Título:	Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil.
Autoria:	CALDAS, A. M. ROLIM NETO, F. C. PARAHYBA, R. da B. V. CORRÊA, M. M. RODRIGUES, A. de C. F.
Afiliação:	ANILDO MONTEIRO CALDAS, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; FERNANDO CARTAXO ROLIM NETO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; ROBERTO DA BOA VIAGEM PARAHYBA, CNPS; MARCUS METRI CORRÊA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; ADRIANA DE CARVALHO FIGUEIREDO RODRIGUES, INSTITUTO FEDERAL DE EDUCAÇÃO, CIÊNCIA E TECNOLOGIA DO SERTÃO PERNAMBUCANO.
Ano de publicação:	2023
Referência:	Engenharia Agrícola, v. 43, n. 4, e20230147, 2023.
Conteúdo:	In the Prata watershed there are units corresponding to the Pleistocene Terraces and the Fluvium-Lagoon Sediments. This watershed is inserted almost entirely in the area of plateaus (Tabuleiros) with altitudes of 10 to 100 meters, and in areas with altitudes of 2 to 10 meters in the area of floodplains and fluvio-lagoon terraces. The present work aimed to characterize and classify soils in the Brazilian Soil Classification System - SiBCS and correlate them with the IUSS Working Group WRB-FAO (in parentheses), besides evidence some soil-landscape relations, that occur in Pleistocene terraces and fluvium- lagoon sediments in the Prata watershed, located in the ecological reserve of Dois Irmãos State Park in Recife – PE, Brazil. Soil samples were used to perform physical, chemical and mineralogical analysis in laboratory. Watershed delimitation, Digital Elevation Model (DEM), slope map, soil map and slope x soil map were obtained and studied. The soils are quite acidic and have a very low natural fertility, with the Latossolos (Ferralsols) predominating in the landscape. The silt and clay fractions of the studied Argissolos (Acrisols) and Latossolos (Ferralsols) presented quartz and kaolinite as the main component. In the profile of Neossolo Quartzarênico (Arenosols) only quartz was identified as a component of the silt and clay fractions. The kaolinitic mineralogy of the clay fraction is consistent with the environment of its formation, that is, hot and humid. There is no relationship between the colors of soils and their exposure to the sun on the slopes where they occur. The occurrence of a sandy and whitish horizon between the litter and the A horizon, is not foreseen in the norms and criteria adopted in the Brazilian Soil Classification System - SiBCS.
Thesagro:	Classificação do Solo Ferralsolo Mapa
NAL Thesaurus:	Soil map Ferralsols
Palavras-chave:	SiBCS Barreiras group Grupo Barreiras
Digital Object Identifier:	https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023
Tipo do material:	Artigo de periódico
Acesso:	openAccess
Aparece nas coleções:	Artigo em periódico indexado (CNPS)