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...
Main Authors: | , , |
---|---|
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 |
id |
doaj-b38ae1222ad843dc8d39dde750b8edba |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT niltoncuri solosdetabuleiroscosteirossobflorestasnaturaisesobcultivo AT josecoelhodearaujofilho solosdetabuleiroscosteirossobflorestasnaturaisesobcultivo AT joaoboscovasconcellosgomes solosdetabuleiroscosteirossobflorestasnaturaisesobcultivo |
_version_ |
1725517529430884352 |