Higher soil capacity of intercepting heavy rainfall in mixed stands than in pure stands in riparian forests.
Identifieur interne : 000910 ( Main/Exploration ); précédent : 000909; suivant : 000911Higher soil capacity of intercepting heavy rainfall in mixed stands than in pure stands in riparian forests.
Auteurs : Beibei Zhang [République populaire de Chine] ; Qing Xu [République populaire de Chine] ; Deqiang Gao [République populaire de Chine] ; Chunwu Jiang [République populaire de Chine] ; Futing Liu [République populaire de Chine] ; Jing Jiang [Canada] ; Yingbin Ma [République populaire de Chine]Source :
- The Science of the total environment [ 1879-1026 ] ; 2019.
Descripteurs français
- KwdFr :
- MESH :
- Wicri :
- geographic : République populaire de Chine.
English descriptors
- KwdEn :
- MESH :
Abstract
Changes in global precipitation patterns would make wet regions more humid and extreme precipitation events occur frequently, followed by widespread flooding. Riparian forests are more capable of withstanding floods than inland forests because they are frequently exposed to short-term flooding events. Although many previous studies have investigated the soil water dynamics of terrestrial forests, little is known about how the soil water of riparian forests responds to different amounts of rainfall and which factors mainly regulate the soil water-holding capacity. Here, we employed stable hydrogen isotope to explore the contribution of different magnitudes of rainfall (7.9, 18.6 and 34.1 mm) to the soil water in two types of riparian forests (pure vs. mixed stand of Populus deltoides) in the middle-lower reaches of the Yangtze River, China. We further used structure equation modelling to determine the relative importance of soil properties and vegetation biomass in affecting the contribution of different magnitudes of rainfall to soil water. Our results revealed that there was no significant difference between these two stand types in the contributions of light and moderate rainfall to soil water, while the contribution of heavy rainfall to soil water (CHRSW) in mixed stand was significantly higher than that in pure stand (74.3% vs. 62.9%), suggesting that mixed stand soil has higher water-holding capacity than pure stand soil. Furthermore, soil properties were the best predictor affecting CHRSW, which explained 68% and 59% of the variation in the CHRSW on the 1st and 8th days after rainfall, respectively. Moreover, the root biomass could indirectly affect the CHRSW. Overall, mixed stand soil had a greater capacity in intercepting and storing rainwater than pure stand soil, implying that the mixed stand plantation, rather than the pure stand, should be recommended in riparian forest restoration projects that aim to improve their capacity for alleviating floods.
DOI: 10.1016/j.scitotenv.2018.12.171
PubMed: 30678009
Affiliations:
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Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China; Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200</wicri:regionArea><wicri:noRegion>Dengkou 015200</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">PubMed</idno><date when="2019">2019</date><idno type="RBID">pubmed:30678009</idno><idno type="pmid">30678009</idno><idno type="doi">10.1016/j.scitotenv.2018.12.171</idno><idno type="wicri:Area/Main/Corpus">000A69</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Corpus" wicri:corpus="PubMed">000A69</idno><idno type="wicri:Area/Main/Curation">000A69</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Curation">000A69</idno><idno type="wicri:Area/Main/Exploration">000A69</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en">Higher soil capacity of intercepting heavy rainfall in mixed stands than in pure stands in riparian forests.</title><author><name sortKey="Zhang, Beibei" sort="Zhang, Beibei" uniqKey="Zhang B" first="Beibei" last="Zhang">Beibei Zhang</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Xu, Qing" sort="Xu, Qing" uniqKey="Xu Q" first="Qing" last="Xu">Qing Xu</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China. Electronic address: xuqing@caf.ac.cn.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Gao, Deqiang" sort="Gao, Deqiang" uniqKey="Gao D" first="Deqiang" last="Gao">Deqiang Gao</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Jiang, Chunwu" sort="Jiang, Chunwu" uniqKey="Jiang C" first="Chunwu" last="Jiang">Chunwu Jiang</name><affiliation wicri:level="1"><nlm:affiliation>Anhui Academy of Forestry, Hefei 230001, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Anhui Academy of Forestry, Hefei 230001</wicri:regionArea><placeName><settlement type="city">Hefei</settlement><region type="province">Anhui</region></placeName></affiliation></author><author><name sortKey="Liu, Futing" sort="Liu, Futing" uniqKey="Liu F" first="Futing" last="Liu">Futing Liu</name><affiliation wicri:level="1"><nlm:affiliation>State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China; University of Chinese Academy of Sciences, Beijing 100049, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China; University of Chinese Academy of Sciences, Beijing 100049</wicri:regionArea><placeName><settlement type="city">Pékin</settlement></placeName></affiliation></author><author><name sortKey="Jiang, Jing" sort="Jiang, Jing" uniqKey="Jiang J" first="Jing" last="Jiang">Jing Jiang</name><affiliation wicri:level="4"><nlm:affiliation>University of Calgary, Calgary T2N1N4, Canada.</nlm:affiliation><country xml:lang="fr">Canada</country><wicri:regionArea>University of Calgary, Calgary T2N1N4</wicri:regionArea><placeName><settlement type="city">Calgary</settlement><region type="state">Alberta</region></placeName><orgName type="university">Université de Calgary</orgName><placeName><settlement type="city">Calgary</settlement><region type="state">Alberta</region></placeName></affiliation></author><author><name sortKey="Ma, Yingbin" sort="Ma, Yingbin" uniqKey="Ma Y" first="Yingbin" last="Ma">Yingbin Ma</name><affiliation wicri:level="1"><nlm:affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China; Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China; Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200</wicri:regionArea><wicri:noRegion>Dengkou 015200</wicri:noRegion></affiliation></author></analytic><series><title level="j">The Science of the total environment</title><idno type="eISSN">1879-1026</idno><imprint><date when="2019" type="published">2019</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Biomass (MeSH)</term><term>Biota (MeSH)</term><term>China (MeSH)</term><term>Forests (MeSH)</term><term>Groundwater (analysis)</term><term>Liquidambar (physiology)</term><term>Populus (physiology)</term><term>Rain (MeSH)</term><term>Soil (chemistry)</term><term>Taxodium (physiology)</term><term>Trees (physiology)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Arbres (physiologie)</term><term>Biomasse (MeSH)</term><term>Biote (MeSH)</term><term>Chine (MeSH)</term><term>Forêts (MeSH)</term><term>Liquidambar (physiologie)</term><term>Nappe phréatique (analyse)</term><term>Pluie (MeSH)</term><term>Populus (physiologie)</term><term>Sol (composition chimique)</term><term>Taxodium (physiologie)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="chemistry" xml:lang="en"><term>Soil</term></keywords><keywords scheme="MESH" type="geographic" xml:lang="en"><term>China</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Nappe phréatique</term></keywords><keywords scheme="MESH" qualifier="analysis" xml:lang="en"><term>Groundwater</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Sol</term></keywords><keywords scheme="MESH" qualifier="physiologie" xml:lang="fr"><term>Arbres</term><term>Liquidambar</term><term>Populus</term><term>Taxodium</term></keywords><keywords scheme="MESH" qualifier="physiology" xml:lang="en"><term>Liquidambar</term><term>Populus</term><term>Taxodium</term><term>Trees</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Biomass</term><term>Biota</term><term>Forests</term><term>Rain</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Biomasse</term><term>Biote</term><term>Chine</term><term>Forêts</term><term>Pluie</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>République populaire de Chine</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Changes in global precipitation patterns would make wet regions more humid and extreme precipitation events occur frequently, followed by widespread flooding. Riparian forests are more capable of withstanding floods than inland forests because they are frequently exposed to short-term flooding events. Although many previous studies have investigated the soil water dynamics of terrestrial forests, little is known about how the soil water of riparian forests responds to different amounts of rainfall and which factors mainly regulate the soil water-holding capacity. Here, we employed stable hydrogen isotope to explore the contribution of different magnitudes of rainfall (7.9, 18.6 and 34.1 mm) to the soil water in two types of riparian forests (pure vs. mixed stand of Populus deltoides) in the middle-lower reaches of the Yangtze River, China. We further used structure equation modelling to determine the relative importance of soil properties and vegetation biomass in affecting the contribution of different magnitudes of rainfall to soil water. Our results revealed that there was no significant difference between these two stand types in the contributions of light and moderate rainfall to soil water, while the contribution of heavy rainfall to soil water (CHRSW) in mixed stand was significantly higher than that in pure stand (74.3% vs. 62.9%), suggesting that mixed stand soil has higher water-holding capacity than pure stand soil. Furthermore, soil properties were the best predictor affecting CHRSW, which explained 68% and 59% of the variation in the CHRSW on the 1st and 8th days after rainfall, respectively. Moreover, the root biomass could indirectly affect the CHRSW. Overall, mixed stand soil had a greater capacity in intercepting and storing rainwater than pure stand soil, implying that the mixed stand plantation, rather than the pure stand, should be recommended in riparian forest restoration projects that aim to improve their capacity for alleviating floods.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">30678009</PMID><DateCompleted><Year>2019</Year><Month>02</Month><Day>26</Day></DateCompleted><DateRevised><Year>2019</Year><Month>02</Month><Day>26</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1879-1026</ISSN><JournalIssue CitedMedium="Internet"><Volume>658</Volume><PubDate><Year>2019</Year><Month>Mar</Month><Day>25</Day></PubDate></JournalIssue><Title>The Science of the total environment</Title><ISOAbbreviation>Sci Total Environ</ISOAbbreviation></Journal><ArticleTitle>Higher soil capacity of intercepting heavy rainfall in mixed stands than in pure stands in riparian forests.</ArticleTitle><Pagination><MedlinePgn>1514-1522</MedlinePgn></Pagination><ELocationID EIdType="pii" ValidYN="Y">S0048-9697(18)35016-2</ELocationID><ELocationID EIdType="doi" ValidYN="Y">10.1016/j.scitotenv.2018.12.171</ELocationID><Abstract><AbstractText>Changes in global precipitation patterns would make wet regions more humid and extreme precipitation events occur frequently, followed by widespread flooding. Riparian forests are more capable of withstanding floods than inland forests because they are frequently exposed to short-term flooding events. Although many previous studies have investigated the soil water dynamics of terrestrial forests, little is known about how the soil water of riparian forests responds to different amounts of rainfall and which factors mainly regulate the soil water-holding capacity. Here, we employed stable hydrogen isotope to explore the contribution of different magnitudes of rainfall (7.9, 18.6 and 34.1 mm) to the soil water in two types of riparian forests (pure vs. mixed stand of Populus deltoides) in the middle-lower reaches of the Yangtze River, China. We further used structure equation modelling to determine the relative importance of soil properties and vegetation biomass in affecting the contribution of different magnitudes of rainfall to soil water. Our results revealed that there was no significant difference between these two stand types in the contributions of light and moderate rainfall to soil water, while the contribution of heavy rainfall to soil water (CHRSW) in mixed stand was significantly higher than that in pure stand (74.3% vs. 62.9%), suggesting that mixed stand soil has higher water-holding capacity than pure stand soil. Furthermore, soil properties were the best predictor affecting CHRSW, which explained 68% and 59% of the variation in the CHRSW on the 1st and 8th days after rainfall, respectively. Moreover, the root biomass could indirectly affect the CHRSW. Overall, mixed stand soil had a greater capacity in intercepting and storing rainwater than pure stand soil, implying that the mixed stand plantation, rather than the pure stand, should be recommended in riparian forest restoration projects that aim to improve their capacity for alleviating floods.</AbstractText><CopyrightInformation>Copyright © 2018 Elsevier B.V. All rights reserved.</CopyrightInformation></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Zhang</LastName><ForeName>Beibei</ForeName><Initials>B</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Xu</LastName><ForeName>Qing</ForeName><Initials>Q</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China. Electronic address: xuqing@caf.ac.cn.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Gao</LastName><ForeName>Deqiang</ForeName><Initials>D</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Jiang</LastName><ForeName>Chunwu</ForeName><Initials>C</Initials><AffiliationInfo><Affiliation>Anhui Academy of Forestry, Hefei 230001, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Liu</LastName><ForeName>Futing</ForeName><Initials>F</Initials><AffiliationInfo><Affiliation>State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China; University of Chinese Academy of Sciences, Beijing 100049, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Jiang</LastName><ForeName>Jing</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>University of Calgary, Calgary T2N1N4, Canada.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Ma</LastName><ForeName>Yingbin</ForeName><Initials>Y</Initials><AffiliationInfo><Affiliation>Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China; Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200, China.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2018</Year><Month>12</Month><Day>12</Day></ArticleDate></Article><MedlineJournalInfo><Country>Netherlands</Country><MedlineTA>Sci Total Environ</MedlineTA><NlmUniqueID>0330500</NlmUniqueID><ISSNLinking>0048-9697</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D012987">Soil</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D018533" MajorTopicYN="Y">Biomass</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D058448" MajorTopicYN="Y">Biota</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D002681" MajorTopicYN="N" Type="Geographic">China</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D065928" MajorTopicYN="Y">Forests</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D060587" MajorTopicYN="N">Groundwater</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D031317" MajorTopicYN="N">Liquidambar</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="N">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="N">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D011891" MajorTopicYN="Y">Rain</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="N">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032489" MajorTopicYN="N">Taxodium</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="N">physiology</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D014197" MajorTopicYN="Y">Trees</DescriptorName><QualifierName UI="Q000502" MajorTopicYN="N">physiology</QualifierName></MeshHeading></MeshHeadingList><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">Different magnitudes of rainfall</Keyword><Keyword MajorTopicYN="N">Riparian forests</Keyword><Keyword MajorTopicYN="N">Soil properties</Keyword><Keyword MajorTopicYN="N">Soil water-holding capacity</Keyword><Keyword MajorTopicYN="N">Stable hydrogen isotope</Keyword><Keyword MajorTopicYN="N">Vegetation biomass</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2018</Year><Month>08</Month><Day>22</Day></PubMedPubDate><PubMedPubDate PubStatus="revised"><Year>2018</Year><Month>12</Month><Day>11</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2018</Year><Month>12</Month><Day>11</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2019</Year><Month>1</Month><Day>26</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2019</Year><Month>1</Month><Day>27</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2019</Year><Month>2</Month><Day>27</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">30678009</ArticleId><ArticleId IdType="pii">S0048-9697(18)35016-2</ArticleId><ArticleId IdType="doi">10.1016/j.scitotenv.2018.12.171</ArticleId></ArticleIdList></PubmedData></pubmed><affiliations><list><country><li>Canada</li><li>République populaire de Chine</li></country><region><li>Alberta</li><li>Anhui</li></region><settlement><li>Calgary</li><li>Hefei</li><li>Pékin</li></settlement><orgName><li>Université de Calgary</li></orgName></list><tree><country name="République populaire de Chine"><noRegion><name sortKey="Zhang, Beibei" sort="Zhang, Beibei" uniqKey="Zhang B" first="Beibei" last="Zhang">Beibei Zhang</name></noRegion><name sortKey="Gao, Deqiang" sort="Gao, Deqiang" uniqKey="Gao D" first="Deqiang" last="Gao">Deqiang Gao</name><name sortKey="Jiang, Chunwu" sort="Jiang, Chunwu" uniqKey="Jiang C" first="Chunwu" last="Jiang">Chunwu Jiang</name><name sortKey="Liu, Futing" sort="Liu, Futing" uniqKey="Liu F" first="Futing" last="Liu">Futing Liu</name><name sortKey="Ma, Yingbin" sort="Ma, Yingbin" uniqKey="Ma Y" first="Yingbin" last="Ma">Yingbin Ma</name><name sortKey="Xu, Qing" sort="Xu, Qing" uniqKey="Xu Q" first="Qing" last="Xu">Qing Xu</name></country><country name="Canada"><region name="Alberta"><name sortKey="Jiang, Jing" sort="Jiang, Jing" uniqKey="Jiang J" first="Jing" last="Jiang">Jing Jiang</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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