Land Use and Changes in Soil Morphology and Physical-Chemical Properties in Southern Amazon

dc.contributor.authorMelo, Vander Freitas
dc.contributor.authorOrrutéa, Alessandro Góis
dc.contributor.authorMotta, Antônio Carlos Vargas
dc.contributor.authorTestoni, Samara Alves
dc.date.accessioned2024-07-08T22:04:41Z
dc.date.available2024-07-08T22:04:41Z
dc.date.issued2017
dc.description.abstractMany Amazonian farmers use the slash-and-burn method rather than fertilization for crop production. The aim of the present study was to evaluate changes in the morphological, physical, and chemical properties of naturally fertile Inceptisols after conversion from native forest to different uses in southern Amazonia, Brazil. Land covered by dense native forest (NF) was split into four areas of 1.0 ha each. Three areas were slashed and burned and then cultivated for 11 years with coffee (CO), secondary forest (SF), and pasture (PA). Four soil profiles were sampled in each treatment (four uses × four replicates). The mean value distribution of each physical and chemical analysis was determined for different depths, and standard error bars were placed to display significant differences among treatments. Results showed that morphology and physical properties were negatively affected after the establishment of PA and CO: a reduction in the thickness of the A horizon and in aggregate stability, a decrease in total porosity and macroporosity, and an increase in aggregate size and bulk density. Soil bulk density (SBD), geometric mean diameter of water-stable aggregates (GMD), and microporosity (SMi) were higher in soil under pasture as a consequence of more intense soil surface compaction. Native and secondary forests were the only treatments that showed granular structures in the A horizon. Significant differences between native forest and secondary forest were mainly found in the top soil layer for total porosity (STP) (NF>SF), macroporosity (SMa) (NF>SF), SBD (NF>SF) and GMD (SF>NF). Phosphorus contents in the A horizon increased from 6.2 to 21.5 mg kg-1 in PA and to 27.2 mg kg-1 in SF. Soil under coffee cultivation exhibited the lowest levels of Ca2+ and sum of bases in surface horizons. In all slash-and-burn areas there was a reduction in the C stock (Mg ha-1) of the A horizon: native forest 6.3, secondary forest 4.5, pasture 3.3, and coffee 3.1.pt_BR
dc.formatpdfpt_BR
dc.identifier.citationMELO, V. F. et al. Land Use and Changes in Soil Morphology and Physical-Chemical Properties in Southern Amazon. Revista Brasileira de Ciência do Solo, Viçosa, v. 41, p. e0170034, 16 feb. 2017.pt_BR
dc.identifier.issn1806-9657
dc.identifier.urihttps://doi.org/10.1590/18069657rbcs20170034pt_BR
dc.identifier.urihttp://www.sbicafe.ufv.br/handle/123456789/14417
dc.language.isoenpt_BR
dc.publisherSociedade Brasileira de Ciência do Solopt_BR
dc.relation.ispartofseriesRevista Brasileira de Ciência do Solo;41, e0170034, 2017
dc.rightsOpen Accesspt_BR
dc.subjectSecondary forestpt_BR
dc.subjectCoffeept_BR
dc.subjectPasturept_BR
dc.subjectSlash and burnpt_BR
dc.subjectAsh effectpt_BR
dc.subject.classificationCafeicultura::Agroclimatologia e fisiologiapt_BR
dc.titleLand Use and Changes in Soil Morphology and Physical-Chemical Properties in Southern Amazonpt_BR
dc.typeArtigopt_BR

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