Emissions of volatile organic compounds from vegetation and the implications for atmospheric chemistry
Identifieur interne : 001624 ( Main/Exploration ); précédent : 001623; suivant : 001625Emissions 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
Affiliations:
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Nicholas Hewitt</name></author><author wicri:is="90%"><name sortKey="Lamb, Brian" sort="Lamb, Brian" uniqKey="Lamb B" first="Brian" last="Lamb">Brian Lamb</name></author><author wicri:is="90%"><name sortKey="Liu, Shaw" sort="Liu, Shaw" uniqKey="Liu S" first="Shaw" last="Liu">Shaw Liu</name></author><author wicri:is="90%"><name sortKey="Trainer, Michael" sort="Trainer, Michael" uniqKey="Trainer M" first="Michael" last="Trainer">Michael Trainer</name></author><author wicri:is="90%"><name sortKey="Westberg, Hal" sort="Westberg, Hal" uniqKey="Westberg H" first="Hal" last="Westberg">Hal Westberg</name></author><author wicri:is="90%"><name sortKey="Zimmerman, Pat" sort="Zimmerman, Pat" uniqKey="Zimmerman P" first="Pat" last="Zimmerman">Pat Zimmerman</name></author></analytic><monogr></monogr><series><title level="j">Global Biogeochemical Cycles</title><title level="j" type="abbrev">Global Biogeochem. Cycles</title><idno type="ISSN">0886-6236</idno><idno type="eISSN">1944-9224</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="1992-12">1992-12</date><biblScope unit="volume">6</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="389">389</biblScope><biblScope unit="page" to="430">430</biblScope></imprint><idno type="ISSN">0886-6236</idno></series><idno type="istex">09BD8E978FC9673C80DA059CD1F96444AD9BF8D6</idno><idno type="DOI">10.1029/92GB02125</idno><idno type="ArticleID">92GB02125</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0886-6236</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><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></front></TEI><affiliations><list></list><tree><noCountry><name sortKey="Calvert, Jack" sort="Calvert, Jack" uniqKey="Calvert J" first="Jack" last="Calvert">Jack Calvert</name><name sortKey="Fall, Ray" sort="Fall, Ray" uniqKey="Fall R" first="Ray" last="Fall">Ray Fall</name><name sortKey="Fehsenfeld, Fred" sort="Fehsenfeld, Fred" uniqKey="Fehsenfeld F" first="Fred" last="Fehsenfeld">Fred Fehsenfeld</name><name sortKey="Goldan, Paul" sort="Goldan, Paul" uniqKey="Goldan P" first="Paul" last="Goldan">Paul Goldan</name><name sortKey="Guenther, Alex B" sort="Guenther, Alex B" uniqKey="Guenther A" first="Alex B." last="Guenther">Alex B. Guenther</name><name sortKey="Hewitt, C Nicholas" sort="Hewitt, C Nicholas" uniqKey="Hewitt C" first="C. Nicholas" last="Hewitt">C. Nicholas Hewitt</name><name sortKey="Lamb, Brian" sort="Lamb, Brian" uniqKey="Lamb B" first="Brian" last="Lamb">Brian Lamb</name><name sortKey="Liu, Shaw" sort="Liu, Shaw" uniqKey="Liu S" first="Shaw" last="Liu">Shaw Liu</name><name sortKey="Trainer, Michael" sort="Trainer, Michael" uniqKey="Trainer M" first="Michael" last="Trainer">Michael Trainer</name><name sortKey="Westberg, Hal" sort="Westberg, Hal" uniqKey="Westberg H" first="Hal" last="Westberg">Hal Westberg</name><name sortKey="Zimmerman, Pat" sort="Zimmerman, Pat" uniqKey="Zimmerman P" first="Pat" last="Zimmerman">Pat Zimmerman</name></noCountry></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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