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Cross-site patterns in the response of Eucalyptus plantations to irrigation, climate and intra-annual weather variation

dc.contributor.authorRyan, Michael G.
dc.contributor.authorStape, José Luiz [UNESP]
dc.contributor.authorBinkley, Dan
dc.contributor.authorAlvares, Clayton A. [UNESP]
dc.contributor.institutionColorado State University
dc.contributor.institutionRocky Mountain Research Station
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionForestry Science and Research Institute (IPEF)
dc.contributor.institutionNorthern Arizona University
dc.date.accessioned2020-12-12T01:33:53Z
dc.date.available2020-12-12T01:33:53Z
dc.date.issued2020-11-01
dc.description.abstractCross-site patterns for multiple sites tend to be more broadly applicable and more useful for constructing and constraining models. We examined cross-site patterns of Eucalyptus plantation response to water supply (including irrigation and 1/3 precipitation removal), mean annual temperature (MAT), vapor pressure deficit during the daytime (VPD), and nutrient addition in eight sites from the Brazil Eucalyptus Productivity Project (BEPP). Mean annual increment (MAI) for all treatments and sites varied from 12.7 to 37.3 Mg ha−1 yr−1 across a 1400 km latitudinal gradient where annual precipitation varied from 940 to 1430 mm yr−1. MAI varied with water added across all sites, with a near linear increase of 1.42 Mg ha−1 yr−1 per 100 mm yr−1 between 640 and 1800 mm yr−1, a MAI plateau of 30.8 Mg ha−1 yr−1 at ~2000 mm yr−1, then decreasing to MAI of 27.2 Mg ha−1 yr−1 at 3060 mm yr−1. Including MAT with the water response showed that MAI decreased at 1.23 Mg ha−1 yr−1 per °C. For the natural precipitation treatments, MAI decreased at 2.52 Mg ha−1 yr−1 per °C, comparable to that for the much broader TECHS Project (Binkley et al., 2020). MAI was not related to temperature for the irrigation treatments, suggesting that some or all of the response of MAI to temperature is related to water supply. The difference between the biomass of the irrigation treatments and that of natural precipitation treatment slowed its increase or stopped increasing at age 30–60 months for five of the eight sites, but increased through the study duration for the other three sites. The difference in biomass between the fertilization and no fertilization treatments increased throughout the study for two sites. Three- and six-month growth was generally unrelated prior 3–12 month weather. Age-related decline was observed for all of the treatments at four of the eight sites. These cross-site comparisons affirm that water supply is the key resource determining levels of plantation productivity in Brazil and that individual site studies are inadequate for understanding many key responses.en
dc.description.affiliationDepartment of Ecosystem Science & Sustainability Colorado State University
dc.description.affiliationUSDA Forest Service Rocky Mountain Research Station
dc.description.affiliationDepartment of Forest Science São Paulo State University – UNESP
dc.description.affiliationForestry Science and Research Institute (IPEF)
dc.description.affiliationSchool of Forestry Northern Arizona University
dc.description.affiliationUnespDepartment of Forest Science São Paulo State University – UNESP
dc.description.sponsorshipInternational Paper
dc.identifierhttp://dx.doi.org/10.1016/j.foreco.2020.118444
dc.identifier.citationForest Ecology and Management, v. 475.
dc.identifier.doi10.1016/j.foreco.2020.118444
dc.identifier.issn0378-1127
dc.identifier.scopus2-s2.0-85089027960
dc.identifier.urihttp://hdl.handle.net/11449/199216
dc.language.isoeng
dc.relation.ispartofForest Ecology and Management
dc.sourceScopus
dc.subjectAge-related decline
dc.subjectForest production ecology
dc.subjectGrowth response to water
dc.subjectIrrigation
dc.subjectNutrition
dc.subjectTemperature
dc.subjectVapor pressure deficit
dc.titleCross-site patterns in the response of Eucalyptus plantations to irrigation, climate and intra-annual weather variationen
dc.typeArtigo
dspace.entity.typePublication
unesp.author.orcid0000-0002-2500-6738 0000-0002-2500-6738[1]
unesp.author.orcid0000-0001-7731-6327[4]

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