Emissions of volatile organic compounds from vegetation and the implications for atmospheric chemistry
Identifieur interne : 001496 ( Istex/Corpus ); précédent : 001495; suivant : 001497Emissions of volatile organic compounds from vegetation and the implications for atmospheric chemistry
Auteurs : Fred Fehsenfeld ; Jack Calvert ; Ray Fall ; Paul Goldan ; Alex B. Guenther ; C. Nicholas Hewitt ; Brian Lamb ; Shaw Liu ; Michael Trainer ; Hal Westberg ; Pat ZimmermanSource :
- Global Biogeochemical Cycles [ 0886-6236 ] ; 1992-12.
Abstract
Vegetation provides a major source of reactive carbon entering the atmosphere. These compounds play an important role in (1) shaping global tropospheric chemistry, (2) regional photochemical oxidant formation, (3) balancing the global carbon cycle, and (4) production of organic acids which contribute to acidic deposition in rural areas. Present estimates place the total annual global emission of these compounds between approximately 500 and 825 Tg yr−1. The volatile olefinic compounds, such as isoprene and the monoterpenes, are thought to constitute the bulk of these emissions. However, it is becoming increasingly clear that a variety of partially oxidized hydrocarbons, principally alcohols, are also emitted. The available information concerning the terrestrial vegetation as sources of volatile organic compounds is reviewed. The biochemical processes associated with these emissions of the compounds and the atmospheric chemistry of the emitted compounds are discussed.
Url:
DOI: 10.1029/92GB02125
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<front><div type="abstract">Vegetation provides a major source of reactive carbon entering the atmosphere. These compounds play an important role in (1) shaping global tropospheric chemistry, (2) regional photochemical oxidant formation, (3) balancing the global carbon cycle, and (4) production of organic acids which contribute to acidic deposition in rural areas. Present estimates place the total annual global emission of these compounds between approximately 500 and 825 Tg yr−1. The volatile olefinic compounds, such as isoprene and the monoterpenes, are thought to constitute the bulk of these emissions. However, it is becoming increasingly clear that a variety of partially oxidized hydrocarbons, principally alcohols, are also emitted. The available information concerning the terrestrial vegetation as sources of volatile organic compounds is reviewed. The biochemical processes associated with these emissions of the compounds and the atmospheric chemistry of the emitted compounds are discussed.</div>
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<edition>Fehsenfeld, F., et al. (1992), Emissions of volatile organic compounds from vegetation and the implications for atmospheric chemistry, Global Biogeochem. Cycles, 6(4), 389–430, doi:10.1029/92GB02125.</edition>
<copyrightDate encoding="w3cdtf">1992</copyrightDate>
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<language><languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
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<physicalDescription><internetMediaType>text/html</internetMediaType>
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<abstract>Vegetation provides a major source of reactive carbon entering the atmosphere. These compounds play an important role in (1) shaping global tropospheric chemistry, (2) regional photochemical oxidant formation, (3) balancing the global carbon cycle, and (4) production of organic acids which contribute to acidic deposition in rural areas. Present estimates place the total annual global emission of these compounds between approximately 500 and 825 Tg yr−1. The volatile olefinic compounds, such as isoprene and the monoterpenes, are thought to constitute the bulk of these emissions. However, it is becoming increasingly clear that a variety of partially oxidized hydrocarbons, principally alcohols, are also emitted. The available information concerning the terrestrial vegetation as sources of volatile organic compounds is reviewed. The biochemical processes associated with these emissions of the compounds and the atmospheric chemistry of the emitted compounds are discussed.</abstract>
<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/specialSection/NATSOUR1">Natural Sources of Acid Precursors, Neutralizing Compounds, and Oxidants</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0315">Biosphere/atmosphere interactions</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0365">Troposphere: composition and chemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0394">Instruments and techniques</topic>
</subject>
<subject><genre>article-category</genre>
<topic>Special Section: Natural Sources of Acid Precursors, Neutralizing Compounds, and Oxidants</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>1992</date>
<detail type="volume"><caption>vol.</caption>
<number>6</number>
</detail>
<detail type="issue"><caption>no.</caption>
<number>4</number>
</detail>
<extent unit="pages"><start>389</start>
<end>430</end>
<total>42</total>
</extent>
</part>
</relatedItem>
<identifier type="istex">09BD8E978FC9673C80DA059CD1F96444AD9BF8D6</identifier>
<identifier type="DOI">10.1029/92GB02125</identifier>
<identifier type="ArticleID">92GB02125</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 1992 by the American Geophysical Union.</accessCondition>
<recordInfo><recordContentSource>WILEY</recordContentSource>
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