Winter soil CO2 flux from different mid-latitude sites from Middle Taihang Mountain in north China.
Identifieur interne : 001F61 ( Main/Exploration ); précédent : 001F60; suivant : 001F62Winter soil CO2 flux from different mid-latitude sites from Middle Taihang Mountain in north China.
Auteurs : Huitao Shen [République populaire de Chine] ; Jiansheng Cao [République populaire de Chine] ; Wanjun Zhang [République populaire de Chine] ; Xinhua Zeng [République populaire de Chine] ; Huaru Wang [République populaire de Chine]Source :
- PloS one [ 1932-6203 ] ; 2014.
Descripteurs français
- KwdFr :
- MESH :
- analyse : Carbone, Dioxyde de carbone.
- composition chimique : Sol.
- croissance et développement : Poaceae.
- Chine, Facteurs temps, Humidité, Saisons, Température, Écosystème.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Carbon, Carbon Dioxide.
- chemical , chemistry : Soil.
- growth & development : Poaceae.
- China, Ecosystem, Humidity, Seasons, Temperature, Time Factors.
Abstract
Winter soil respiration is a very important component of the annual soil carbon flux in some ecosystems. We hypothesized that, with all other factors being equal, shorter winter SR result in reduced contribution to annual soil C flux. In this study, the contribution of winter soil respiration to annual soil respiration was measured for three sites (grassland: dominated by Artemisia sacrorum, Bothriochloa ischaemum and Themeda japonica; shrubland: dominated by Vitex negundo var. heterophylla; plantation: dominated by Populus tomatosa) in a mountainous area of north China. Diurnal and intra-annual soil CO2 flux patterns were consistent among different sites, with the maximum soil respiration rates at 12∶00 or 14∶00, and in July or August. The lowest respiration rates were seen in February. Mean soil respiration rates ranged from 0.26 to 0.45 µmol m(-2) s(-1) in the winter (December to February), and between 2.38 to 3.16 µmol m(-2) s(-1) during the growing season (May-September). The winter soil carbon flux was 24.6 to 42.8 g C m(-2), which contributed 4.8 to 7.1% of the annual soil carbon flux. Based on exponential functions, soil temperature explained 73.8 to 91.8% of the within year variability in soil respiration rates. The Q10 values of SR against ST at 10 cm ranged from 3.60 to 4.90 among different sites. In addition, the equation between soil respiration and soil temperature for the growing season was used to calculate the "modeled" annual soil carbon flux based on the actual measured soil temperature. The "measured" annual value was significantly higher than the "modeled" annual value. Our results suggest that winter soil respiration plays a significant role in annual soil carbon balance, and should not be neglected when soil ecosystems are assessed as either sinks or sources of atmospheric CO2.
DOI: 10.1371/journal.pone.0091589
PubMed: 24614868
PubMed Central: PMC3948914
Affiliations:
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W" first="Wanjun" last="Zhang">Wanjun Zhang</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei</wicri:regionArea><wicri:noRegion>Hebei</wicri:noRegion></affiliation></author><author><name sortKey="Zeng, Xinhua" sort="Zeng, Xinhua" uniqKey="Zeng X" first="Xinhua" last="Zeng">Xinhua Zeng</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory 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wicri:level="1"><nlm:affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei</wicri:regionArea><wicri:noRegion>Hebei</wicri:noRegion></affiliation></author><author><name sortKey="Cao, Jiansheng" sort="Cao, Jiansheng" uniqKey="Cao J" first="Jiansheng" last="Cao">Jiansheng Cao</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei</wicri:regionArea><wicri:noRegion>Hebei</wicri:noRegion></affiliation></author><author><name sortKey="Zhang, Wanjun" sort="Zhang, Wanjun" uniqKey="Zhang W" first="Wanjun" last="Zhang">Wanjun Zhang</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</nlm:affiliation><country 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(analysis)</term><term>Carbon Dioxide (analysis)</term><term>China (MeSH)</term><term>Ecosystem (MeSH)</term><term>Humidity (MeSH)</term><term>Poaceae (growth & development)</term><term>Seasons (MeSH)</term><term>Soil (chemistry)</term><term>Temperature (MeSH)</term><term>Time Factors (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Carbone (analyse)</term><term>Chine (MeSH)</term><term>Dioxyde de carbone (analyse)</term><term>Facteurs temps (MeSH)</term><term>Humidité (MeSH)</term><term>Poaceae (croissance et développement)</term><term>Saisons (MeSH)</term><term>Sol (composition chimique)</term><term>Température (MeSH)</term><term>Écosystème (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en"><term>Carbon</term><term>Carbon Dioxide</term></keywords><keywords scheme="MESH" type="chemical" qualifier="chemistry" xml:lang="en"><term>Soil</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Carbone</term><term>Dioxyde de carbone</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Sol</term></keywords><keywords scheme="MESH" qualifier="croissance et développement" xml:lang="fr"><term>Poaceae</term></keywords><keywords scheme="MESH" qualifier="growth & development" xml:lang="en"><term>Poaceae</term></keywords><keywords scheme="MESH" xml:lang="en"><term>China</term><term>Ecosystem</term><term>Humidity</term><term>Seasons</term><term>Temperature</term><term>Time Factors</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Chine</term><term>Facteurs temps</term><term>Humidité</term><term>Saisons</term><term>Température</term><term>Écosystème</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Winter soil respiration is a very important component of the annual soil carbon flux in some ecosystems. We hypothesized that, with all other factors being equal, shorter winter SR result in reduced contribution to annual soil C flux. In this study, the contribution of winter soil respiration to annual soil respiration was measured for three sites (grassland: dominated by Artemisia sacrorum, Bothriochloa ischaemum and Themeda japonica; shrubland: dominated by Vitex negundo var. heterophylla; plantation: dominated by Populus tomatosa) in a mountainous area of north China. Diurnal and intra-annual soil CO2 flux patterns were consistent among different sites, with the maximum soil respiration rates at 12∶00 or 14∶00, and in July or August. The lowest respiration rates were seen in February. Mean soil respiration rates ranged from 0.26 to 0.45 µmol m(-2) s(-1) in the winter (December to February), and between 2.38 to 3.16 µmol m(-2) s(-1) during the growing season (May-September). The winter soil carbon flux was 24.6 to 42.8 g C m(-2), which contributed 4.8 to 7.1% of the annual soil carbon flux. Based on exponential functions, soil temperature explained 73.8 to 91.8% of the within year variability in soil respiration rates. The Q10 values of SR against ST at 10 cm ranged from 3.60 to 4.90 among different sites. In addition, the equation between soil respiration and soil temperature for the growing season was used to calculate the "modeled" annual soil carbon flux based on the actual measured soil temperature. The "measured" annual value was significantly higher than the "modeled" annual value. Our results suggest that winter soil respiration plays a significant role in annual soil carbon balance, and should not be neglected when soil ecosystems are assessed as either sinks or sources of atmospheric CO2.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">24614868</PMID><DateCompleted><Year>2016</Year><Month>03</Month><Day>31</Day></DateCompleted><DateRevised><Year>2018</Year><Month>11</Month><Day>13</Day></DateRevised><Article PubModel="Electronic-eCollection"><Journal><ISSN IssnType="Electronic">1932-6203</ISSN><JournalIssue CitedMedium="Internet"><Volume>9</Volume><Issue>3</Issue><PubDate><Year>2014</Year></PubDate></JournalIssue><Title>PloS one</Title><ISOAbbreviation>PLoS One</ISOAbbreviation></Journal><ArticleTitle>Winter soil CO2 flux from different mid-latitude sites from Middle Taihang Mountain in north China.</ArticleTitle><Pagination><MedlinePgn>e91589</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1371/journal.pone.0091589</ELocationID><Abstract><AbstractText>Winter soil respiration is a very important component of the annual soil carbon flux in some ecosystems. We hypothesized that, with all other factors being equal, shorter winter SR result in reduced contribution to annual soil C flux. In this study, the contribution of winter soil respiration to annual soil respiration was measured for three sites (grassland: dominated by Artemisia sacrorum, Bothriochloa ischaemum and Themeda japonica; shrubland: dominated by Vitex negundo var. heterophylla; plantation: dominated by Populus tomatosa) in a mountainous area of north China. Diurnal and intra-annual soil CO2 flux patterns were consistent among different sites, with the maximum soil respiration rates at 12∶00 or 14∶00, and in July or August. The lowest respiration rates were seen in February. Mean soil respiration rates ranged from 0.26 to 0.45 µmol m(-2) s(-1) in the winter (December to February), and between 2.38 to 3.16 µmol m(-2) s(-1) during the growing season (May-September). The winter soil carbon flux was 24.6 to 42.8 g C m(-2), which contributed 4.8 to 7.1% of the annual soil carbon flux. Based on exponential functions, soil temperature explained 73.8 to 91.8% of the within year variability in soil respiration rates. The Q10 values of SR against ST at 10 cm ranged from 3.60 to 4.90 among different sites. In addition, the equation between soil respiration and soil temperature for the growing season was used to calculate the "modeled" annual soil carbon flux based on the actual measured soil temperature. The "measured" annual value was significantly higher than the "modeled" annual value. Our results suggest that winter soil respiration plays a significant role in annual soil carbon balance, and should not be neglected when soil ecosystems are assessed as either sinks or sources of atmospheric CO2.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Shen</LastName><ForeName>Huitao</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Cao</LastName><ForeName>Jiansheng</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhang</LastName><ForeName>Wanjun</ForeName><Initials>W</Initials><AffiliationInfo><Affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zeng</LastName><ForeName>Xinhua</ForeName><Initials>X</Initials><AffiliationInfo><Affiliation>Key Laboratory for Agricultural Water Resources, Hebei Key Laboratory for Agricultural Water-Saving, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, Hebei, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Huaru</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>Yellow River Water Resources Protection Institute, Zhengzhou, He'nan, China.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType><PublicationType UI="D013485">Research Support, Non-U.S. Gov't</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2014</Year><Month>03</Month><Day>10</Day></ArticleDate></Article><MedlineJournalInfo><Country>United States</Country><MedlineTA>PLoS One</MedlineTA><NlmUniqueID>101285081</NlmUniqueID><ISSNLinking>1932-6203</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical><Chemical><RegistryNumber>142M471B3J</RegistryNumber><NameOfSubstance UI="D002245">Carbon Dioxide</NameOfSubstance></Chemical><Chemical><RegistryNumber>7440-44-0</RegistryNumber><NameOfSubstance UI="D002244">Carbon</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D002244" MajorTopicYN="N">Carbon</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="N">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D002245" MajorTopicYN="N">Carbon Dioxide</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D017753" MajorTopicYN="Y">Ecosystem</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D006813" MajorTopicYN="N">Humidity</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D006109" MajorTopicYN="N">Poaceae</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="N">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D012621" MajorTopicYN="Y">Seasons</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D013696" MajorTopicYN="N">Temperature</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D013997" MajorTopicYN="N">Time Factors</DescriptorName></MeshHeading></MeshHeadingList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2013</Year><Month>12</Month><Day>31</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2014</Year><Month>02</Month><Day>13</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2014</Year><Month>3</Month><Day>12</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2014</Year><Month>3</Month><Day>13</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2016</Year><Month>4</Month><Day>1</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>epublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">24614868</ArticleId><ArticleId IdType="doi">10.1371/journal.pone.0091589</ArticleId><ArticleId IdType="pii">PONE-D-13-55172</ArticleId><ArticleId IdType="pmc">PMC3948914</ArticleId></ArticleIdList><ReferenceList><Reference><Citation>Sci Total Environ. 2013 Feb 1;444:363-8</Citation><ArticleIdList><ArticleId IdType="pubmed">23280294</ArticleId></ArticleIdList></Reference><Reference><Citation>New Phytol. 2008 Jul;179(2):460-71</Citation><ArticleIdList><ArticleId IdType="pubmed">19086292</ArticleId></ArticleIdList></Reference><Reference><Citation>PLoS One. 2012;7(8):e42354</Citation><ArticleIdList><ArticleId 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Shen</name></noRegion><name sortKey="Cao, Jiansheng" sort="Cao, Jiansheng" uniqKey="Cao J" first="Jiansheng" last="Cao">Jiansheng Cao</name><name sortKey="Wang, Huaru" sort="Wang, Huaru" uniqKey="Wang H" first="Huaru" last="Wang">Huaru Wang</name><name sortKey="Zeng, Xinhua" sort="Zeng, Xinhua" uniqKey="Zeng X" first="Xinhua" last="Zeng">Xinhua Zeng</name><name sortKey="Zhang, Wanjun" sort="Zhang, Wanjun" uniqKey="Zhang W" first="Wanjun" last="Zhang">Wanjun Zhang</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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