Modeling global annual N2O and NO emissions from fertilized fields
Identifieur interne : 000952 ( Istex/Corpus ); précédent : 000951; suivant : 000953Modeling global annual N2O and NO emissions from fertilized fields
Auteurs : A. F. Bouwman ; L. J. M. Boumans ; N. H. BatjesSource :
- Global Biogeochemical Cycles [ 0886-6236 ] ; 2002-12.
Abstract
Information from 846 N2O emission measurements in agricultural fields and 99 measurements for NO emissions was used to describe the influence of various factors regulating emissions from mineral soils in models for calculating global N2O and NO emissions. Only those factors having a significant influence on N2O and NO emissions were included in the models. For N2O these were (1) environmental factors (climate, soil organic C content, soil texture, drainage and soil pH); (2) management‐related factors (N application rate per fertilizer type, type of crop, with major differences between grass, legumes and other annual crops); and (3) factors related to the measurements (length of measurement period and frequency of measurements). The most important controls on NO emission include the N application rate per fertilizer type, soil organic‐C content and soil drainage. Calculated global annual N2O‐N and NO‐N emissions from fertilized agricultural fields amount to 2.8 and 1.6 Mtonne, respectively. The global mean fertilizer‐induced emissions for N2O and NO amount to 0.9% and 0.7%, respectively, of the N applied. These overall results account for the spatial variability of the main N2O and NO emission controls on the landscape scale.
Url:
DOI: 10.1029/2001GB001812
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ISTEX:9AE4674161EE80700375393FBAD5EA56B6EAE765Le document en format XML
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Only those factors having a significant influence on N2O and NO emissions were included in the models. For N2O these were (1) environmental factors (climate, soil organic C content, soil texture, drainage and soil pH); (2) management‐related factors (N application rate per fertilizer type, type of crop, with major differences between grass, legumes and other annual crops); and (3) factors related to the measurements (length of measurement period and frequency of measurements). The most important controls on NO emission include the N application rate per fertilizer type, soil organic‐C content and soil drainage. Calculated global annual N2O‐N and NO‐N emissions from fertilized agricultural fields amount to 2.8 and 1.6 Mtonne, respectively. The global mean fertilizer‐induced emissions for N2O and NO amount to 0.9% and 0.7%, respectively, of the N applied. These overall results account for the spatial variability of the main N2O and NO emission controls on the landscape scale.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>A. F. Bouwman</name><affiliations><json:string>National Institute for Public Health and the Environment (RIVM), Bilthoven, Netherlands</json:string></affiliations></json:item><json:item><name>L. J. M. Boumans</name><affiliations><json:string>National Institute for Public Health and the Environment (RIVM), Bilthoven, Netherlands</json:string></affiliations></json:item><json:item><name>N. H. 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Only those factors having a significant influence on N2O and NO emissions were included in the models. For N2O these were (1) environmental factors (climate, soil organic C content, soil texture, drainage and soil pH); (2) management‐related factors (N application rate per fertilizer type, type of crop, with major differences between grass, legumes and other annual crops); and (3) factors related to the measurements (length of measurement period and frequency of measurements). The most important controls on NO emission include the N application rate per fertilizer type, soil organic‐C content and soil drainage. Calculated global annual N2O‐N and NO‐N emissions from fertilized agricultural fields amount to 2.8 and 1.6 Mtonne, respectively. The global mean fertilizer‐induced emissions for N2O and NO amount to 0.9% and 0.7%, respectively, of the N applied. 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F.</givenNames></author>, <author><givenNames>L. J. M.</givenNames> <familyName>Boumans</familyName></author>, and <author><givenNames>N. H.</givenNames> <familyName>Batjes</familyName></author>, <articleTitle>Modeling global annual N<sub>2</sub>O and NO emissions from fertilized fields</articleTitle>, <journalTitle>Global Biogeochem. Cycles</journalTitle>, <vol>16</vol>(<issue>4</issue>), 1080, doi:<accessionId ref="info:doi/10.1029/2001GB001812">10.1029/2001GB001812</accessionId>, <pubYear year="2002">2002</pubYear>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:GBC.GBC807.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="2"></count><count type="tableTotal" number="3"></count></countGroup><titleGroup><title type="main">Modeling global annual N<sub>2</sub>O and NO emissions from fertilized fields</title><title type="short">N<sub>2</sub>O AND NO EMISSIONS FROM FERTILIZERS</title><title type="shortAuthors">Bouwman <i>et al</i>.</title></titleGroup><creators><creator creatorRole="author" xml:id="gbc807-cr-0001" affiliationRef="#gbc807-aff-0001"><personName><givenNames>A. F.</givenNames> <familyName>Bouwman</familyName></personName></creator><creator creatorRole="author" xml:id="gbc807-cr-0002" affiliationRef="#gbc807-aff-0001"><personName><givenNames>L. J. M.</givenNames> <familyName>Boumans</familyName></personName></creator><creator creatorRole="author" xml:id="gbc807-cr-0003" affiliationRef="#gbc807-aff-0002"><personName><givenNames>N. H.</givenNames> <familyName>Batjes</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="NL" type="organization" xml:id="gbc807-aff-0001"><orgName>National Institute for Public Health and the Environment (RIVM)</orgName><address><city>Bilthoven</city><country>Netherlands</country></address></affiliation><affiliation countryCode="NL" type="organization" xml:id="gbc807-aff-0002"><orgName>International Soil Reference and Information Centre (ISRIC)</orgName><address><city>Wageningen</city><country>Netherlands</country></address></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="gbc807-kwd-0001">animal manure</keyword><keyword xml:id="gbc807-kwd-0002">gas emission</keyword><keyword xml:id="gbc807-kwd-0003">fertilizer</keyword><keyword xml:id="gbc807-kwd-0004">global model</keyword><keyword xml:id="gbc807-kwd-0005">nitric oxide (NO)</keyword><keyword xml:id="gbc807-kwd-0006">nitrous oxide (N<sub>2</sub>O)</keyword></keywordGroup><supportingInformation></supportingInformation><abstractGroup><abstract type="main"><p xml:id="gbc807-para-0001" label="1">Information from 846 N<sub>2</sub>O emission measurements in agricultural fields and 99 measurements for NO emissions was used to describe the influence of various factors regulating emissions from mineral soils in models for calculating global N<sub>2</sub>O and NO emissions. Only those factors having a significant influence on N<sub>2</sub>O and NO emissions were included in the models. For N<sub>2</sub>O these were (1) environmental factors (climate, soil organic C content, soil texture, drainage and soil pH); (2) management‐related factors (N application rate per fertilizer type, type of crop, with major differences between grass, legumes and other annual crops); and (3) factors related to the measurements (length of measurement period and frequency of measurements). The most important controls on NO emission include the N application rate per fertilizer type, soil organic‐C content and soil drainage. Calculated global annual N<sub>2</sub>O‐N and NO‐N emissions from fertilized agricultural fields amount to 2.8 and 1.6 Mtonne, respectively. The global mean fertilizer‐induced emissions for N<sub>2</sub>O and NO amount to 0.9% and 0.7%, respectively, of the N applied. These overall results account for the spatial variability of the main N<sub>2</sub>O and NO emission controls on the landscape scale.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Modeling global annual N2O and NO emissions from fertilized fields</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>N2O AND NO EMISSIONS FROM FERTILIZERS</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Modeling global annual N2O and NO emissions from fertilized fields</title></titleInfo><name type="personal"><namePart type="given">A. F.</namePart><namePart type="family">Bouwman</namePart><affiliation>National Institute for Public Health and the Environment (RIVM), Bilthoven, Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">L. J. M.</namePart><namePart type="family">Boumans</namePart><affiliation>National Institute for Public Health and the Environment (RIVM), Bilthoven, Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">N. H.</namePart><namePart type="family">Batjes</namePart><affiliation>International Soil Reference and Information Centre (ISRIC), Wageningen, Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2002-12</dateIssued><dateCaptured encoding="w3cdtf">2001-10-17</dateCaptured><dateValid encoding="w3cdtf">2002-09-06</dateValid><edition>Bouwman, A. F., L. J. M. Boumans, and N. H. Batjes, Modeling global annual N2O and NO emissions from fertilized fields, Global Biogeochem. Cycles, 16(4), 1080, doi:10.1029/2001GB001812, 2002.</edition><copyrightDate encoding="w3cdtf">2002</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">2</extent><extent unit="tables">3</extent></physicalDescription><abstract>Information from 846 N2O emission measurements in agricultural fields and 99 measurements for NO emissions was used to describe the influence of various factors regulating emissions from mineral soils in models for calculating global N2O and NO emissions. Only those factors having a significant influence on N2O and NO emissions were included in the models. For N2O these were (1) environmental factors (climate, soil organic C content, soil texture, drainage and soil pH); (2) management‐related factors (N application rate per fertilizer type, type of crop, with major differences between grass, legumes and other annual crops); and (3) factors related to the measurements (length of measurement period and frequency of measurements). The most important controls on NO emission include the N application rate per fertilizer type, soil organic‐C content and soil drainage. Calculated global annual N2O‐N and NO‐N emissions from fertilized agricultural fields amount to 2.8 and 1.6 Mtonne, respectively. The global mean fertilizer‐induced emissions for N2O and NO amount to 0.9% and 0.7%, respectively, of the N applied. These overall results account for the spatial variability of the main N2O and NO emission controls on the landscape scale.</abstract><subject><genre>keywords</genre><topic>animal manure</topic><topic>gas emission</topic><topic>fertilizer</topic><topic>global model</topic><topic>nitric oxide (NO)</topic><topic>nitrous oxide (N2O)</topic></subject><relatedItem type="host"><titleInfo><title>Global Biogeochemical Cycles</title></titleInfo><titleInfo type="abbreviated"><title>Global Biogeochem. Cycles</title></titleInfo><genre type="journal">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0365">Troposphere: composition and chemistry</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0315">Biosphere/atmosphere interactions</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0325">Evolution of the atmosphere</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0412">Biogeochemical kinetics and reaction modeling</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0414">Biogeochemical cycles, processes, and modeling</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0793">Biogeochemistry</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1610">Atmosphere</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1615">Biogeochemical cycles, processes, and modeling</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4805">Biogeochemical cycles, processes, and modeling</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4900">PALEOCEANOGRAPHY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4912">Biogeochemical cycles, processes, and modeling</topic></subject><identifier type="ISSN">0886-6236</identifier><identifier type="eISSN">1944-9224</identifier><identifier type="DOI">10.1002/(ISSN)1944-9224</identifier><identifier type="CODEN">GBCYEP</identifier><identifier type="PublisherID">GBC</identifier><part><date>2002</date><detail type="volume"><caption>vol.</caption><number>16</number></detail><detail type="issue"><caption>no.</caption><number>4</number></detail><extent unit="pages"><start>28-1</start><end>28-9</end><total>9</total></extent></part></relatedItem><identifier type="istex">9AE4674161EE80700375393FBAD5EA56B6EAE765</identifier><identifier type="DOI">10.1029/2001GB001812</identifier><identifier type="ArticleID">2001GB001812</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2002 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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