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Registro Completo |
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Biblioteca(s): |
Embrapa Mandioca e Fruticultura. |
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Data corrente: |
14/09/2011 |
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Data da última atualização: |
04/08/2017 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
SILVA JUNIOR, J. F. da; FERRAZ, L. G. B.; LEDO, A. da S.; SILVA, S. de O. e; LEDO, C. A. da S. |
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Afiliação: |
JOSUE FRANCISCO DA SILVA JUNIOR, CPATC; LUIZ GONZAGA BIONE FERRAZ, IPA; ANA DA SILVA LEDO, CPATC; SEBASTIÃO DE OLIVEIRA E SILVA, CNPMF; CARLOS ALBERTO DA SILVA LEDO, CNPMF. |
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Título: |
Variedades. |
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Ano de publicação: |
2010 |
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Fonte/Imprenta: |
In: SILVA JUNIOR, J. F. da; LOPES, G. M. B.; FERRAZ, L. G. B. (Ed.). Sistema de produção de banana para a Zona da Mata de Pernambuco. Aracaju: Embrapa Tabuleiros Costeiros, 2010. 139 p. (Embrpa-CPATC. Sistema de produção, 3). |
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Páginas: |
p. 35-45 |
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Idioma: |
Português |
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Conteúdo: |
Em geral, a escolha da variedade a ser explorada é determinada pelo mercado consumidor. Na Zona da Mata pernambucana são três os destinos de consumo predominantes na comercialização da banana: ao natural; frita ou cozida e indústria ou mercado externo. Nessa ordem, as principais variedades de bananeira atualmente cultivadas em larga escala na Zona da Mata de Pernambuco são, respectivamente, de três tipos: a) Tipo Prata/Pacovan ('Pacovan, 'Prata Comum', 'Prata Caiana') e tipo Maçã (Maçã); b) Tipo Terra ou Comprida ('Comprida Verdadeira', 'Chifre de Vaca', 'Mongolô', 'Matapagipe', etc.); e c) Tipo Cavendish ou Anã ('Anã' ou 'Nanica', 'Anã do Alto' ou 'Nanicão', 'Grande Naine'). Outras cultivares locais, a exemplo da 'Pão' e da 'Vinagre' ou 'Roxa', são inexpressivas economicamente. |
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Palavras-Chave: |
Banana Chifre de Vaca; Banana Comprida Verdadeira; Banana Comum; Banana Matapagipe; Banana Mongolô; Banana Naine; Banana Pacovan; Banana Prata Caiana; Banana PratalPacovan; Banana Terra; Variedade de banana. |
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Thesagro: |
Banana; Banana Maca. |
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Categoria do assunto: |
F Plantas e Produtos de Origem Vegetal |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/42664/1/Variedade-Carlos-Alberto-Silva-Ledo.pdf
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Marc: |
LEADER 01863naa a2200337 a 4500
001 1900435
005 2017-08-04
008 2010 bl uuuu u00u1 u #d
100 1 $aSILVA JUNIOR, J. F. da
245 $aVariedades.
260 $c2010
300 $ap. 35-45
520 $aEm geral, a escolha da variedade a ser explorada é determinada pelo mercado consumidor. Na Zona da Mata pernambucana são três os destinos de consumo predominantes na comercialização da banana: ao natural; frita ou cozida e indústria ou mercado externo. Nessa ordem, as principais variedades de bananeira atualmente cultivadas em larga escala na Zona da Mata de Pernambuco são, respectivamente, de três tipos: a) Tipo Prata/Pacovan ('Pacovan, 'Prata Comum', 'Prata Caiana') e tipo Maçã (Maçã); b) Tipo Terra ou Comprida ('Comprida Verdadeira', 'Chifre de Vaca', 'Mongolô', 'Matapagipe', etc.); e c) Tipo Cavendish ou Anã ('Anã' ou 'Nanica', 'Anã do Alto' ou 'Nanicão', 'Grande Naine'). Outras cultivares locais, a exemplo da 'Pão' e da 'Vinagre' ou 'Roxa', são inexpressivas economicamente.
650 $aBanana
650 $aBanana Maca
653 $aBanana Chifre de Vaca
653 $aBanana Comprida Verdadeira
653 $aBanana Comum
653 $aBanana Matapagipe
653 $aBanana Mongolô
653 $aBanana Naine
653 $aBanana Pacovan
653 $aBanana Prata Caiana
653 $aBanana PratalPacovan
653 $aBanana Terra
653 $aVariedade de banana
700 1 $aFERRAZ, L. G. B.
700 1 $aLEDO, A. da S.
700 1 $aSILVA, S. de O. e
700 1 $aLEDO, C. A. da S.
773 $tIn: SILVA JUNIOR, J. F. da; LOPES, G. M. B.; FERRAZ, L. G. B. (Ed.). Sistema de produção de banana para a Zona da Mata de Pernambuco. Aracaju: Embrapa Tabuleiros Costeiros, 2010. 139 p. (Embrpa-CPATC. Sistema de produção, 3).
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Registro original: |
Embrapa Mandioca e Fruticultura (CNPMF) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Florestas. Para informações adicionais entre em contato com cnpf.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
22/09/2008 |
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Data da última atualização: |
22/09/2008 |
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Autoria: |
HEDDE, M.; BUREAU, F.; CECILLON, L.; DECAENS, T. |
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Título: |
Effects of five earthworm species on soil structure and organic matter in LUVISOLs. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
In: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM. |
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Idioma: |
Inglês |
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Conteúdo: |
Earthworms are frequently cited as key stone soil organisms, however, their effects on soil
structure stability and organic matter (OM) in macro-aggregates are mainly driven by soil type
and land use. Loamy soils of the Bassin Parisien are mainly dedicated to intensive crop which
have led to soil degradation. Introduction of pastures is one of the most promising practices that
may restore them. The aim of this work is to quantify and compare, in laboratory experiments,
the effects of 5 earthworm species on soil OM. We hypothesize that direction and magnitude of
earthworm effects depend on (i) earthworm species and (ii) OM of the substrate hosting it.
Five earthworm species were retained for the experiment (Aporrectodea caliginosa,
Aporrectodea rosea, Allolobophora chlorotica, Aporrectodea icterica and Aporrectodea longa).
The superficial soil of 3 stands were sampled in May 2006: a 30 yrs intensive crop stand (CS);
a 5 yrs pasture (YP); a 46 yrs permanent pasture (PP). Soil (150 g of 2mm-sieved) was added
to microcosms and moistened at field capacity at the onset of the experiment. Three replicates
were set up for each treatment (species x substrate) and stored for 3 weeks in climate chambers.
C-CO2 release during the experiment was estimated by the conductivity method (Heemsbergen
et al., 2004). At the end of the experiment, soil was air-dried and dry-sieved at 2 mm to isolate
and weight the large macro-aggregate fraction (> 2mm, LMA). LMA were characterized by (i)
their organic matter content (loss-in-ignition at 550 °C); (ii) their stability estimated by the more
desegregating test of Le Bissonnais? (1996) method and expressed as the mean weight diameter
(MWD) and (iii) their organic composition assessed by Near Infrared Spectroscopy (NIRS, Antaris
II Thermo electron).
The C-CO2 release may result from quality or localisation of soil OM. The high C-CO2 release
observed in CS-microcosms hosting earthworm can be explained by the mineralization of a
labile OM pool. This hypothesis was confirmed by the decrease of OM content in LMA. On the
other hand, in pasture soils, the lack of C-CO2 release increase in earthworm presence may be
due to a physical or chemical protection of OM.
Globally the rate of LMA production decreased with soil OM content increase. On low OM content
soil, earthworms should ingest a larger amount of soil than on high OM content soil to cover the
energetic needs.
Aggregate structural stability produced in earthworms hosting microcosms was lower (CS soil),
similar (YP soil) and higher (PP soil) than in animal-free controls. Although the factor ?species?
mattered, short-term stabilisation mechanisms in those loamy soils were firstly linked to the
initial soil OM content.
Interpretation of NIRS spectra showed that the regular disturbance regime YP was submitted to
might have maintained OM biochemical composition similar to CS one and that the composition
of soil OM influence the capacities of earthworms to modify this OM composition.
Biodiversity, Conservation and
Sustainable Management of Soil Animals
August 25 - 29, 2008
Positivo University
Curitiba - Paraná - Brazil
We demonstrated that earthworm short-term effects depend on both earthworm species and
initial soil OM. These effects are complex and appear mainly in the more contrasted soils.
Conversely, in the 5-years old pasture soil, earthworm presence has very few effects. MenosEarthworms are frequently cited as key stone soil organisms, however, their effects on soil
structure stability and organic matter (OM) in macro-aggregates are mainly driven by soil type
and land use. Loamy soils of the Bassin Parisien are mainly dedicated to intensive crop which
have led to soil degradation. Introduction of pastures is one of the most promising practices that
may restore them. The aim of this work is to quantify and compare, in laboratory experiments,
the effects of 5 earthworm species on soil OM. We hypothesize that direction and magnitude of
earthworm effects depend on (i) earthworm species and (ii) OM of the substrate hosting it.
Five earthworm species were retained for the experiment (Aporrectodea caliginosa,
Aporrectodea rosea, Allolobophora chlorotica, Aporrectodea icterica and Aporrectodea longa).
The superficial soil of 3 stands were sampled in May 2006: a 30 yrs intensive crop stand (CS);
a 5 yrs pasture (YP); a 46 yrs permanent pasture (PP). Soil (150 g of 2mm-sieved) was added
to microcosms and moistened at field capacity at the onset of the experiment. Three replicates
were set up for each treatment (species x substrate) and stored for 3 weeks in climate chambers.
C-CO2 release during the experiment was estimated by the conductivity method (Heemsbergen
et al., 2004). At the end of the experiment, soil was air-dried and dry-sieved at 2 mm to isolate
and weight the large macro-aggregate fraction (> 2mm, LMA). LMA were characterized by (i)
their or... Mostrar Tudo |
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Categoria do assunto: |
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Marc: |
LEADER 04113naa a2200157 a 4500
001 1314907
005 2008-09-22
008 2008 bl uuuu u00u1 u #d
100 1 $aHEDDE, M.
245 $aEffects of five earthworm species on soil structure and organic matter in LUVISOLs.
260 $c2008
520 $aEarthworms are frequently cited as key stone soil organisms, however, their effects on soil structure stability and organic matter (OM) in macro-aggregates are mainly driven by soil type and land use. Loamy soils of the Bassin Parisien are mainly dedicated to intensive crop which have led to soil degradation. Introduction of pastures is one of the most promising practices that may restore them. The aim of this work is to quantify and compare, in laboratory experiments, the effects of 5 earthworm species on soil OM. We hypothesize that direction and magnitude of earthworm effects depend on (i) earthworm species and (ii) OM of the substrate hosting it. Five earthworm species were retained for the experiment (Aporrectodea caliginosa, Aporrectodea rosea, Allolobophora chlorotica, Aporrectodea icterica and Aporrectodea longa). The superficial soil of 3 stands were sampled in May 2006: a 30 yrs intensive crop stand (CS); a 5 yrs pasture (YP); a 46 yrs permanent pasture (PP). Soil (150 g of 2mm-sieved) was added to microcosms and moistened at field capacity at the onset of the experiment. Three replicates were set up for each treatment (species x substrate) and stored for 3 weeks in climate chambers. C-CO2 release during the experiment was estimated by the conductivity method (Heemsbergen et al., 2004). At the end of the experiment, soil was air-dried and dry-sieved at 2 mm to isolate and weight the large macro-aggregate fraction (> 2mm, LMA). LMA were characterized by (i) their organic matter content (loss-in-ignition at 550 °C); (ii) their stability estimated by the more desegregating test of Le Bissonnais? (1996) method and expressed as the mean weight diameter (MWD) and (iii) their organic composition assessed by Near Infrared Spectroscopy (NIRS, Antaris II Thermo electron). The C-CO2 release may result from quality or localisation of soil OM. The high C-CO2 release observed in CS-microcosms hosting earthworm can be explained by the mineralization of a labile OM pool. This hypothesis was confirmed by the decrease of OM content in LMA. On the other hand, in pasture soils, the lack of C-CO2 release increase in earthworm presence may be due to a physical or chemical protection of OM. Globally the rate of LMA production decreased with soil OM content increase. On low OM content soil, earthworms should ingest a larger amount of soil than on high OM content soil to cover the energetic needs. Aggregate structural stability produced in earthworms hosting microcosms was lower (CS soil), similar (YP soil) and higher (PP soil) than in animal-free controls. Although the factor ?species? mattered, short-term stabilisation mechanisms in those loamy soils were firstly linked to the initial soil OM content. Interpretation of NIRS spectra showed that the regular disturbance regime YP was submitted to might have maintained OM biochemical composition similar to CS one and that the composition of soil OM influence the capacities of earthworms to modify this OM composition. Biodiversity, Conservation and Sustainable Management of Soil Animals August 25 - 29, 2008 Positivo University Curitiba - Paraná - Brazil We demonstrated that earthworm short-term effects depend on both earthworm species and initial soil OM. These effects are complex and appear mainly in the more contrasted soils. Conversely, in the 5-years old pasture soil, earthworm presence has very few effects.
700 1 $aBUREAU, F.
700 1 $aCECILLON, L.
700 1 $aDECAENS, T.
773 $tIn: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM.
Download
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