Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil.
Autor(a) principal: | |
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Data de Publicação: | 2023 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
Texto Completo: | http://www.alice.cnptia.embrapa.br/alice/handle/doc/1159426 https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023 |
Resumo: | 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. |
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Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil.SiBCSBarreiras groupGrupo BarreirasClassificação do SoloFerralsoloMapaSoil mapFerralsolsIn 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.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.CALDAS, A. M.ROLIM NETO, F. C.PARAHYBA, R. da B. V.CORRÊA, M. M.RODRIGUES, A. de C. F.2023-12-11T14:32:55Z2023-12-11T14:32:55Z2023-12-112023info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleEngenharia Agrícola, v. 43, n. 4, e20230147, 2023.http://www.alice.cnptia.embrapa.br/alice/handle/doc/1159426https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023enginfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPA2023-12-11T14:32:55Zoai:www.alice.cnptia.embrapa.br:doc/1159426Repositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestopendoar:21542023-12-11T14:32:55falseRepositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestcg-riaa@embrapa.bropendoar:21542023-12-11T14:32:55Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
title |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
spellingShingle |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. CALDAS, A. M. SiBCS Barreiras group Grupo Barreiras Classificação do Solo Ferralsolo Mapa Soil map Ferralsols |
title_short |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
title_full |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
title_fullStr |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
title_full_unstemmed |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
title_sort |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
author |
CALDAS, A. M. |
author_facet |
CALDAS, A. M. ROLIM NETO, F. C. PARAHYBA, R. da B. V. CORRÊA, M. M. RODRIGUES, A. de C. F. |
author_role |
author |
author2 |
ROLIM NETO, F. C. PARAHYBA, R. da B. V. CORRÊA, M. M. RODRIGUES, A. de C. F. |
author2_role |
author author author author |
dc.contributor.none.fl_str_mv |
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. |
dc.contributor.author.fl_str_mv |
CALDAS, A. M. ROLIM NETO, F. C. PARAHYBA, R. da B. V. CORRÊA, M. M. RODRIGUES, A. de C. F. |
dc.subject.por.fl_str_mv |
SiBCS Barreiras group Grupo Barreiras Classificação do Solo Ferralsolo Mapa Soil map Ferralsols |
topic |
SiBCS Barreiras group Grupo Barreiras Classificação do Solo Ferralsolo Mapa Soil map Ferralsols |
description |
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. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-12-11T14:32:55Z 2023-12-11T14:32:55Z 2023-12-11 2023 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
Engenharia Agrícola, v. 43, n. 4, e20230147, 2023. http://www.alice.cnptia.embrapa.br/alice/handle/doc/1159426 https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023 |
identifier_str_mv |
Engenharia Agrícola, v. 43, n. 4, e20230147, 2023. |
url |
http://www.alice.cnptia.embrapa.br/alice/handle/doc/1159426 https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa) instacron:EMBRAPA |
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Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
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EMBRAPA |
institution |
EMBRAPA |
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Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
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Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) |
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Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
repository.mail.fl_str_mv |
cg-riaa@embrapa.br |
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