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dc.contributor.authorKrainovic, Pedro Medrado-
dc.contributor.authorBastos, Rodrigo Pinheiro-
dc.contributor.authorAlmeida, Danilo Roberti Alves de-
dc.contributor.authorNeves Junior, Afrânio Ferreira-
dc.contributor.authorSampaio, Paulo de Tarso Barbosa-
dc.contributor.authorSouza, Luiz Augusto Gomes de-
dc.contributor.authorFalcão, Newton P.S.-
dc.date.accessioned2020-05-14T15:32:07Z-
dc.date.available2020-05-14T15:32:07Z-
dc.date.issued2020-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/15472-
dc.description.abstractRosewood (Aniba rosaeodora Ducke) is an endangered Amazonian tree species that produces a commercially valuable essential oil, used mainly in cosmetics and fine fragrances production. The species can also be used in reforestation programs, which generate jobs and as a source of income and reduce the pressure of exploitation on natural rosewood populations. The objective of this study was to verify the influence of rosewood stands on physical and chemical soil attributes. This study was conducted at a rural farm in the Maués municipality, 350 km from Manaus, Amazonas State, Brazil. Samples were collected in five areas; 4-, 10- and 20-year-old rosewood stands, and 15- and 60-year-old secondary forests. The latter two served as control treatments, reflecting natural spontaneous succession conditions over time. Soil was sampled at 10 equidistant points within each area to measure physicochemical attributes, and at the center of each one, a soil profile was dug for description and classification of morphological characteristics. Based on the profile description, the soils were classified as Xanthic Hapludox. The results show that soil conditions under 20-year-old rosewood stand resembled those beneath the 60-year-old secondary forest, and likewise for the soil under the 10-year-old rosewood stand and the 15-year-old secondary forest. The soil bulk density ranged from 0.81 to 0.99 g cm−3 among all areas and no significant difference was found (P = 0.052). With exception to 4-year-old stand, the organic matter (2.68–5.87%) and carbon stock (18.57–31.71 Mg ha−1) did not differ significantly between stands and control treatments. For the soil macronutrients, nitrogen (0.10–0.22%), phosphorus (1.17–11.70 mg kg−1), calcium (0.03–0.31 mg kg−1) and magnesium (0.02–0.16 mg kg−1) were higher or equal in the rosewood stands in comparison to the two controls, while the potassium values (0.03–0.36 mg kg−1) were significantly higher in 60-year-old secondary forests only compared to the 10-year-old rosewood stands (P = 0.005). The soil beneath the 4-year-old rosewood stand, however, differed from the other four areas, having significantly higher natural clay content (>600 g kg−1) and higher topsoil chemical concentrations, associated with the more recent burning. This result represents the first step in addressing concern about sustainable soil use in rosewood forestry economics. Consequently, this kind of rosewood plantation can be recommended as an appropriate use of historically exploited areas, providing economic return from local biodiversity. © 2019 Elsevier B.V.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 357pt_BR
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Brazil*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/br/*
dc.subjectBiodiversityen
dc.subjectConservationen
dc.subjectEssential Oilsen
dc.subjectReforestationen
dc.subjectSoilsen
dc.subjectAmazon Planted Foresten
dc.subjectEndangered Treesen
dc.subjectRecovery Areasen
dc.subjectSilvicultureen
dc.subjectSpecies Conservationsen
dc.subjectWooden
dc.subjectChronosequenceen
dc.subjectCommercial Activityen
dc.subjectEndangered Speciesen
dc.subjectForest Soilen
dc.subjectOld-growth Foresten
dc.subjectPlantationen
dc.subjectRecovery Planen
dc.subjectReforestationen
dc.subjectSecondary Foresten
dc.subjectSilvicultureen
dc.subjectSoil Analysisen
dc.subjectSpecies Conservationsen
dc.subjectAmazonasen
dc.subjectManausen
dc.subjectAniba Rosaeodoraen
dc.titleEffect of rosewood plantation chronosequence on soil attributes in Central Amazoniaen
dc.typeArtigopt_BR
dc.identifier.doi10.1016/j.geoderma.2019.113952-
dc.publisher.journalGeodermapt_BR
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