirst>–<pageLast>9783</pageLast>, doi:<accessionId ref="info:doi/10.1029/92JD00510">10.1029/92JD00510</accessionId>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:JGRD.JGRD2245.pdf"></link></linkGroup></publicationMeta><contentMeta><titleGroup><title type="main">A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications</title><title type="shortAuthors">Li ET AL.</title></titleGroup><creators><creator xml:id="jgrd2245-cr-0001"><personName><givenNames>Changsheng</givenNames><familyName>Li</familyName></personName></creator><creator xml:id="jgrd2245-cr-0002"><personName><givenNames>Steve</givenNames><familyName>Frolking</familyName></personName></creator><creator xml:id="jgrd2245-cr-0003"><personName><givenNames>Tod A.</givenNames><familyName>Frolking</familyName></personName></creator></creators><abstractGroup><abstract type="main"><p xml:id="jgrd2245-para-0001">Simulations of nitrous oxide (N<sub>2</sub>O) and carbon dioxide (CO<sub>2</sub>) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). Model simulations were compared with five field studies: a 1‐month denitrification study of a fertilized grassland in England; a 2‐month study of N<sub>2</sub>O emissions from a native and fertilized grassland in Colorado; a 1‐year study of N<sub>2</sub>O emissions from agricultural fields on drained, organic soils in Florida; a 1‐year study of CO<sub>2</sub> emissions from a grassland in Germany; and a 1‐year study of CO<sub>2</sub> emissions from a cultivated agricultural site in Missouri. The trends and magnitude of simulated N<sub>2</sub>O (or N<sub>2</sub>O + N<sub>2</sub>) and CO<sub>2</sub> emissions were consistent with the results obtained in field experiments. The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications</title></titleInfo><name type="personal"><namePart type="given">Changsheng</namePart><namePart type="family">Li</namePart></name><name type="personal"><namePart type="given">Steve</namePart><namePart type="family">Frolking</namePart></name><name type="personal"><namePart type="given">Tod A.</namePart><namePart type="family">Frolking</namePart></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">1992-06-20</dateIssued><dateCaptured encoding="w3cdtf">1991-07-16</dateCaptured><dateValid encoding="w3cdtf">1992-02-27</dateValid><edition>Li, C., S. Frolking, and T. A. Frolking (1992), A model of nitrous oxide evolution from soil driven by rainfall events: 2. Model applications, J. Geophys. Res., 97(D9), 9777–9783, doi:10.1029/92JD00510.</edition><copyrightDate encoding="w3cdtf">1992</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract>Simulations of nitrous oxide (N2O) and carbon dioxide (CO2) emissions from soils were carried out with a rain‐event model of nitrogen and carbon cycling processes in soils (Li et al., this issue). Model simulations were compared with five field studies: a 1‐month denitrification study of a fertilized grassland in England; a 2‐month study of N2O emissions from a native and fertilized grassland in Colorado; a 1‐year study of N2O emissions from agricultural fields on drained, organic soils in Florida; a 1‐year study of CO2 emissions from a grassland in Germany; and a 1‐year study of CO2 emissions from a cultivated agricultural site in Missouri. The trends and magnitude of simulated N2O (or N2O + N2) and CO2 emissions were consistent with the results obtained in field experiments. The successful simulation of nitrous oxide and carbon dioxide emissions from the wide range of soil types studied indicates that the model, DNDC, will be a useful tool for studying linkages among climate, land use, soil‐atmosphere interactions, and trace gas fluxes.</abstract><relatedItem type="host"><titleInfo><title>Journal of Geophysical Research: Atmospheres</title></titleInfo><titleInfo type="abbreviated"><title>J. Geophys. 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