Spatial variations in concentration, compositions of glomalin related soil protein in poplar plantations in northeastern China, and possible relations with soil physicochemical properties.
Identifieur interne : 002046 ( Main/Exploration ); précédent : 002045; suivant : 002047Spatial variations in concentration, compositions of glomalin related soil protein in poplar plantations in northeastern China, and possible relations with soil physicochemical properties.
Auteurs : Qiong Wang [République populaire de Chine] ; Yan Wu [République populaire de Chine] ; Wenjie Wang [République populaire de Chine] ; Zhaoliang Zhong [République populaire de Chine] ; Zhongxue Pei [République populaire de Chine] ; Jie Ren [République populaire de Chine] ; Huimei Wang [République populaire de Chine] ; Yuangang Zu [République populaire de Chine]Source :
- TheScientificWorldJournal [ 1537-744X ] ; 2014.
Descripteurs français
- KwdFr :
- MESH :
- composition chimique : Sol.
- Chine, Diffraction des rayons X.
English descriptors
- KwdEn :
- MESH :
- chemical , chemistry : Soil.
- China, X-Ray Diffraction.
Abstract
Concentration of Glomalin Related Soil Protein is reportedly close related to soil functions, but few data is available for GRSP compositional variations and function related to soil properties. In this paper, soils from 0-20 cm, 20-40 cm, 40-60 cm, 60-80 cm, and 80-100 cm layers were collected in 72 poplar shelterbelts in Songnen Plain (6 regions) for implementing this data shortage. GRSP mainly consists of stretching of O-H, N-H, C-H, C=O, COO-, C-O, and Si-O-Si and bending of C-H and O-H. It has seven fluorescent substances of tyrosine-like protein, tryptophan-like protein, fulvic acid-like, humic acid-like, soluble microbial byproduct-like, nitrobenzoxadiazole-like, and calcofluor white-like, with characteristic X-ray diffraction peak at 2 θ = 19.8° and 129.3 nm grain size as well as 1.08% low crystallinity. Large spatial variations (intersite and intrasite down profile) were found in either GRSP concentration or these compositional traits. Regression analysis clearly manifested that soil pH should be responsible for these variations. However, negative relations between soil bulk density and GRSP quantity were observed, but not its compositional traits. These basic data in poplar shelterbelt forests are good for understanding the underlying mechanism of GRSP in soil functional maintenance.
DOI: 10.1155/2014/160403
PubMed: 24955385
PubMed Central: PMC3997909
Affiliations:
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150040</wicri:noRegion></affiliation></author><author><name sortKey="Wu, Yan" sort="Wu, Yan" uniqKey="Wu Y" first="Yan" last="Wu">Yan Wu</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China ; Daqing Normal University, Daqing 163712, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China ; Daqing Normal University, Daqing 163712</wicri:regionArea><wicri:noRegion>Daqing 163712</wicri:noRegion></affiliation></author><author><name sortKey="Wang, Wenjie" sort="Wang, Wenjie" uniqKey="Wang W" first="Wenjie" last="Wang">Wenjie Wang</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</nlm:affiliation><country xml:lang="fr">République populaire de 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150040, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040</wicri:regionArea><wicri:noRegion>Harbin 150040</wicri:noRegion></affiliation></author><author><name sortKey="Ren, Jie" sort="Ren, Jie" uniqKey="Ren J" first="Jie" last="Ren">Jie Ren</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040</wicri:regionArea><wicri:noRegion>Harbin 150040</wicri:noRegion></affiliation></author><author><name sortKey="Wang, Huimei" sort="Wang, Huimei" uniqKey="Wang H" first="Huimei" last="Wang">Huimei Wang</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040</wicri:regionArea><wicri:noRegion>Harbin 150040</wicri:noRegion></affiliation></author><author><name sortKey="Zu, Yuangang" sort="Zu, Yuangang" uniqKey="Zu Y" first="Yuangang" last="Zu">Yuangang Zu</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040</wicri:regionArea><wicri:noRegion>Harbin 150040</wicri:noRegion></affiliation></author></analytic><series><title level="j">TheScientificWorldJournal</title><idno type="eISSN">1537-744X</idno><imprint><date when="2014" type="published">2014</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>China (MeSH)</term><term>Soil (chemistry)</term><term>X-Ray Diffraction (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Chine (MeSH)</term><term>Diffraction des rayons X (MeSH)</term><term>Sol (composition chimique)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="chemistry" xml:lang="en"><term>Soil</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Sol</term></keywords><keywords scheme="MESH" xml:lang="en"><term>China</term><term>X-Ray Diffraction</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Chine</term><term>Diffraction des rayons X</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Concentration of Glomalin Related Soil Protein is reportedly close related to soil functions, but few data is available for GRSP compositional variations and function related to soil properties. In this paper, soils from 0-20 cm, 20-40 cm, 40-60 cm, 60-80 cm, and 80-100 cm layers were collected in 72 poplar shelterbelts in Songnen Plain (6 regions) for implementing this data shortage. GRSP mainly consists of stretching of O-H, N-H, C-H, C=O, COO-, C-O, and Si-O-Si and bending of C-H and O-H. It has seven fluorescent substances of tyrosine-like protein, tryptophan-like protein, fulvic acid-like, humic acid-like, soluble microbial byproduct-like, nitrobenzoxadiazole-like, and calcofluor white-like, with characteristic X-ray diffraction peak at 2 θ = 19.8° and 129.3 nm grain size as well as 1.08% low crystallinity. Large spatial variations (intersite and intrasite down profile) were found in either GRSP concentration or these compositional traits. Regression analysis clearly manifested that soil pH should be responsible for these variations. However, negative relations between soil bulk density and GRSP quantity were observed, but not its compositional traits. These basic data in poplar shelterbelt forests are good for understanding the underlying mechanism of GRSP in soil functional maintenance.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">24955385</PMID><DateCompleted><Year>2015</Year><Month>02</Month><Day>02</Day></DateCompleted><DateRevised><Year>2018</Year><Month>11</Month><Day>13</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1537-744X</ISSN><JournalIssue CitedMedium="Internet"><Volume>2014</Volume><PubDate><Year>2014</Year></PubDate></JournalIssue><Title>TheScientificWorldJournal</Title><ISOAbbreviation>ScientificWorldJournal</ISOAbbreviation></Journal><ArticleTitle>Spatial variations in concentration, compositions of glomalin related soil protein in poplar plantations in northeastern China, and possible relations with soil physicochemical properties.</ArticleTitle><Pagination><MedlinePgn>160403</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1155/2014/160403</ELocationID><Abstract><AbstractText>Concentration of Glomalin Related Soil Protein is reportedly close related to soil functions, but few data is available for GRSP compositional variations and function related to soil properties. In this paper, soils from 0-20 cm, 20-40 cm, 40-60 cm, 60-80 cm, and 80-100 cm layers were collected in 72 poplar shelterbelts in Songnen Plain (6 regions) for implementing this data shortage. GRSP mainly consists of stretching of O-H, N-H, C-H, C=O, COO-, C-O, and Si-O-Si and bending of C-H and O-H. It has seven fluorescent substances of tyrosine-like protein, tryptophan-like protein, fulvic acid-like, humic acid-like, soluble microbial byproduct-like, nitrobenzoxadiazole-like, and calcofluor white-like, with characteristic X-ray diffraction peak at 2 θ = 19.8° and 129.3 nm grain size as well as 1.08% low crystallinity. Large spatial variations (intersite and intrasite down profile) were found in either GRSP concentration or these compositional traits. Regression analysis clearly manifested that soil pH should be responsible for these variations. However, negative relations between soil bulk density and GRSP quantity were observed, but not its compositional traits. These basic data in poplar shelterbelt forests are good for understanding the underlying mechanism of GRSP in soil functional maintenance.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Qiong</ForeName><Initials>Q</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wu</LastName><ForeName>Yan</ForeName><Initials>Y</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China ; Daqing Normal University, Daqing 163712, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Wenjie</ForeName><Initials>W</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhong</LastName><ForeName>Zhaoliang</ForeName><Initials>Z</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Pei</LastName><ForeName>Zhongxue</ForeName><Initials>Z</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Ren</LastName><ForeName>Jie</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Huimei</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zu</LastName><ForeName>Yuangang</ForeName><Initials>Y</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, 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>04</Month><Day>06</Day></ArticleDate></Article><MedlineJournalInfo><Country>United States</Country><MedlineTA>ScientificWorldJournal</MedlineTA><NlmUniqueID>101131163</NlmUniqueID><ISSNLinking>1537-744X</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D014961" MajorTopicYN="N">X-Ray Diffraction</DescriptorName></MeshHeading></MeshHeadingList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2013</Year><Month>12</Month><Day>09</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2014</Year><Month>02</Month><Day>20</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2014</Year><Month>6</Month><Day>24</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2014</Year><Month>6</Month><Day>24</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2015</Year><Month>2</Month><Day>3</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">24955385</ArticleId><ArticleId IdType="doi">10.1155/2014/160403</ArticleId><ArticleId IdType="pmc">PMC3997909</ArticleId></ArticleIdList><ReferenceList><Reference><Citation>Nature. 2001 Nov 22;414(6862):462-70</Citation><ArticleIdList><ArticleId IdType="pubmed">11719809</ArticleId></ArticleIdList></Reference><Reference><Citation>Environ Sci Technol. 2003 Jan 1;37(1):18A-26A</Citation><ArticleIdList><ArticleId IdType="pubmed">12542280</ArticleId></ArticleIdList></Reference><Reference><Citation>Environ Sci Technol. 2003 Dec 15;37(24):5701-10</Citation><ArticleIdList><ArticleId 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Chine</li></country></list><tree><country name="République populaire de Chine"><noRegion><name sortKey="Wang, Qiong" sort="Wang, Qiong" uniqKey="Wang Q" first="Qiong" last="Wang">Qiong Wang</name></noRegion><name sortKey="Pei, Zhongxue" sort="Pei, Zhongxue" uniqKey="Pei Z" first="Zhongxue" last="Pei">Zhongxue Pei</name><name sortKey="Ren, Jie" sort="Ren, Jie" uniqKey="Ren J" first="Jie" last="Ren">Jie Ren</name><name sortKey="Wang, Huimei" sort="Wang, Huimei" uniqKey="Wang H" first="Huimei" last="Wang">Huimei Wang</name><name sortKey="Wang, Wenjie" sort="Wang, Wenjie" uniqKey="Wang W" first="Wenjie" last="Wang">Wenjie Wang</name><name sortKey="Wu, Yan" sort="Wu, Yan" uniqKey="Wu Y" first="Yan" last="Wu">Yan Wu</name><name sortKey="Zhong, Zhaoliang" sort="Zhong, Zhaoliang" uniqKey="Zhong Z" first="Zhaoliang" last="Zhong">Zhaoliang Zhong</name><name sortKey="Zu, Yuangang" sort="Zu, Yuangang" uniqKey="Zu Y" first="Yuangang" last="Zu">Yuangang 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