Use este identificador para citar ou linkar para este item: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1110454
Registro completo de metadados
Campo DCValorIdioma
dc.contributor.authorSILVA, G. A. daeng
dc.contributor.authorCAMÊLO, D. de L.eng
dc.contributor.authorCORRÊA, M. M.eng
dc.contributor.authorSOUZA JÚNIOR, V. S. deeng
dc.contributor.authorRIBEIRO FILHO, M. R.eng
dc.contributor.authorARAUJO FILHO, J. C. deeng
dc.date.accessioned2019-07-09T00:44:49Z-
dc.date.available2019-07-09T00:44:49Z-
dc.date.created2019-07-08
dc.date.issued2019
dc.identifier.citationRevista Caatinga, v. 32, n. 2, p. 458-471, abr./jun. 2019.eng
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1110454-
dc.descriptionSmall variations of relief may change drainage and runoff and hence promote the formation of sandy surface horizons and hardened subsurface horizons (fragipans and/or duripans) in Coastal Tablelands soils. This study aimed to investigate the pedogenesis on Coastal Tablelands area with low range altimetry in Paraíba state; secondly, we also sought to contribute to the improvement of the Brazilian Soil Classification System (BSCS). Four soil profiles ware described and collected to be submitted to routine physical and chemical analysis, determination of Fe, Al and Si extracted by sulfuric acid digestion, sodium citrate-bicarbonate-dithionite and acid ammonium oxalate, sodium pyrophosphate, and mineralogical analysis in the sand and clay fractions by X-ray diffractometry. Optical density of the oxalate extract (ODOE) was also determined; the results were statistically evaluated using the R software. Microrelief variations conditioning differentiated water flows, along with the sandy texture of the surface horizons (A and E) and the lower coarse sand/fine sand ratio in the subsurface horizon, seem to promote clay accumulation in depth in the Spodosols developed on Coastal Tablelands environments. For this soils, the argilluvic (argissólico) character at the subgroup level of the BSCS should be incorporated. In addition, Al amorphous mineral phases and/or poorly crystalline play an important role in the formation of strongly cemented horizons (duripans) of the Spodosols, as also reported by other authors. Finally, the ODOE showed to be an efficient indicator of soils under podzolization process, being possible its use as a taxonomic criterion for classification of Spodosols by the BSCS.eng
dc.language.isoengeng
dc.rightsopenAccesseng
dc.titlePedogenesis on coastal tablelands area with low range altimetry in Paraíba state.eng
dc.typeArtigo de periódicoeng
dc.date.updated2019-11-08T11:11:11Z
dc.subject.thesagroPodzólicoeng
dc.subject.thesagroHorizonteeng
dc.subject.nalthesaurusFormica podzolicaeng
dc.subject.nalthesaurusKaoliniteeng
dc.subject.nalthesaurusSoil horizonseng
riaa.ainfo.id1110454eng
riaa.ainfo.lastupdate2019-11-08 -02:00:00
dc.identifier.doihttps://doi.org/10.1590/1983-21252019v32n219rceng
dc.contributor.institutionGIVANILDO ALVES DA SILVA, UFRPE; DANILO DE LIMA CAMÊLO, UFES; MARCELO METRI CORRÊA, UFRPE; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UFRPE; MATEUS ROSAS RIBEIRO FILHO, UFRPE; JOSE COELHO DE ARAUJO FILHO, CNPS.eng
Aparece nas coleções:Artigo em periódico indexado (CNPS)

Arquivos associados a este item:
Arquivo Descrição TamanhoFormato 
2019025.pdf1,26 MBAdobe PDFThumbnail
Visualizar/Abrir
Mostrar registro simples do item Visualizar estatísticas

FacebookTwitterDeliciousLinkedInGoogle BookmarksMySpace