[Influences of shallow groundwater on sap flow of riparian poplar plantations in northern China.]
Identifieur interne : 001586 ( Main/Exploration ); précédent : 001585; suivant : 001587[Influences of shallow groundwater on sap flow of riparian poplar plantations in northern China.]
Auteurs : Chao Luo [République populaire de Chine] ; Tong Gang Zha [République populaire de Chine] ; Meng Xun Zhu [République populaire de Chine] ; Zhi Jun Zhu [République populaire de Chine] ; Zi Yao Wang [République populaire de Chine] ; Wen Na Liu [République populaire de Chine]Source :
- Ying yong sheng tai xue bao = The journal of applied ecology [ 1001-9332 ] ; 2016.
Descripteurs français
- KwdFr :
- MESH :
- physiologie : Populus, Tiges de plante.
- Chine, Eau, Gaz, Lumière du soleil, Nappe phréatique, Pékin, Rivières, Saisons, Sol.
English descriptors
- KwdEn :
- MESH :
Abstract
Water use strategy in growing seasons plays a great role in the management of riparian poplar plantations in northern China. The research was conducted on a poplar (Populus × euramericana cv. '74/76') plantation located near the floodplain of Chaobai River in the northeastern su-burb of Beijing. The influencing factors of poplar sap flow (SF) were presented based on the measurements on the stem SF with thermal dissipation sap flow probe (TDP), soil volumetric water content (VWC) with time-domain-reflectometer (TDR) and environmental factors with eddy cova-riance system from June to July, 2014, to explore the impact of shallow ground water on SF. The results showed that the diurnal variation of SF presented single or double peaks depending on the varia-tion of solar radiation (R). The SF density decreased in soil water relative deficient period (RDP), and the peak time advanced to 12:30 from 14:00, while the time lag between the SF density and R showed no obvious change. The solar radiation and air vapor pressure deficit were the predominant factors of SF during soil water relative sufficient period (RSP), while soil water became the limiting factor in RDP. During the RDP, the daily water consumption of individual poplar tree was significantly negatively correlated with soil VWC at the depth of 100 cm, and significantly positively correlated with soil VWC of the other depths. The shallow ground water (at the depth of ≥150 cm where the soil water content showed little change) might move to the upper soil layer controlled by the capillary force and supply for poplar growth during the soil water-relatively deficient period.
DOI: 10.13287/j.1001-9332.201605.025
PubMed: 29732800
Affiliations:
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type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Zha, Tong Gang" sort="Zha, Tong Gang" uniqKey="Zha T" first="Tong Gang" last="Zha">Tong Gang Zha</name><affiliation wicri:level="1"><nlm:affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Zhu, Meng Xun" sort="Zhu, Meng Xun" uniqKey="Zhu M" first="Meng Xun" last="Zhu">Meng Xun Zhu</name><affiliation wicri:level="1"><nlm:affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Zhu, Zhi Jun" sort="Zhu, Zhi Jun" uniqKey="Zhu Z" first="Zhi Jun" last="Zhu">Zhi Jun Zhu</name><affiliation wicri:level="1"><nlm:affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Wang, Zi Yao" sort="Wang, Zi Yao" uniqKey="Wang Z" first="Zi Yao" last="Wang">Zi Yao Wang</name><affiliation wicri:level="1"><nlm:affiliation>School of Landscape Architecture, Beijing Forestry University, Beijing 100083, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>School of Landscape Architecture, Beijing Forestry University, Beijing 100083</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Liu, Wen Na" sort="Liu, Wen Na" uniqKey="Liu W" first="Wen Na" last="Liu">Wen Na Liu</name><affiliation wicri:level="1"><nlm:affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author></analytic><series><title level="j">Ying yong sheng tai xue bao = The journal of applied ecology</title><idno type="ISSN">1001-9332</idno><imprint><date when="2016" type="published">2016</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Beijing (MeSH)</term><term>China (MeSH)</term><term>Gases (MeSH)</term><term>Groundwater (MeSH)</term><term>Plant Stems (physiology)</term><term>Populus (physiology)</term><term>Rivers (MeSH)</term><term>Seasons (MeSH)</term><term>Soil (MeSH)</term><term>Sunlight (MeSH)</term><term>Water (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Chine (MeSH)</term><term>Eau (MeSH)</term><term>Gaz (MeSH)</term><term>Lumière du soleil (MeSH)</term><term>Nappe phréatique (MeSH)</term><term>Populus (physiologie)</term><term>Pékin (MeSH)</term><term>Rivières (MeSH)</term><term>Saisons (MeSH)</term><term>Sol (MeSH)</term><term>Tiges de plante (physiologie)</term></keywords><keywords scheme="MESH" type="chemical" xml:lang="en"><term>Gases</term><term>Soil</term><term>Water</term></keywords><keywords scheme="MESH" qualifier="physiologie" xml:lang="fr"><term>Populus</term><term>Tiges de plante</term></keywords><keywords scheme="MESH" qualifier="physiology" xml:lang="en"><term>Plant Stems</term><term>Populus</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Beijing</term><term>China</term><term>Groundwater</term><term>Rivers</term><term>Seasons</term><term>Sunlight</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Chine</term><term>Eau</term><term>Gaz</term><term>Lumière du soleil</term><term>Nappe phréatique</term><term>Pékin</term><term>Rivières</term><term>Saisons</term><term>Sol</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Water use strategy in growing seasons plays a great role in the management of riparian poplar plantations in northern China. The research was conducted on a poplar (Populus × euramericana cv. '74/76') plantation located near the floodplain of Chaobai River in the northeastern su-burb of Beijing. The influencing factors of poplar sap flow (SF) were presented based on the measurements on the stem SF with thermal dissipation sap flow probe (TDP), soil volumetric water content (VWC) with time-domain-reflectometer (TDR) and environmental factors with eddy cova-riance system from June to July, 2014, to explore the impact of shallow ground water on SF. The results showed that the diurnal variation of SF presented single or double peaks depending on the varia-tion of solar radiation (R). The SF density decreased in soil water relative deficient period (RDP), and the peak time advanced to 12:30 from 14:00, while the time lag between the SF density and R showed no obvious change. The solar radiation and air vapor pressure deficit were the predominant factors of SF during soil water relative sufficient period (RSP), while soil water became the limiting factor in RDP. During the RDP, the daily water consumption of individual poplar tree was significantly negatively correlated with soil VWC at the depth of 100 cm, and significantly positively correlated with soil VWC of the other depths. The shallow ground water (at the depth of ≥150 cm where the soil water content showed little change) might move to the upper soil layer controlled by the capillary force and supply for poplar growth during the soil water-relatively deficient period.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Curated" Owner="NLM"><PMID Version="1">29732800</PMID><DateCompleted><Year>2018</Year><Month>07</Month><Day>05</Day></DateCompleted><DateRevised><Year>2018</Year><Month>12</Month><Day>02</Day></DateRevised><Article PubModel="Print"><Journal><ISSN IssnType="Print">1001-9332</ISSN><JournalIssue CitedMedium="Print"><Volume>27</Volume><Issue>5</Issue><PubDate><Year>2016</Year><Month>May</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>[Influences of shallow groundwater on sap flow of riparian poplar plantations in northern China.]</ArticleTitle><Pagination><MedlinePgn>1401-1407</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.13287/j.1001-9332.201605.025</ELocationID><Abstract><AbstractText>Water use strategy in growing seasons plays a great role in the management of riparian poplar plantations in northern China. The research was conducted on a poplar (Populus × euramericana cv. '74/76') plantation located near the floodplain of Chaobai River in the northeastern su-burb of Beijing. The influencing factors of poplar sap flow (SF) were presented based on the measurements on the stem SF with thermal dissipation sap flow probe (TDP), soil volumetric water content (VWC) with time-domain-reflectometer (TDR) and environmental factors with eddy cova-riance system from June to July, 2014, to explore the impact of shallow ground water on SF. The results showed that the diurnal variation of SF presented single or double peaks depending on the varia-tion of solar radiation (R). The SF density decreased in soil water relative deficient period (RDP), and the peak time advanced to 12:30 from 14:00, while the time lag between the SF density and R showed no obvious change. The solar radiation and air vapor pressure deficit were the predominant factors of SF during soil water relative sufficient period (RSP), while soil water became the limiting factor in RDP. During the RDP, the daily water consumption of individual poplar tree was significantly negatively correlated with soil VWC at the depth of 100 cm, and significantly positively correlated with soil VWC of the other depths. The shallow ground water (at the depth of ≥150 cm where the soil water content showed little change) might move to the upper soil layer controlled by the capillary force and supply for poplar growth during the soil water-relatively deficient period.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Luo</LastName><ForeName>Chao</ForeName><Initials>C</Initials><AffiliationInfo><Affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zha</LastName><ForeName>Tong Gang</ForeName><Initials>TG</Initials><AffiliationInfo><Affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhu</LastName><ForeName>Meng Xun</ForeName><Initials>MX</Initials><AffiliationInfo><Affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhu</LastName><ForeName>Zhi Jun</ForeName><Initials>ZJ</Initials><AffiliationInfo><Affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Zi Yao</ForeName><Initials>ZY</Initials><AffiliationInfo><Affiliation>School of Landscape Architecture, Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Liu</LastName><ForeName>Wen Na</ForeName><Initials>WN</Initials><AffiliationInfo><Affiliation>Ministry of Education Forestry Ecological Engineering Research Center,Beijing Forestry University, Beijing 100083, China.</Affiliation></AffiliationInfo></Author></AuthorList><Language>chi</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><VernacularTitle>浅层地下水对华北地区河岸杨树林树干液流的影响.</VernacularTitle></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="D005740">Gases</NameOfSubstance></Chemical><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical><Chemical><RegistryNumber>059QF0KO0R</RegistryNumber><NameOfSubstance UI="D014867">Water</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D000068476" MajorTopicYN="N">Beijing</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D005740" MajorTopicYN="N">Gases</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D060587" MajorTopicYN="Y">Groundwater</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D018547" MajorTopicYN="N">Plant Stems</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="Y">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="Y">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D045483" MajorTopicYN="N">Rivers</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012621" MajorTopicYN="N">Seasons</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D013472" MajorTopicYN="N">Sunlight</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D014867" MajorTopicYN="N">Water</DescriptorName></MeshHeading></MeshHeadingList><OtherAbstract Type="Publisher" Language="chi"><AbstractText>华北地区河岸杨树林生长季的用水特征对杨树人工林经营管理具有重要意义.本文以北京市潮白河畔的杨树人工林为研究对象,采用热扩散式探针(TDP)测定树干液流、管式TDR土壤含水量法测定土壤体积含水量、开路涡度相关系统测定环境因子数据,对2014年6—7月的杨树树干液流及其影响因素进行系统研究,以探究浅层地下水对树干液流的可能影响.结果表明: 杨树树干液流日变化随太阳辐射呈现单峰或双峰变化,在土壤水分相对亏缺时,杨树树干液流密度明显减小,达到峰值的时间从14:00提前到12:30,但树干液流对太阳辐射的时滞效应没有明显变化.在表层土壤水分相对充足时,太阳辐射和空气饱和水汽压差是杨树树干液流变化的主导因子,但在表层土壤水分亏缺时,土壤水会成为杨树树干液流的限制因子;当表层土壤水分相对亏缺时,杨树单株耗水与100 cm土层土壤体积含水量呈显著负相关,与其余各土层体积含水量呈显著正相关.浅层地下水(相对稳定的150 cm及更深处)在土壤表层土壤水分含量相对亏缺时,可在毛管力作用下对上层土壤水进行补充,供给杨树生长需要.</AbstractText></OtherAbstract><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">riparian poplar plantation</Keyword><Keyword MajorTopicYN="N">sap flow</Keyword><Keyword MajorTopicYN="N">shallow groundwater</Keyword><Keyword MajorTopicYN="N">soil water</Keyword><Keyword MajorTopicYN="N">thermal dissipation probe</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="entrez"><Year>2018</Year><Month>5</Month><Day>8</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2016</Year><Month>5</Month><Day>1</Day><Hour>0</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2016</Year><Month>5</Month><Day>1</Day><Hour>0</Hour><Minute>1</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">29732800</ArticleId><ArticleId IdType="doi">10.13287/j.1001-9332.201605.025</ArticleId></ArticleIdList></PubmedData></pubmed><affiliations><list><country><li>République populaire de Chine</li></country><settlement><li>Pékin</li></settlement></list><tree><country name="République populaire de Chine"><noRegion><name sortKey="Luo, Chao" sort="Luo, Chao" uniqKey="Luo C" first="Chao" last="Luo">Chao Luo</name></noRegion><name sortKey="Liu, Wen Na" sort="Liu, Wen Na" uniqKey="Liu W" first="Wen Na" last="Liu">Wen Na Liu</name><name sortKey="Wang, Zi Yao" sort="Wang, Zi Yao" uniqKey="Wang Z" first="Zi Yao" last="Wang">Zi Yao Wang</name><name sortKey="Zha, Tong Gang" sort="Zha, Tong Gang" uniqKey="Zha T" first="Tong Gang" last="Zha">Tong Gang Zha</name><name sortKey="Zhu, Meng Xun" sort="Zhu, Meng Xun" uniqKey="Zhu M" first="Meng Xun" last="Zhu">Meng Xun Zhu</name><name sortKey="Zhu, Zhi Jun" sort="Zhu, Zhi Jun" uniqKey="Zhu Z" first="Zhi Jun" last="Zhu">Zhi Jun Zhu</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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