Quantification of aluminium in soil of the Solimões formation, Acre State, Brazil.

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dc.contributorThiago Andrade Bernini, UFRRJ; Marcos Gervasio Pereira, UFRRJ; Lúcia Helena Cunha dos Anjos, UFRRJ; DANIEL VIDAL PEREZ, CNPS; ADEMIR FONTANA, CNPS; SEBASTIAO BARREIROS CALDERANO, CNPS; PAULO GUILHERME SALVADOR WADT, CPAF-AC.
dc.creatorBERNINI, T. A.
dc.creatorPEREIRA, M. G.
dc.creatorANJOS, L. H. C. dos
dc.creatorPEREZ, D. V.
dc.creatorFONTANA, A.
dc.creatorCALDERANO, S. B.
dc.creatorWADT, P. G. S.
dc.date2014-02-28T11:11:11Z
dc.date2014-02-28T11:11:11Z
dc.date2014-02-28
dc.date2013
dc.date2019-01-10T11:11:11Z
dc.date.accessioned2026-06-30T22:48:19Z
dc.descriptionThe variety of soils in the State of Acre is wide and their chemical profiles are still not fully understood. The nature of the material of origin of these soils is indicated by the high aluminium (Al) content, commonly associated with high calcium (Ca) and magnesium (Mg) contents. The study objective was to use different methods to quantify Al in soils from toposequences formed from material of a sedimentary nature originating from the Solimões Formation, in Acre, Brazil. Trenches were opened at three distinct points in the landscape: shoulder, backslope and footslope positions. Soil samples were collected for physical, chemical, mineralogical analyses. The Al content was quantified using different methods. High Al contents were found in most of these horizons, associated with high Ca and Mg levels, representing the predominant cations in the sum of exchangeable bases. The mineralogy indicates that the soils are still in a low weathering phase, with the presence of significant quantities of 2:1 minerals. Similar Al contents were determined by the methods of NaOH titration, xylenol orange spectrometry and inductively coupled plasma optical emission spectrometry. However, no consistent data were obtained by the pyrocatechol violet method. Extraction with KCl overestimated the exchangeable Al content due to its ability to extract the non-exchangeable Al present in the smectite interlayers. It was observed that high Al contents are related to the instability of the hydroxyl-Al smectite interlayers.
dc.identifierRevista Brasileira de Ciência do Solo, Rio de Janeiro, v. 37,n. 6, p. 1441-1453, 2013.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/981532
dc.identifier.urihttp://hdl.handle.net/123456789/368450
dc.languageeng
dc.rightsopenAccess
dc.subjectAlumínio trocável
dc.subjectEsmectita
dc.subjectFormação Solimões
dc.subjectAmazônia Ocidental
dc.subjectWestern Amazon
dc.subjectAmazonia Occidental
dc.subjectQuímica del suelo
dc.subjectAluminio intercambiable
dc.subjectQuímica do solo
dc.subjectAlumínio
dc.subjectSoil chemistry
dc.subjectExchangeable aluminum
dc.titleQuantification of aluminium in soil of the Solimões formation, Acre State, Brazil.
dc.typeArtigo de periódico

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