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| Registros recuperados : 147 | |
| 22. |  | HOFF, R.; DUCATI, J. R.; BERGMANN, M. Geologic and geomorphologic features applied for identification of wine terroir unit by digital image processing, spectroradiometric and GIS techniques in Encruzilhada do Sul, RS, Brazil. In: INTERNATIONAL TERROIR CONGRESS, 8., Soave, 2010. Proceedings... Conegliano: CRA-VIT, 2010. p. 44-49. 1 CD-ROM.| Biblioteca(s): Embrapa Uva e Vinho. |
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| 23. | | HOFF, R.; FALCADE, I.; TONIETTO, J. The geology in the context of geographical indications of fine wines in Serra Gaúcha region (Brazil). CONGRES DES TERROIRS VITIVINICOLES. 9., 2012, Bourgogne, France. Actes... Bourgogne, Dijon; Champgne, Reims, CIVC, 25 a 29 Juin 2012. 8-41| Biblioteca(s): Embrapa Uva e Vinho. |
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| 24. | | ALBERTI, R.; PAULETTO, H.; HOFF, R. Geotecnologias para atualização de uma década de dados de uso da terra e para identificação de áreas de preservação permanente na região vitivinícola Serra Gaúcha, Brasil. In: ENCONTRO DE INICIAÇÃO CIENTÍFICA, 14. ENCONTRO DE PÓS-GRADUANDOS DA EMBRAPA UVA E VINHO, 10., 2016, Bento Gonçalves. Resumos...Bento Gonçalves, RS: Embrapa uva e Vinho, 2016. p. 76. (Embrapa Uva e Vinho. Documentos, 99)| Biblioteca(s): Embrapa Uva e Vinho. |
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| 26. | | PAULETTO, H.; JUNGES, A. H.; HOFF, R. Imagens de média e alta resolução espacial como apoio à viticultura de precisão: variabilidade do índice de vegetação por diferença normalizada em vinhedo da região da Campanha, Brasil. In: ENCONTRO DE INICIAÇÃO CIENTÍFICA, 16.; ENCONTRO DE PÓS-GRADUANDOS DA EMBRAPA UVA E VINHO, 12., 2018, Bento Gonçalves. Anais... Bento Gonçalves, RS: Embrapa Uva e Vinho, 26 a 27 de setembro de 2018. p. 11. (Embrapa Uva e Vinho. Documentos, 108)| Biblioteca(s): Embrapa Uva e Vinho. |
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| 29. | | HOFF, R.; ALBERTI, R.; PAULETTO, H. Caracterização física de terroir pela geologia e geomorfologa na região vitivinícola serra do sudeste, Brasil. In: SIMPÓSIO NACIONAL DE ESTUDOS TECTÔNICOS, 17.; INTERNATIONAL SYMPOSIUM ON TECTONICS, 11.; SIMPÓSIO SUL-BRASILEIRO DE GEOLOGIA, 11., 2019, Bento Gonçalves, RS. Anais... Beno Gonçalves: XVII SNET: XI SSBG, 2019. p. 424.| Biblioteca(s): Embrapa Uva e Vinho. |
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| 35. | | JUNGES, A. H.; ANZANELLO, R.; HOFF, R. Perfil temporal de índice de vegetação obtido por sensor remoto ativo em vinhedos "Chardonnay" em Veranópolis, Brasil. In: CONGRESSO LATINO-AMERICANO DE VITICULTURA E ENOLOGIA, 15.; CONGRESSO BRASILEIRO DE VITICULTURA E ENOLOGIA, 13., 2015, Bento Gonçalves. Resumos... Bento Gonçalves: Embrapa Uva e Vinho: Associação Brasileira de Enologia, 2015. p. 527. XV Congresso Latino-Americano de Viticultura e Enologia E XIII Congresso Brasileiro de Viticultura e Enologia. Bento Gonçalves-RS, 3 a 7 de Novembro de 2015.| Biblioteca(s): Embrapa Uva e Vinho. |
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| Registros recuperados : 147 | |
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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: |
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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
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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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Embrapa Uva e Vinho (CNPUV) |
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