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dc.contributor.authorMENDONÇA, B. A. F. de
dc.contributor.authorSCHAEFER, C. E. G. R.
dc.contributor.authorFERNANDES-FILHO, E. I.
dc.contributor.authorSIMAS, F. N. B.
dc.contributor.authorAMARAL, E. F. do
dc.date.accessioned2020-09-01T04:41:32Z-
dc.date.available2020-09-01T04:41:32Z-
dc.date.created2020-08-31
dc.date.issued2020
dc.identifier.citationRevista Brasileira de Ciência do Solo, v. 44, e0200038, 2020.
dc.identifier.issn0100-0683 (print) / 1806-9657 (online)
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1124663-
dc.descriptionThe northwestern part of the Acre State (Brazil) possesses singular soils in Brazilian Amazonia, but have been very little studied. This study aimed to discuss the genesis and some micropedological aspects of the soils from Serra do Divisor and adjacent floodplain soils of the Moa river, to enhance the knowledge on their formation. A toposequence of soils ranging from the uppermost part of sub-Andean Serra do Divisor to the Alluvial soils of Moa river floodplain was studied, regarding chemical, physical, mineralogical, and micromorphological attributes. The parent material of the Serra do Divisor is basically quartzose sandstone, and the soils along the toposequence were classified as Typic Haplorthods (P1), Spodic Quartzipsamment (P2), Lithic Quartzipsamment (P3), and Lithic Quartzipsamment (P4). Along the Moa river floodplain, we also identified and collected, Typic Udifluvent (P5), Typic Kandiudult (P6), Typic Kandiudalf (P7), and Arenic Plinthic Kandiudult (P8). The Serra do Divisor soils have very low fertility, high acidity, and low cation exchange capacities, presenting a coarse sandy texture, even shallow pedons. The X-ray diffraction analysis of these soils indicates the predominance of kaolinite, with traces of quartz and gibbsite. The shallow mountain Podzols on sandstone have an expressive accumulation of organic material in surface horizons, with evidence of ferrihydrite and imogolite in the subsurface. At the Moa river floodplain, all soils are originated from recent sediments (Cenozoic), which have a geological source upstream. Varying sedimentary layers are key aspects influencing soil genesis. Those soils have evidence of 2:1 clays with hydroxyl-Al interlayers in subsurface horizons. The Serra do Divisor steep landforms and the coarse texture of the soils promote good drainage and favor leaching and chemical impoverishment. Kaolinite and gibbsite were formed by severe leaching and there are evidences of in situ neoformation of gibbsite by extreme Si losses. All studied soils have some peculiarities such as high accumulation of organic material or 2:1 clay minerals. Most investigated soils were affected by colluvial, reworking, mass movements or a strong variation on sedimentation.
dc.language.isoeng
dc.rightsopenAccesseng
dc.subjectMicropedologiaeng
dc.subjectMicropedologyeng
dc.subjectPlanície de inundaçãoeng
dc.subjectFormación del sueloeng
dc.subjectMineralogía del sueloeng
dc.subjectMateria orgánica del sueloeng
dc.subjectLlanuras sujetas a inundacioneseng
dc.subjectSerra do Divisor (AC)eng
dc.subjectRio Moa (AC)eng
dc.subjectNorthwestern Acreeng
dc.subjectAmazônia Ocidentaleng
dc.subjectWestern Amazoneng
dc.subjectAmazonia Occidentaleng
dc.titleGenesis and micropedology of soils at Serra do Divisor and Moa river floodplain, northwestern Acre, Brazilian Amazonia.
dc.typeArtigo de periódico
dc.subject.thesagroGênese do Solo
dc.subject.thesagroMineralogiaeng
dc.subject.thesagroMatéria Orgânicaeng
dc.subject.thesagroVárzeaeng
dc.subject.nalthesaurusSoil formationeng
dc.subject.nalthesaurusSoil mineralogyeng
dc.subject.nalthesaurusSoil organic mattereng
dc.subject.nalthesaurusFloodplainseng
riaa.ainfo.id1124663
riaa.ainfo.lastupdate2020-10-07 -03:00:00
dc.identifier.doi10.36783/18069657rbcs20200038
dc.contributor.institutionBruno Araujo Furtado de Mendonça, Universidade Federal Rural do Rio de Janeiro; Carlos Ernesto Gonçalves Reynaud Schaefer, Universidade Federal de Viçosa; Elpídio Inácio Fernandes-Filho, Universidade Federal de Viçosa; Felipe Nogueira Bello Simas, Universidade Federal de Viçosa; EUFRAN FERREIRA DO AMARAL, CPAF-AC.
Aparece nas coleções:Artigo em periódico indexado (CPAF-AC)

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