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Registro Completo |
Biblioteca(s): |
Embrapa Florestas. |
Data corrente: |
27/07/2009 |
Data da última atualização: |
25/02/2015 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
VILLA, F.; FRÁGUAS, C. B.; DUTRA, L. F.; PIO, L. A. S.; PASQUAL, M. |
Título: |
Multiplicação in vitro de amoreira-preta cultivar Brazos. |
Ano de publicação: |
2006 |
Fonte/Imprenta: |
Ciência e Agrotecnologia, Lavras, v. 30, n.2, p. 266-270, mar./abr. 2006 |
Idioma: |
Português |
Conteúdo: |
A micropropagação da amoreira-preta pode gerar plantas livres de vírus e em curto espaço de tempo. Com o objetivo de aprimorar técnicas de micropropagação de amoreira-preta cultivar Brazos (Rubus idaeus L.), segmentos nodais, oriundos de plântulas preestabelecidas in vitro foram excisados e inoculados em meio WPM (0, 50, 100, 150 e 200%), suplementado com diferentes concentrações de BAP (0; 0,5; 1,0; 2,0 e 4,0 mg L-1). Após a inoculação, os explantes foram transferidos para sala de crescimento a 27±1ºC, irradiância de 35 mmol m 2 s 1 e fotoperíodo de 16 horas, onde permaneceram por 60 dias. O delineamento experimental utilizado foi inteiramente casualizado, utilizando-se de quatro repetições com quatro explantes cada. Maior número de brotos foi proporcionado com 1,0 mg L-1 de BAP associado a 100% de meio WPM e maior comprimento médio dos brotos após 60 dias foi verificado em 1,0 mg L-1 de BAP associado a 200% de meio WPM. Maior peso de matéria seca da parte aérea foi obtido em meio WPM 200% acrescido de 0,5 mg L-1 de BAP. |
Palavras-Chave: |
Benzilaminopurina; Meio de cultura WPM; Rubis idaeus L. |
Thesagro: |
Micropropagação. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/27185/1/v30n2a11.pdf
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Marc: |
LEADER 01690naa a2200217 a 4500 001 1316138 005 2015-02-25 008 2006 bl uuuu u00u1 u #d 100 1 $aVILLA, F. 245 $aMultiplicação in vitro de amoreira-preta cultivar Brazos.$h[electronic resource] 260 $c2006 520 $aA micropropagação da amoreira-preta pode gerar plantas livres de vírus e em curto espaço de tempo. Com o objetivo de aprimorar técnicas de micropropagação de amoreira-preta cultivar Brazos (Rubus idaeus L.), segmentos nodais, oriundos de plântulas preestabelecidas in vitro foram excisados e inoculados em meio WPM (0, 50, 100, 150 e 200%), suplementado com diferentes concentrações de BAP (0; 0,5; 1,0; 2,0 e 4,0 mg L-1). Após a inoculação, os explantes foram transferidos para sala de crescimento a 27±1ºC, irradiância de 35 mmol m 2 s 1 e fotoperíodo de 16 horas, onde permaneceram por 60 dias. O delineamento experimental utilizado foi inteiramente casualizado, utilizando-se de quatro repetições com quatro explantes cada. Maior número de brotos foi proporcionado com 1,0 mg L-1 de BAP associado a 100% de meio WPM e maior comprimento médio dos brotos após 60 dias foi verificado em 1,0 mg L-1 de BAP associado a 200% de meio WPM. Maior peso de matéria seca da parte aérea foi obtido em meio WPM 200% acrescido de 0,5 mg L-1 de BAP. 650 $aMicropropagação 653 $aBenzilaminopurina 653 $aMeio de cultura WPM 653 $aRubis idaeus L 700 1 $aFRÁGUAS, C. B. 700 1 $aDUTRA, L. F. 700 1 $aPIO, L. A. S. 700 1 $aPASQUAL, M. 773 $tCiência e Agrotecnologia, Lavras$gv. 30, n.2, p. 266-270, mar./abr. 2006
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Embrapa Florestas (CNPF) |
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Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
16/05/2018 |
Data da última atualização: |
11/11/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
COSTA, E. U. C. da; SANTOS, J. C. B. dos; AZEVEDO, A. C. de; ARAUJO FILHO, J. C. de; CORRÊA, M. M.; NEVES, L. V. de M. W.; VIDAL-TORRADO, P.; SOUZA-JÚNIOR, V. S. de. |
Afiliação: |
EDIVAN UCHÔA CAVALCANTI DA COSTA, UFRPE; JEAN CHEYSON BARROS DOS SANTOS, UFRPE; ANTONIO CARLOS DE AZEVEDO, ESALQ-USP; JOSE COELHO DE ARAUJO FILHO, CNPS; MARCELO METRI CORRÊA, UFRPE; LAÉRCIO VIEIRA DE MELO WANDERLEY NEVES, UFRPE; PABLO VIDAL-TORRADO, ESALQ-USP; VALDOMIRO SEVERINO DE SOUZA-JÚNIOR, UFRPE. |
Título: |
Mineral alteration and genesis of Al-rich soils derived from conglomerate deposits in Cabo Basin, NE Brazil. |
Ano de publicação: |
2018 |
Fonte/Imprenta: |
Catena, v. 167, p. 198-211, Aug. 2018. |
DOI: |
https://doi.org/10.1016/j.catena.2018.04.039 |
Idioma: |
Inglês |
Conteúdo: |
In the Cabo Basin, NE Brazil, conglomerates have given rise to soils with attributes that are rarely observed in humid tropical climates and remain relatively unknown within the scientific community. These soils have high levels of Al in the exchangeable phase, diminishing their agricultural and environmental potential in an underdeveloped region of great socioeconomic importance. This paper presents the mineralogy and genesis of soils derived from conglomerates on a slope in the Cabo Basin, with the aim of meeting the demand for studies on Al-rich soils. Three soils were classified, morphologically described and sampled for the accomplishment of chemical, physical and mineralogical analyses, including the main exchangeable cations content, mineralogy of the sand, silt and clay fraction, differentiation of the Fe and Al forms, mineral micromorphology and chemical composition of mineral species. In addition, chemical and physical attributes were used in multivariate analyses. The soil mineralogy is associated with the weathering evolution of three mineralogical zones identified in the Cr horizons. Pathways of alteration followed by feldspars and micas resulted in kaolinite, smectite and hydroxy-Al interlayered smectite formation (argilification). The susceptibility of the conglomerate to weathering, constant releases of Al from the structure of aluminous minerals, low contents of exchangeable bases and consequent low pH values (<5.3) were associated with high levels of exchangeable Al. At the highest position on the slope, a C/Cr transitional horizon provided evidence of the pedogenesis advance on the Cr horizon. Pedogenetic processes then resulted in morphological, physical and mineralogical differentiation between the A and Bt horizons. In addition, a cluster analysis showed similarities between attributes of the Bt and Cr horizons due to their genetic relationships. MenosIn the Cabo Basin, NE Brazil, conglomerates have given rise to soils with attributes that are rarely observed in humid tropical climates and remain relatively unknown within the scientific community. These soils have high levels of Al in the exchangeable phase, diminishing their agricultural and environmental potential in an underdeveloped region of great socioeconomic importance. This paper presents the mineralogy and genesis of soils derived from conglomerates on a slope in the Cabo Basin, with the aim of meeting the demand for studies on Al-rich soils. Three soils were classified, morphologically described and sampled for the accomplishment of chemical, physical and mineralogical analyses, including the main exchangeable cations content, mineralogy of the sand, silt and clay fraction, differentiation of the Fe and Al forms, mineral micromorphology and chemical composition of mineral species. In addition, chemical and physical attributes were used in multivariate analyses. The soil mineralogy is associated with the weathering evolution of three mineralogical zones identified in the Cr horizons. Pathways of alteration followed by feldspars and micas resulted in kaolinite, smectite and hydroxy-Al interlayered smectite formation (argilification). The susceptibility of the conglomerate to weathering, constant releases of Al from the structure of aluminous minerals, low contents of exchangeable bases and consequent low pH values (<5.3) were associated with high levels of exchan... Mostrar Tudo |
Thesagro: |
Alumínio; Hidróxido de Alumínio; Solo. |
Thesaurus NAL: |
Aluminum hydroxide; Exchangeable aluminum; Hydroxy-interlayered minerals; Saprolite; Smectite; Soil. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02897naa a2200325 a 4500 001 2091480 005 2021-11-11 008 2018 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1016/j.catena.2018.04.039$2DOI 100 1 $aCOSTA, E. U. C. da 245 $aMineral alteration and genesis of Al-rich soils derived from conglomerate deposits in Cabo Basin, NE Brazil.$h[electronic resource] 260 $c2018 520 $aIn the Cabo Basin, NE Brazil, conglomerates have given rise to soils with attributes that are rarely observed in humid tropical climates and remain relatively unknown within the scientific community. These soils have high levels of Al in the exchangeable phase, diminishing their agricultural and environmental potential in an underdeveloped region of great socioeconomic importance. This paper presents the mineralogy and genesis of soils derived from conglomerates on a slope in the Cabo Basin, with the aim of meeting the demand for studies on Al-rich soils. Three soils were classified, morphologically described and sampled for the accomplishment of chemical, physical and mineralogical analyses, including the main exchangeable cations content, mineralogy of the sand, silt and clay fraction, differentiation of the Fe and Al forms, mineral micromorphology and chemical composition of mineral species. In addition, chemical and physical attributes were used in multivariate analyses. The soil mineralogy is associated with the weathering evolution of three mineralogical zones identified in the Cr horizons. Pathways of alteration followed by feldspars and micas resulted in kaolinite, smectite and hydroxy-Al interlayered smectite formation (argilification). The susceptibility of the conglomerate to weathering, constant releases of Al from the structure of aluminous minerals, low contents of exchangeable bases and consequent low pH values (<5.3) were associated with high levels of exchangeable Al. At the highest position on the slope, a C/Cr transitional horizon provided evidence of the pedogenesis advance on the Cr horizon. Pedogenetic processes then resulted in morphological, physical and mineralogical differentiation between the A and Bt horizons. In addition, a cluster analysis showed similarities between attributes of the Bt and Cr horizons due to their genetic relationships. 650 $aAluminum hydroxide 650 $aExchangeable aluminum 650 $aHydroxy-interlayered minerals 650 $aSaprolite 650 $aSmectite 650 $aSoil 650 $aAlumínio 650 $aHidróxido de Alumínio 650 $aSolo 700 1 $aSANTOS, J. C. B. dos 700 1 $aAZEVEDO, A. C. de 700 1 $aARAUJO FILHO, J. C. de 700 1 $aCORRÊA, M. M. 700 1 $aNEVES, L. V. de M. W. 700 1 $aVIDAL-TORRADO, P. 700 1 $aSOUZA-JÚNIOR, V. S. de 773 $tCatena$gv. 167, p. 198-211, Aug. 2018.
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