Solos de tabuleiros costeiros sob florestas naturais e sob cultivo

Landscapes formed on Barreiras Formation sediments occupy significant area on Brazilian territory. Many of these landscapes have highly intensive agricultural use, due to favorable climate and topography. The objective of this study was to characterize and to compare soil profiles situated on non-di...

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Main Authors: Nilton Curi, José Coelho de Araújo Filho, João Bosco Vasconcellos Gomes
Format: Article
Language:English
Published: Embrapa Florestas 2012-09-01
Series:Pesquisa Florestal Brasileira
Subjects:
Online Access:http://www.cnpf.embrapa.br/pfb/index.php/pfb/article/view/324/pdf
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spelling doaj-b38ae1222ad843dc8d39dde750b8edba2020-11-24T23:38:13ZengEmbrapa FlorestasPesquisa Florestal Brasileira1809-36471983-26052012-09-013271233246Solos de tabuleiros costeiros sob florestas naturais e sob cultivoNilton CuriJosé Coelho de Araújo FilhoJoão Bosco Vasconcellos GomesLandscapes formed on Barreiras Formation sediments occupy significant area on Brazilian territory. Many of these landscapes have highly intensive agricultural use, due to favorable climate and topography. The objective of this study was to characterize and to compare soil profiles situated on non-dissected coastal plains from southern Bahia to Alagoas, occurring under natural vegetation (forest) and agricultural use. Seven soil profiles were analyzed and data from six soil profiles obtained in other works were incorporated. Particle size distribution, organic C (OC), Al, Ca, Mg, Al+H, K, Na, P, Fe, Ti and Si were determined. Clay mineralogy was analyzed by X-ray diffraction. Soil profiles occur on flat relief, have yellow color, weak small to medium subangular blocky structure on B horizon and sub-superficial cohesive character. Texture was the most significant attribute that differentiated soil profiles from each other. All soils have low Fe content. X-ray diffraction results showed kaolinite dominance in the clay fraction. The soil OC was the only attribute tested that significantly varied between the surface materials of forest soils and the cultivated systems (sugarcane, orange, coconut and eucalyptus).http://www.cnpf.embrapa.br/pfb/index.php/pfb/article/view/324/pdfCohesive characterBarreiras FormationKaolinite
collection DOAJ
language English
format Article
sources DOAJ
author Nilton Curi
José Coelho de Araújo Filho
João Bosco Vasconcellos Gomes
spellingShingle Nilton Curi
José Coelho de Araújo Filho
João Bosco Vasconcellos Gomes
Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
Pesquisa Florestal Brasileira
Cohesive character
Barreiras Formation
Kaolinite
author_facet Nilton Curi
José Coelho de Araújo Filho
João Bosco Vasconcellos Gomes
author_sort Nilton Curi
title Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
title_short Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
title_full Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
title_fullStr Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
title_full_unstemmed Solos de tabuleiros costeiros sob florestas naturais e sob cultivo
title_sort solos de tabuleiros costeiros sob florestas naturais e sob cultivo
publisher Embrapa Florestas
series Pesquisa Florestal Brasileira
issn 1809-3647
1983-2605
publishDate 2012-09-01
description Landscapes formed on Barreiras Formation sediments occupy significant area on Brazilian territory. Many of these landscapes have highly intensive agricultural use, due to favorable climate and topography. The objective of this study was to characterize and to compare soil profiles situated on non-dissected coastal plains from southern Bahia to Alagoas, occurring under natural vegetation (forest) and agricultural use. Seven soil profiles were analyzed and data from six soil profiles obtained in other works were incorporated. Particle size distribution, organic C (OC), Al, Ca, Mg, Al+H, K, Na, P, Fe, Ti and Si were determined. Clay mineralogy was analyzed by X-ray diffraction. Soil profiles occur on flat relief, have yellow color, weak small to medium subangular blocky structure on B horizon and sub-superficial cohesive character. Texture was the most significant attribute that differentiated soil profiles from each other. All soils have low Fe content. X-ray diffraction results showed kaolinite dominance in the clay fraction. The soil OC was the only attribute tested that significantly varied between the surface materials of forest soils and the cultivated systems (sugarcane, orange, coconut and eucalyptus).
topic Cohesive character
Barreiras Formation
Kaolinite
url http://www.cnpf.embrapa.br/pfb/index.php/pfb/article/view/324/pdf
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