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Registro Completo |
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Biblioteca(s): |
Embrapa Agrobiologia; Embrapa Mandioca e Fruticultura. |
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Data corrente: |
27/12/2005 |
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Data da última atualização: |
10/03/2006 |
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Autoria: |
SOUZA, J. C. de; HAGA, A.; SOUZA, M. de A. |
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Título: |
Pragas da goiabeira. |
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Ano de publicação: |
2003 |
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Fonte/Imprenta: |
Belo Horizonte: EPAMIG, 2003. |
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Páginas: |
60 p. |
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Série: |
(EPAMIG. Boletim Técnico, 71). |
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ISSN: |
0101-062X |
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Idioma: |
Português |
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Conteúdo: |
A família Myrtaceae é uma das mais importantes para a fruticultura, abrangendo 140 gêneros e 3 mil espécies. No Brasil, são conhecidas mais de cem espécies, distribuídas de norte a sul do país. Os genêros Eugenia, Campomanesia, Psidium e Myrciaria são os mais importantes do ponto de vista de exploração econômica frutícola (DONADIO, 1996). Atualmente, a goiaba pode ser encontrada em mais de 50 países das regiões tropicais e subtropicais, com destaque para Brasil, Índia e México (WONDERFUL..., 2002), sendo o Brasil o maior produtor mundial. Em 1998, foram produzidas 256.616 toneladas de goiabas no país em 11.504 há, com destaque para o estado de São Paulo, que respondeu por 68,3% desse total. Naquele ano, Minas Gerais ocupava a oitava posição nacional, com 4.252 toneladas produzidas em 728 há (AGRIANUAL, 2001), posição que tende a melhorar significativamente com a plena produção dos novos pomares implantados. |
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Palavras-Chave: |
Guava; Pragas. |
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Thesagro: |
Goiaba; Praga de Planta. |
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Categoria do assunto: |
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X Pesquisa, Tecnologia e Engenharia |
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Marc: |
LEADER 01454nam a2200217 a 4500
001 1628608
005 2006-03-10
008 2003 bl uuuu u0uu1 u #d
022 $a0101-062X
100 1 $aSOUZA, J. C. de
245 $aPragas da goiabeira.
260 $aBelo Horizonte: EPAMIG$c2003
300 $a60 p.
490 $a(EPAMIG. Boletim Técnico, 71).
520 $aA família Myrtaceae é uma das mais importantes para a fruticultura, abrangendo 140 gêneros e 3 mil espécies. No Brasil, são conhecidas mais de cem espécies, distribuídas de norte a sul do país. Os genêros Eugenia, Campomanesia, Psidium e Myrciaria são os mais importantes do ponto de vista de exploração econômica frutícola (DONADIO, 1996). Atualmente, a goiaba pode ser encontrada em mais de 50 países das regiões tropicais e subtropicais, com destaque para Brasil, Índia e México (WONDERFUL..., 2002), sendo o Brasil o maior produtor mundial. Em 1998, foram produzidas 256.616 toneladas de goiabas no país em 11.504 há, com destaque para o estado de São Paulo, que respondeu por 68,3% desse total. Naquele ano, Minas Gerais ocupava a oitava posição nacional, com 4.252 toneladas produzidas em 728 há (AGRIANUAL, 2001), posição que tende a melhorar significativamente com a plena produção dos novos pomares implantados.
650 $aGoiaba
650 $aPraga de Planta
653 $aGuava
653 $aPragas
700 1 $aHAGA, A.
700 1 $aSOUZA, M. de A.
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Registro original: |
Embrapa Agrobiologia (CNPAB) |
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Biblioteca |
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Cutter |
Registro |
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Registro Completo
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Biblioteca(s): |
Embrapa Agricultura Digital. |
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Data corrente: |
15/10/2013 |
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Data da última atualização: |
15/10/2013 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
ASSAD, E. D.; PINTO, H. S.; MARTINS, S. C.; GROPPO, J. D.; SALGADO, P. R.; EVANGELISTA, B.; VASCONCELLOS, E.; SANO, E. E.; PAVÃO, E.; LUNA, R.; CAMARGO, P. B.; MARTINELLI, L. A. |
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Afiliação: |
EDUARDO DELGADO ASSAD, CNPTIA; Unicamp; CNPTIA; CNPTIA; PAULA RODRIGUES SALGADO, SAPC; BALBINO ANTONIO EVANGELISTA, CPAC; CNPTIA; EDSON EYJI SANO, CPAC; CNPTIA; CNPTIA; USP; USP. |
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Título: |
Changes in soil carbon stocks in Brazil due to land use: paired site comparisons and a regional pasture soil survey. |
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Ano de publicação: |
2013 |
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Fonte/Imprenta: |
Biogeosciences, v. 10, n. 10, p. 6141-6160, 2013. |
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ISBN: |
10.5194/bg-10-6141-2013 |
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Idioma: |
Inglês |
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Conteúdo: |
Abstract. In this paper we calculated soil carbon stocks in Brazil using 17 paired sites where soil stocks were determined in native vegetation, pastures and crop-livestock systems (CPS), and in other regional samplings encompassing more than 100 pasture soils, from 6.58° S to 31.53° S, involving three major Brazilian biomes: Cerrado, Atlantic Forest, and the Pampa. The average native vegetation soil carbon stocks at 10, 30 and 60 cm soil depth were equal to approximately 29, 64, and 92 Mg ha-1, respectively. In the paired sites, carbon losses of 7.5 Mg ha-1 and 11.6 Mg ha-1 in CPS systems were observed at 10 cm and 30 cm soil depths, respectively. In pasture soils, carbon losses were similar and equal to 7.5 Mg ha-1 and 11.0 Mg ha-1 at 10 cm and 30 cm soil depths, respectively. Differences at 60 cm soil depth were equal to -25.4%o and -24.0%o, increasing to -19.6 %o and -17.7%o in CPS, and to -18.9%o, and -18.3%o in pasture soils, respectively; indicating an increasing contribution of C4 carbon in these agrosystems. In the regional survey of pasture soils, the soil carbon stock at 30 cm was equal to approximately 51 Mg ha-1, with an average d13C value of -19.6%o. Key controllers of soil carbon stock in pasture sites were sand content and mean annual temperature. Collectively, both could explain approximately half of the variance of soil carbon stocks. When pasture soil carbon stocks were compared with the average soil carbon stocks of native vegetation estimated for Brazilian biomes and soil types by Bernoux et al. (2002) there was a carbon gain of 6.7 Mg ha-1, which is equivalent to a carbon gain of 15% compared to the carbon soil stock of the native vegetation. The findings of this study are consistent with differences found between regional comparisons like our pasture sites and local paired study sites in estimating soil carbon stocks changes due to land use changes. MenosAbstract. In this paper we calculated soil carbon stocks in Brazil using 17 paired sites where soil stocks were determined in native vegetation, pastures and crop-livestock systems (CPS), and in other regional samplings encompassing more than 100 pasture soils, from 6.58° S to 31.53° S, involving three major Brazilian biomes: Cerrado, Atlantic Forest, and the Pampa. The average native vegetation soil carbon stocks at 10, 30 and 60 cm soil depth were equal to approximately 29, 64, and 92 Mg ha-1, respectively. In the paired sites, carbon losses of 7.5 Mg ha-1 and 11.6 Mg ha-1 in CPS systems were observed at 10 cm and 30 cm soil depths, respectively. In pasture soils, carbon losses were similar and equal to 7.5 Mg ha-1 and 11.0 Mg ha-1 at 10 cm and 30 cm soil depths, respectively. Differences at 60 cm soil depth were equal to -25.4%o and -24.0%o, increasing to -19.6 %o and -17.7%o in CPS, and to -18.9%o, and -18.3%o in pasture soils, respectively; indicating an increasing contribution of C4 carbon in these agrosystems. In the regional survey of pasture soils, the soil carbon stock at 30 cm was equal to approximately 51 Mg ha-1, with an average d13C value of -19.6%o. Key controllers of soil carbon stock in pasture sites were sand content and mean annual temperature. Collectively, both could explain approximately half of the variance of soil carbon stocks. When pasture soil carbon stocks were compared with the average soil carbon stocks of native vegetation estimated for Brazili... Mostrar Tudo |
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Palavras-Chave: |
Carbon stocks; Estoque de carbono no solo; Soils; Solo de pastagem. |
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Thesagro: |
Uso da Terra. |
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Thesaurus NAL: |
Land use. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/90991/1/bg-10-6141-2013.pdf
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Marc: |
LEADER 02830naa a2200325 a 4500
001 1968591
005 2013-10-15
008 2013 bl uuuu u00u1 u #d
100 1 $aASSAD, E. D.
245 $aChanges in soil carbon stocks in Brazil due to land use$bpaired site comparisons and a regional pasture soil survey.$h[electronic resource]
260 $c2013
520 $aAbstract. In this paper we calculated soil carbon stocks in Brazil using 17 paired sites where soil stocks were determined in native vegetation, pastures and crop-livestock systems (CPS), and in other regional samplings encompassing more than 100 pasture soils, from 6.58° S to 31.53° S, involving three major Brazilian biomes: Cerrado, Atlantic Forest, and the Pampa. The average native vegetation soil carbon stocks at 10, 30 and 60 cm soil depth were equal to approximately 29, 64, and 92 Mg ha-1, respectively. In the paired sites, carbon losses of 7.5 Mg ha-1 and 11.6 Mg ha-1 in CPS systems were observed at 10 cm and 30 cm soil depths, respectively. In pasture soils, carbon losses were similar and equal to 7.5 Mg ha-1 and 11.0 Mg ha-1 at 10 cm and 30 cm soil depths, respectively. Differences at 60 cm soil depth were equal to -25.4%o and -24.0%o, increasing to -19.6 %o and -17.7%o in CPS, and to -18.9%o, and -18.3%o in pasture soils, respectively; indicating an increasing contribution of C4 carbon in these agrosystems. In the regional survey of pasture soils, the soil carbon stock at 30 cm was equal to approximately 51 Mg ha-1, with an average d13C value of -19.6%o. Key controllers of soil carbon stock in pasture sites were sand content and mean annual temperature. Collectively, both could explain approximately half of the variance of soil carbon stocks. When pasture soil carbon stocks were compared with the average soil carbon stocks of native vegetation estimated for Brazilian biomes and soil types by Bernoux et al. (2002) there was a carbon gain of 6.7 Mg ha-1, which is equivalent to a carbon gain of 15% compared to the carbon soil stock of the native vegetation. The findings of this study are consistent with differences found between regional comparisons like our pasture sites and local paired study sites in estimating soil carbon stocks changes due to land use changes.
650 $aLand use
650 $aUso da Terra
653 $aCarbon stocks
653 $aEstoque de carbono no solo
653 $aSoils
653 $aSolo de pastagem
700 1 $aPINTO, H. S.
700 1 $aMARTINS, S. C.
700 1 $aGROPPO, J. D.
700 1 $aSALGADO, P. R.
700 1 $aEVANGELISTA, B.
700 1 $aVASCONCELLOS, E.
700 1 $aSANO, E. E.
700 1 $aPAVÃO, E.
700 1 $aLUNA, R.
700 1 $aCAMARGO, P. B.
700 1 $aMARTINELLI, L. A.
773 $tBiogeosciences$gv. 10, n. 10, p. 6141-6160, 2013.
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Embrapa Agricultura Digital (CNPTIA) |
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