[Soil respiration of degraded Korean pine forest ecosystem in Changbai Mountains].
Identifieur interne : 003100 ( Main/Curation ); précédent : 003099; suivant : 003101[Soil respiration of degraded Korean pine forest ecosystem in Changbai Mountains].
Auteurs : Yu Liang [République populaire de Chine] ; Jia-Wei Xu ; Yuan-Man Hu ; Yu Chang ; Ren-Cang BuSource :
- Ying yong sheng tai xue bao = The journal of applied ecology [ 1001-9332 ] ; 2010.
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- MESH :
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- MESH :
Abstract
Taking the broad-leaved Korean pine forest area in Changbai Mountains, a typical eastern forest belt of Northeast China for global change as test object, and by using the approaches of trenching-plot and infrared gas exchange analyzer, this paper analyzed the soil respiration in a selected series of degraded Korean pine forest ecosystem, i.e., broad-leaved Korean pine forest (CK), poplar-birch forest (Y), hardwood forest (S), Mongolian oak forest (M), and bare land (L). In the growth season of the forests, soil respiration showed a clear single peak curve, with the maximum in July or August. The soil respiration decreased in the sequence of Y>M>CK>S>L. The amount of CO2 release in Y and M was about 0.4 and 0.3 times higher than that in CK; and that in S and L accounted for 88% and 78% of CK, respectively.
PubMed: 20707087
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<author><name sortKey="Liang, Yu" sort="Liang, Yu" uniqKey="Liang Y" first="Yu" last="Liang">Yu Liang</name>
<affiliation wicri:level="1"><nlm:affiliation>College of Urban and Environmental Sciences, Northeast Normal University, Changchun 130024, China. liangysts@gmail.com</nlm:affiliation>
<country xml:lang="fr">République populaire de Chine</country>
<wicri:regionArea>College of Urban and Environmental Sciences, Northeast Normal University, Changchun 130024</wicri:regionArea>
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<author><name sortKey="Xu, Jia Wei" sort="Xu, Jia Wei" uniqKey="Xu J" first="Jia-Wei" last="Xu">Jia-Wei Xu</name>
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<author><name sortKey="Hu, Yuan Man" sort="Hu, Yuan Man" uniqKey="Hu Y" first="Yuan-Man" last="Hu">Yuan-Man Hu</name>
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<author><name sortKey="Chang, Yu" sort="Chang, Yu" uniqKey="Chang Y" first="Yu" last="Chang">Yu Chang</name>
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<author><name sortKey="Bu, Ren Cang" sort="Bu, Ren Cang" uniqKey="Bu R" first="Ren-Cang" last="Bu">Ren-Cang Bu</name>
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<term>Carbon Dioxide (analysis)</term>
<term>China (MeSH)</term>
<term>Ecosystem (MeSH)</term>
<term>Pinus (growth & development)</term>
<term>Pinus (metabolism)</term>
<term>Populus (growth & development)</term>
<term>Populus (metabolism)</term>
<term>Quercus (growth & development)</term>
<term>Quercus (metabolism)</term>
<term>Soil (analysis)</term>
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<keywords scheme="KwdFr" xml:lang="fr"><term>Carbone (analyse)</term>
<term>Chine (MeSH)</term>
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<term>Pinus (métabolisme)</term>
<term>Populus (croissance et développement)</term>
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<term>Quercus (croissance et développement)</term>
<term>Quercus (métabolisme)</term>
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<front><div type="abstract" xml:lang="en">Taking the broad-leaved Korean pine forest area in Changbai Mountains, a typical eastern forest belt of Northeast China for global change as test object, and by using the approaches of trenching-plot and infrared gas exchange analyzer, this paper analyzed the soil respiration in a selected series of degraded Korean pine forest ecosystem, i.e., broad-leaved Korean pine forest (CK), poplar-birch forest (Y), hardwood forest (S), Mongolian oak forest (M), and bare land (L). In the growth season of the forests, soil respiration showed a clear single peak curve, with the maximum in July or August. The soil respiration decreased in the sequence of Y>M>CK>S>L. The amount of CO2 release in Y and M was about 0.4 and 0.3 times higher than that in CK; and that in S and L accounted for 88% and 78% of CK, respectively.</div>
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<Abstract><AbstractText>Taking the broad-leaved Korean pine forest area in Changbai Mountains, a typical eastern forest belt of Northeast China for global change as test object, and by using the approaches of trenching-plot and infrared gas exchange analyzer, this paper analyzed the soil respiration in a selected series of degraded Korean pine forest ecosystem, i.e., broad-leaved Korean pine forest (CK), poplar-birch forest (Y), hardwood forest (S), Mongolian oak forest (M), and bare land (L). In the growth season of the forests, soil respiration showed a clear single peak curve, with the maximum in July or August. The soil respiration decreased in the sequence of Y>M>CK>S>L. The amount of CO2 release in Y and M was about 0.4 and 0.3 times higher than that in CK; and that in S and L accounted for 88% and 78% of CK, respectively.</AbstractText>
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