| |
|
|
|
Registro Completo |
|
Biblioteca(s): |
Embrapa Gado de Leite. |
|
Data corrente: |
02/12/2015 |
|
Data da última atualização: |
03/02/2024 |
|
Tipo da produção científica: |
Artigo em Anais de Congresso |
|
Autoria: |
ZOCCAL, R.; PEREIRA, V. da F.; OLIVEIRA, O. C. DE. |
|
Afiliação: |
ROSANGELA ZOCCAL, CNPGL; VANESSA DA FONSECA PEREIRA, DTT; OCTAVIO COSTA DE OLIVEIRA, IBGE. |
|
Título: |
A pecuária de leite no Brasil: quantificação e caracterização dos produtores. |
|
Ano de publicação: |
2015 |
|
Fonte/Imprenta: |
In: CONGRESSO DA SOCIEDADE BRASILEIRA DE ECONOMIA, ADMINISTRAÇÃO E SOCIOLOGIA RURAL, 53., 2015, João Pessoa. Agropecuária, meio ambiente e desenvolvimento: anais. João Pessoa: Sober, 2015. |
|
Idioma: |
Português |
|
Palavras-Chave: |
Concentração; Pecuária de leite. |
|
Thesagro: |
Produtividade. |
|
Categoria do assunto: |
E Economia e Indústria Agrícola |
|
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1030303/1/A-pecuaria-de-leite-no-Brasil.pdf
|
|
Marc: |
LEADER 00645nam a2200157 a 4500
001 2030303
005 2024-02-03
008 2015 bl uuuu u00u1 u #d
100 1 $aZOCCAL, R.
245 $aA pecuária de leite no Brasil$bquantificação e caracterização dos produtores.$h[electronic resource]
260 $aIn: CONGRESSO DA SOCIEDADE BRASILEIRA DE ECONOMIA, ADMINISTRAÇÃO E SOCIOLOGIA RURAL, 53., 2015, João Pessoa. Agropecuária, meio ambiente e desenvolvimento: anais. João Pessoa: Sober$c2015
650 $aProdutividade
653 $aConcentração
653 $aPecuária de leite
700 1 $aPEREIRA, V. da F.
700 1 $aOLIVEIRA, O. C. DE
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Gado de Leite (CNPGL) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
URL |
Voltar
|
|
|
Registro Completo
|
Biblioteca(s): |
Embrapa Solos. |
|
Data corrente: |
11/12/2023 |
|
Data da última atualização: |
25/01/2024 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Circulação/Nível: |
B - 1 |
|
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. |
|
Título: |
Soil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil. |
|
Ano de publicação: |
2023 |
|
Fonte/Imprenta: |
Engenharia Agrícola, v. 43, n. 4, e20230147, 2023. |
|
DOI: |
https://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023 |
|
Idioma: |
Inglês |
|
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. MenosIn 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 rela... Mostrar Tudo |
|
Palavras-Chave: |
Barreiras group; Grupo Barreiras; SiBCS. |
|
Thesagro: |
Classificação do Solo; Ferralsolo; Mapa. |
|
Thesaurus NAL: |
Ferralsols; Soil map. |
|
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1159426/1/Soil-landscape-relationship-in-a-watershed-2023.pdf
|
|
Marc: |
LEADER 02681naa a2200277 a 4500
001 2159426
005 2024-01-25
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1590/1809-4430-Eng.Agric.v43n4e20230147/2023$2DOI
100 1 $aCALDAS, A. M.
245 $aSoil-landscape relationship in a watershed located on pleistocenic terraces and fluvio-lagunarian sediments in municipality of Recife, Brazil.$h[electronic resource]
260 $c2023
520 $aIn 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.
650 $aFerralsols
650 $aSoil map
650 $aClassificação do Solo
650 $aFerralsolo
650 $aMapa
653 $aBarreiras group
653 $aGrupo Barreiras
653 $aSiBCS
700 1 $aROLIM NETO, F. C.
700 1 $aPARAHYBA, R. da B. V.
700 1 $aCORRÊA, M. M.
700 1 $aRODRIGUES, A. de C. F.
773 $tEngenharia Agrícola$gv. 43, n. 4, e20230147, 2023.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Solos (CNPS) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
Fechar
|
| Expressão de busca inválida. Verifique!!! |
|
|
