[Root biomass and underground C and N storage of primitive Korean pine and broad-leaved climax forest in Changbai Mountains at its different succession stages].
Identifieur interne : 003F34 ( Main/Corpus ); précédent : 003F33; suivant : 003F35[Root biomass and underground C and N storage of primitive Korean pine and broad-leaved climax forest in Changbai Mountains at its different succession stages].
Auteurs : Liyun Yang ; Tianxiang Luo ; Songtao WuSource :
- Ying yong sheng tai xue bao = The journal of applied ecology [ 1001-9332 ] ; 2005.
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- KwdEn :
- MESH :
Abstract
With more than 200 years old primitive Korean pine and broad-leaved climax forest and its two 20 and 80 years old secondary Populus davidiana and Betula platyphylla forests in Changbai Mountains as test objects, this paper studied their root biomass and underground C and N storage. The results showed that with forest succession, the root biomass of 20 years old, 80 years old, and climax forests was 2.437, 2.742 and 4.114 kg x m(-2), respectively. The root C storage was 1.113, 1.323 and 2.023 kg x m(-2), soil C storage was 11.911, 11.943 and 12.587 kg x m(-2), and underground C storage was 13.024, 13.266 and 14.610 kg x m(-2), respectively, while the root N storage was 0.035, 0.032 and 0.038 kg x m(-2), soil N storage was 1.207, 1.222 and 0.915 kg x m(-2), and underground N storage was 1.243, 1.254 and 0.955 kg x m(-2), respectively, which indicated that along with forest succession, forest underground became a potential "carbon sink", whereas underground N storage did not change obviously.
PubMed: 16252851
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The results showed that with forest succession, the root biomass of 20 years old, 80 years old, and climax forests was 2.437, 2.742 and 4.114 kg x m(-2), respectively. The root C storage was 1.113, 1.323 and 2.023 kg x m(-2), soil C storage was 11.911, 11.943 and 12.587 kg x m(-2), and underground C storage was 13.024, 13.266 and 14.610 kg x m(-2), respectively, while the root N storage was 0.035, 0.032 and 0.038 kg x m(-2), soil N storage was 1.207, 1.222 and 0.915 kg x m(-2), and underground N storage was 1.243, 1.254 and 0.955 kg x m(-2), respectively, which indicated that along with forest succession, forest underground became a potential "carbon sink", whereas underground N storage did not change obviously.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">16252851</PMID><DateCompleted><Year>2007</Year><Month>01</Month><Day>23</Day></DateCompleted><DateRevised><Year>2017</Year><Month>11</Month><Day>16</Day></DateRevised><Article PubModel="Print"><Journal><ISSN IssnType="Print">1001-9332</ISSN><JournalIssue CitedMedium="Print"><Volume>16</Volume><Issue>7</Issue><PubDate><Year>2005</Year><Month>Jul</Month></PubDate></JournalIssue><Title>Ying yong sheng tai xue bao = The journal of applied ecology</Title><ISOAbbreviation>Ying Yong Sheng Tai Xue Bao</ISOAbbreviation></Journal><ArticleTitle>[Root biomass and underground C and N storage of primitive Korean pine and broad-leaved climax forest in Changbai Mountains at its different succession stages].</ArticleTitle><Pagination><MedlinePgn>1195-9</MedlinePgn></Pagination><Abstract><AbstractText>With more than 200 years old primitive Korean pine and broad-leaved climax forest and its two 20 and 80 years old secondary Populus davidiana and Betula platyphylla forests in Changbai Mountains as test objects, this paper studied their root biomass and underground C and N storage. The results showed that with forest succession, the root biomass of 20 years old, 80 years old, and climax forests was 2.437, 2.742 and 4.114 kg x m(-2), respectively. The root C storage was 1.113, 1.323 and 2.023 kg x m(-2), soil C storage was 11.911, 11.943 and 12.587 kg x m(-2), and underground C storage was 13.024, 13.266 and 14.610 kg x m(-2), respectively, while the root N storage was 0.035, 0.032 and 0.038 kg x m(-2), soil N storage was 1.207, 1.222 and 0.915 kg x m(-2), and underground N storage was 1.243, 1.254 and 0.955 kg x m(-2), respectively, which indicated that along with forest succession, forest underground became a potential "carbon sink", whereas underground N storage did not change obviously.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Yang</LastName><ForeName>Liyun</ForeName><Initials>L</Initials><AffiliationInfo><Affiliation>Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China. wendy6393@sina.com</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Luo</LastName><ForeName>Tianxiang</ForeName><Initials>T</Initials></Author><Author ValidYN="Y"><LastName>Wu</LastName><ForeName>Songtao</ForeName><Initials>S</Initials></Author></AuthorList><Language>chi</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType><PublicationType UI="D013485">Research Support, Non-U.S. Gov't</PublicationType></PublicationTypeList></Article><MedlineJournalInfo><Country>China</Country><MedlineTA>Ying Yong Sheng Tai Xue Bao</MedlineTA><NlmUniqueID>9425159</NlmUniqueID><ISSNLinking>1001-9332</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical><Chemical><RegistryNumber>7440-44-0</RegistryNumber><NameOfSubstance UI="D002244">Carbon</NameOfSubstance></Chemical><Chemical><RegistryNumber>N762921K75</RegistryNumber><NameOfSubstance UI="D009584">Nitrogen</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D029662" MajorTopicYN="N">Betula</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="N">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D018533" MajorTopicYN="Y">Biomass</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D002244" MajorTopicYN="N">Carbon</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D009584" MajorTopicYN="N">Nitrogen</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D028223" MajorTopicYN="N">Pinus</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="Y">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D018517" MajorTopicYN="N">Plant Roots</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="N">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="N">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="N">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D014197" MajorTopicYN="N">Trees</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="Y">growth & development</QualifierName></MeshHeading></MeshHeadingList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="pubmed"><Year>2005</Year><Month>10</Month><Day>29</Day><Hour>9</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2007</Year><Month>1</Month><Day>24</Day><Hour>9</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2005</Year><Month>10</Month><Day>29</Day><Hour>9</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">16252851</ArticleId></ArticleIdList></PubmedData></pubmed></record>Pour manipuler ce document sous Unix (Dilib)
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