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dc.creatorCandel Pérez, Davides_ES
dc.creatorLo, Yueh-Hsines_ES
dc.creatorBlanco Vaca, Juan Antonioes_ES
dc.creatorChiu, Chih-Minges_ES
dc.creatorCamarero, Jesús Julioes_ES
dc.creatorGonzález de Andrés, Esteres_ES
dc.creatorImbert Rodríguez, Boscoes_ES
dc.creatorCastillo Martínez, Federicoes_ES
dc.date.accessioned2018-01-23T08:04:09Z
dc.date.available2018-01-23T08:04:09Z
dc.date.issued2018
dc.identifier.issn1999-4907 (Print)
dc.identifier.issn1999-4907 (Electronic)
dc.identifier.urihttps://hdl.handle.net/2454/26894
dc.description.abstractDensity is an important wood mechanical property and an indicator of xylem architecture and hydraulic conductivity. It can be influenced by forest management and climate. We studied the impact of thinning and climate variables on annual stem radial growth (ring width and ring density, and their earlywood and latewood components) in two contrasting Scots pine (Pinus sylvestris L.) stands in northern Spain (one continental, one Mediterranean). At each site, three thinning regimes (control or T0, removing 20% basal area or T20, and removing 30% or T30) were randomly applied to nine plots per site (three plots per treatment) in 1999. Thinning was repeated at the Mediterranean site in 2009 (increasing thinning intensity in T30 to 40%). Eight trees per plot were cored in spring 2014. Second thinning at the Mediterranean site and first thinning at the continental site generally caused significantly wider ring (RW), earlywood (EW) and latewood (LW) widths, although no differences between T20 and T30/40 were found, supporting in part the common observation that radial growth is enhanced following thinning as competition for water and nutrients is reduced. At the Mediterranean site, values of latewood density (LD) and maximum density (Dmax) relative to pre-thinning conditions were significantly lower in T0 than in T30. However, at the continental site, relative changes of ring density (RD) and LD were significantly higher in T0 than in T20 and T30. Climate significantly affected not only RWbut also RD, with significant RD drops during or right after unusually warm-dry years (e.g., 2003, 2011), which were characterized by LD reductions between 5.4 and 8.0%. Such RD decreases were quickly followed by recovery of pre-drought density values. These results indicate trees temporarily reduce LD as a way to enhance hydraulic conductivity during dry summers. However, climate effects on wood density were site-dependent. We also detected that the thinning effect was not intense enough to prevent drought-induced changes in wood density by altering water availability, but it could help to reduce wood properties fluctuations and therefore maintain more homogeneous wood mechanic features.en
dc.description.sponsorshipE.G.A. was funded through a Spanish Predoctoral Research Grant (ref. BES-2013-066705). Funding for this research has been provided by the Spanish Ministry of Economy and Competitiveness (project AGL2012-33465), which also funded Y.-H.L. J.A.B. was funded through a Ramón y Cajal contract (ref. RYC-2011-08082) and a Marie Curie Action (ref CIG-2012-326718-ECOPYREN3), which also funded D.C.-P. Funds to cover the costs of publishing in open access were provided by the OpenAIRE pilot program of the European Union 7th Framework Programme.en
dc.format.mimetypeapplication/pdfen
dc.language.isoengen
dc.publisherMDPIen
dc.relation.ispartofForests 2018, 9 (1), 4en
dc.rights© 2018 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.en
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectDendroecologyen
dc.subjectScots pineen
dc.subjectTree-ring widthen
dc.subjectWood densityen
dc.subjectX-rayen
dc.subjectDensitometryen
dc.subjectDroughten
dc.titleDrought-induced changes in wood density are not prevented by thinning in Scots pine standsen
dc.typeArtículo / Artikuluaes
dc.typeinfo:eu-repo/semantics/articleen
dc.contributor.departmentCiencias del Medio Naturales_ES
dc.contributor.departmentNatura Ingurunearen Zientziakeu
dc.rights.accessRightsAcceso abierto / Sarbide irekiaes
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen
dc.identifier.doi10.3390/f9010004
dc.relation.projectIDinfo:eu-repo/grantAgreement/European Commission/FP7/326718en
dc.relation.projectIDinfo:eu-repo/grantAgreement/MINECO//AGL2012-33465/ES/en
dc.relation.publisherversionhttps://doi.org/10.3390/f9010004
dc.type.versionVersión publicada / Argitaratu den bertsioaes
dc.type.versioninfo:eu-repo/semantics/publishedVersionen


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© 2018 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.
La licencia del ítem se describe como © 2018 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.

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