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| Registros recuperados : 81 | |
| 26. |  | FIALHO, J. S.; AGUIAR, M. I. de; CORREIA, M. E. F.; CAMPANHA, M. M.; OLIVEIRA, T. S. de. Abundância da pedofauna em sistemas tradicionais, agroflorestais e caatinga conservada. In: SIMPÓSIO BRASILEIRO DE RECURSOS NATURAIS DO SEMIÁRIDO, 2., 2015, Quixadá, CE. Anais... Quixadá: UFC, 2015.| Biblioteca(s): Embrapa Milho e Sorgo. |
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| 27. | | OLIVEIRA, T. S. DE; COSTA, A. M. M.; CABRAL, L. M. C.; FREITAS-SILVA, O.; ROSENTHAL, A.; TONON, R. V. Anthracnose Controlled by Essential Oils: Are Nanoemulsion-Based Films and Coatings a Viable and Efficient Technology for Tropical Fruit Preservation? Foods, 2023, v. 2, n. 279, 2023.| Biblioteca(s): Embrapa Agroindústria de Alimentos. |
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| 29. | | CRISOSTOMO, L. A.; SOUSA, A. F.; WEBER, O. B.; ESCOBAR, M. E. O.; OLIVEIRA, T. S. de. Changes in the mineralisation of nutrients and sunflower biomass in soil irrigated with water from oil exploration in a Semi-Arid environment. International Journal of Environment, Agriculture and Biotechnology, v. 2, n. 4, p. 2156-2162, 2017.| Biblioteca(s): Embrapa Agroindústria Tropical. |
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| 31. | | PEREIRA, W. D.; MARTINS NETO, F. L.; SANTOS, R. H. S.; OLIVEIRA, T. S. de; URQUIAGA, S. Changes in the stocks of C and N in organic matter fractions in soil cropped with coffee and fertilized with sunn hemp and ammonium sulfate. Alterações dos estoques de C e N nas frações da matéria orgânica de solo cultivado com cafeeiro e adubado com crotalária e sulfato de amônio Semina: Ciências Agrárias, Londrina, v. 39, n. 3, p. 999-1014, maio/jun. 2018.| Biblioteca(s): Embrapa Agrobiologia. |
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| 32. | | PEREIRA, W. D.; MARTINS NETO, F. L.; SANTOS, R. H. S.; OLIVEIRA, T. S. de; URQUIAGA, S. Changes in the stocks of C and N in organic matter fractions in soil cropped with coffee and fertilized with sunn hemp and ammonium sulfate Semina: Ciências Agrárias, Londrina, v. 39, n. 3, p. 999-1014, maio/jun. 2018.| Biblioteca(s): Embrapa Agrobiologia. |
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| 36. | | LIMA, H. V. de; OLIVEIRA, T. S. de; OLIVEIRA, M. M. de; LIMA, P. J, B. F. Indicadores de qualidade do solo em sistemas de cultivo orgânico e convencional no semi-árido cearense. Revista Brasileira de Ciência do Solo, Viçosa, v. 31, n. 5, p. 1085-1098, set./out. 2007. Título em Inglês: Soil quality indicators in organic and conventional cultivation systems in the semi arid of Ceará - Brazil.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| Registros recuperados : 81 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Uva e Vinho. |
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Data corrente: |
05/07/2012 |
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Data da última atualização: |
10/10/2023 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
HOFF, R.; FALCADE, I.; TONIETTO, J. |
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Afiliação: |
ROSEMARY HOFF, CNPUV; IVANIRA FALCADE, UNIVERSIDADE DE CAXIAS DO SUL; JORGE TONIETTO, CNPUV. |
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Título: |
The geology in the context of geographical indications of fine wines in Serra Gaúcha region (Brazil). |
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Ano de publicação: |
2012 |
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Fonte/Imprenta: |
CONGRES DES TERROIRS VITIVINICOLES. 9., 2012, Bourgogne, France. Actes... Bourgogne, Dijon; Champgne, Reims, CIVC, 25 a 29 Juin 2012. |
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Páginas: |
8-41 |
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Idioma: |
Inglês |
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Conteúdo: |
In Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors of natural factors. To construct the geological sketch, photo-interpretation techniques were employed high-resolution aerial photos associated with field work. The digital image processing was used to construct the digital elevation model from high resolution orbital data and its derivatives such as altimetry, slope and exposure, as well as the geological structures and land forms. MenosIn Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors o... Mostrar Tudo |
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Palavras-Chave: |
Geology and wine; Indicação geográfica; Pinto Bandeira; Rio Grande do Sul; Wine terroir; Zoneamento. |
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Thesagro: |
Enologia; Uva; Viticultura. |
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Categoria do assunto: |
--
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1157182/1/Hoff-8-41.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/61773/1/41-HOFF.pdf
|
|
Marc: |
LEADER 02690nam a2200253 a 4500
001 2157182
005 2023-10-10
008 2012 bl uuuu u00u1 u #d
100 1 $aHOFF, R.
245 $aThe geology in the context of geographical indications of fine wines in Serra Gaúcha region (Brazil).$h[electronic resource]
260 $aCONGRES DES TERROIRS VITIVINICOLES. 9., 2012, Bourgogne, France. Actes... Bourgogne, Dijon; Champgne, Reims, CIVC, 25 a 29 Juin 2012.$c2012
300 $a8-41
520 $aIn Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors of natural factors. To construct the geological sketch, photo-interpretation techniques were employed high-resolution aerial photos associated with field work. The digital image processing was used to construct the digital elevation model from high resolution orbital data and its derivatives such as altimetry, slope and exposure, as well as the geological structures and land forms.
650 $aEnologia
650 $aUva
650 $aViticultura
653 $aGeology and wine
653 $aIndicação geográfica
653 $aPinto Bandeira
653 $aRio Grande do Sul
653 $aWine terroir
653 $aZoneamento
700 1 $aFALCADE, I.
700 1 $aTONIETTO, J.
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