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Registro Completo |
Biblioteca(s): |
Embrapa Semiárido. |
Data corrente: |
10/01/2003 |
Data da última atualização: |
12/03/2020 |
Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
Autoria: |
CUENCA, M. A. G.; RESENDE, J. M.; SAGGIN JUNIOR, O. J.; REIS, C. dos S. |
Afiliação: |
ORIVALDO JOSE SAGGIN JUNIOR, CPATSA. |
Título: |
Mercado brasileiro do coco: situação atual e perspectivas. |
Ano de publicação: |
2002 |
Fonte/Imprenta: |
In: ARAGÃO, W. M. (Ed.). Coco: pós-colheita. Brasília, DF: Embrapa Informação Tecnológica, 2002. |
Páginas: |
cap. 2, p. 11-18. |
Série: |
(Frutas do Brasil, 29). |
Idioma: |
Português |
Conteúdo: |
A cultura do coqueiro é uma atividade agrícola que tem grande importância em mais de 86 países, seja na geração de divisas, emprego, renda ou alimentação para a população. |
Palavras-Chave: |
Mercado brasileiro. |
Thesagro: |
Coco; Comercialização; Mercado; Preço. |
Thesaurus Nal: |
Coconuts; Commercialization. |
Categoria do assunto: |
E Economia e Indústria Agrícola |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/211793/1/Mercado-brasileiro-do-coco-situacao-atual-e-perspectivas.pdf
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Marc: |
LEADER 00940naa a2200265 a 4500 001 1150893 005 2020-03-12 008 2002 bl uuuu u00u1 u #d 100 1 $aCUENCA, M. A. G. 245 $aMercado brasileiro do coco$bsituação atual e perspectivas. 260 $c2002 300 $acap. 2, p. 11-18. 490 $a(Frutas do Brasil, 29). 520 $aA cultura do coqueiro é uma atividade agrícola que tem grande importância em mais de 86 países, seja na geração de divisas, emprego, renda ou alimentação para a população. 650 $aCoconuts 650 $aCommercialization 650 $aCoco 650 $aComercialização 650 $aMercado 650 $aPreço 653 $aMercado brasileiro 700 1 $aRESENDE, J. M. 700 1 $aSAGGIN JUNIOR, O. J. 700 1 $aREIS, C. dos S. 773 $tIn: ARAGÃO, W. M. (Ed.). Coco: pós-colheita. Brasília, DF: Embrapa Informação Tecnológica, 2002.
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Embrapa Semiárido (CPATSA) |
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
30/01/2023 |
Data da última atualização: |
13/03/2023 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 2 |
Autoria: |
NEVES, L. V. de M. W.; SOUSA, J. E. S. de; SANTOS, J. C. B. dos; ARAUJO FILHO, J. C. de; CORRÊA, M. M.; SOUSA, M. G.; FRACETTO, F. J. C.; FRACETTO, G. G. M.; ARAUJO, J. K. S.; FREIRE, G. A. P.; FERREIRA, T. O.; SOUZA JÚNIOR, V. S. de. |
Afiliação: |
LAÉRCIO VIEIRA DE MELO WANDERLEY NEVES, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JULIET EMILIA SANTOS DE SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JEAN CHEYSON BARROS DOS SANTOS, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JOSE COELHO DE ARAUJO FILHO, CNPS; MARCELO METRI CORRÊA, UNIVERSIDADE FEDERAL DO AGRESTE DE PERNAMBUCO; MARILYA GABRYELLA SOUSA, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; FELIPE JOSÉ CURY FRACETTO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; GISELLE GOMES MONTEIRO FRACETTO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; JANE KELLY SILVA ARAUJO, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO; GABRIEL ARAÚJO PAES FREIRE, FUNDAÇÃO UNIVERSITÁRIA FEDERAL DE RONDÔNIA; TIAGO OSÓRIO FERREIRA, UNIVERSIDADE DE SÃO PAULO; VALDOMIRO SEVERINO DE SOUZA JÚNIOR, UNIVERSIDADE FEDERAL RURAL DE PERNAMBUCO. |
Título: |
Weathering of gneiss saprolites and formation of Planosols under semiarid climate (NE Brazil). |
Ano de publicação: |
2023 |
Fonte/Imprenta: |
Journal of South American Earth Sciences, v. 123, 104206, Mar. 2023. |
DOI: |
https://doi.org/10.1016/j.jsames.2023.104206 |
Idioma: |
Inglês |
Conteúdo: |
The Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, with no evidence of argilluviation. For total regolith profile, acidic metamorphic rocks present high structural variability directly influencing the evolution of saprolites, the alteration of primary minerals, and the formation routes of secondary minerals. The secondary assemblage was rather similar and comprised illite, smectite, and kaolinite in both regoliths. The saprolite inclination in P1 favors water movement in relation to P2. The regolith in P1 shows greater mineral alteration with increased pedogenic development. MenosThe Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, wi... Mostrar Tudo |
Palavras-Chave: |
Ilita; K-feldspars; K-feldspato; Perfis de regolito; Plagioclásio; Regolith profile. |
Thesaurus NAL: |
Illite; Plagioclase. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 03117naa a2200361 a 4500 001 2151336 005 2023-03-13 008 2023 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1016/j.jsames.2023.104206$2DOI 100 1 $aNEVES, L. V. de M. W. 245 $aWeathering of gneiss saprolites and formation of Planosols under semiarid climate (NE Brazil).$h[electronic resource] 260 $c2023 520 $aThe Brazilian semiarid is one of the most populous regions in the world. The main income for populations in this region is agricultural production, which in turn is limited by climatic and soil conditions. This region has environmental and economic correlations with underdeveloped regions in northwestern Africa, displaying soil surface with monotonous landscapes of smooth undulating relief with large extensions of Planosols. Climatic conditions that lead to the formation of poorly developed soils and to losses of surface layers make these soils susceptible to degradation. In the Brazilian semiarid, lithology shows that felsic rocks are the main factor in pedogenesis of Planosols, conferring the main physical, chemical, and mineralogical attributes to the soil. In this study, we evaluated the pedogenesis by weathering of gneisses (felsic rocks) in two profiles of Planosols in the Cabrobó Desertification Nucleus, Pernambuco State, northeast Brazil, highlighting the role of the parent material in the soil intrinsic characteristics in the pedogenetic processes. The primary assemblage and pedological features were determined by optical microscopy in thin sections of the A, B, and C horizons from the two soil profiles. The secondary assemblage was identified by X-ray diffractometry using the technique: SEM-scanning electron microscopy. Clay formation in situ, colluvial contribution, and elutriation process contributed to the formation of the gradient textural in both Planosols, with no evidence of argilluviation. For total regolith profile, acidic metamorphic rocks present high structural variability directly influencing the evolution of saprolites, the alteration of primary minerals, and the formation routes of secondary minerals. The secondary assemblage was rather similar and comprised illite, smectite, and kaolinite in both regoliths. The saprolite inclination in P1 favors water movement in relation to P2. The regolith in P1 shows greater mineral alteration with increased pedogenic development. 650 $aIllite 650 $aPlagioclase 653 $aIlita 653 $aK-feldspars 653 $aK-feldspato 653 $aPerfis de regolito 653 $aPlagioclásio 653 $aRegolith profile 700 1 $aSOUSA, J. E. S. de 700 1 $aSANTOS, J. C. B. dos 700 1 $aARAUJO FILHO, J. C. de 700 1 $aCORRÊA, M. M. 700 1 $aSOUSA, M. G. 700 1 $aFRACETTO, F. J. C. 700 1 $aFRACETTO, G. G. M. 700 1 $aARAUJO, J. K. S. 700 1 $aFREIRE, G. A. P. 700 1 $aFERREIRA, T. O. 700 1 $aSOUZA JÚNIOR, V. S. de 773 $tJournal of South American Earth Sciences$gv. 123, 104206, Mar. 2023.
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