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Registro Completo |
Biblioteca(s): |
Embrapa Tabuleiros Costeiros; Embrapa Trigo. |
Data corrente: |
04/02/2014 |
Data da última atualização: |
10/03/2014 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
PROCOPIO, S. de O.; FERNANDES, M. F.; TELES, D. A.; SENA FILHO, J. G. de; CARGNELUTTI FILHO, A.; VARGAS, L. |
Afiliação: |
SERGIO DE OLIVEIRA PROCOPIO, CPATC; MARCELO FERREIRA FERNANDES, CPATC; JOSE GUEDES DE SENA FILHO, CPATC; LEANDRO VARGAS, CNPT. |
Título: |
Tolerância da bactéria diazotrófica Gluconacetobacter diazotrophicus a herbicidas utilizados na cultura da cana-de-açúcar. |
Ano de publicação: |
2013 |
Fonte/Imprenta: |
Agrária - Revista Brasileira de Ciências Agrárias, Recife v. 8, n. 4, p. 610-617, out./dez. 2013. |
ISSN: |
1981-0997 |
DOI: |
10.5039/agraria.v8i4a3433 |
Idioma: |
Português |
Palavras-Chave: |
Bological nitrogen fixation; Fixação biológica de nitrogênio; Pesticidas; Saccharum spp. |
Thesaurus Nal: |
pesticides. |
Categoria do assunto: |
-- H Saúde e Patologia |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/97121/1/Toleranciaprocopio.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/96392/1/2013-agraria-v.8n4p610.pdf
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Marc: |
LEADER 00880naa a2200253 a 4500 001 1979588 005 2014-03-10 008 2013 bl uuuu u00u1 u #d 022 $a1981-0997 024 7 $a10.5039/agraria.v8i4a3433$2DOI 100 1 $aPROCOPIO, S. de O. 245 $aTolerância da bactéria diazotrófica Gluconacetobacter diazotrophicus a herbicidas utilizados na cultura da cana-de-açúcar.$h[electronic resource] 260 $c2013 650 $apesticides 653 $aBological nitrogen fixation 653 $aFixação biológica de nitrogênio 653 $aPesticidas 653 $aSaccharum spp 700 1 $aFERNANDES, M. F. 700 1 $aTELES, D. A. 700 1 $aSENA FILHO, J. G. de 700 1 $aCARGNELUTTI FILHO, A. 700 1 $aVARGAS, L. 773 $tAgrária - Revista Brasileira de Ciências Agrárias, Recife$gv. 8, n. 4, p. 610-617, out./dez. 2013.
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Registro original: |
Embrapa Tabuleiros Costeiros (CPATC) |
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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
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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.
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