Determination of the geographical origin of Brazilian wines by isotope and mineral analysis

被引:50
|
作者
Dutra, S. V. [1 ,2 ]
Adami, L. [1 ]
Marcon, A. R. [1 ]
Carnieli, G. J. [1 ]
Roani, C. A. [1 ]
Spinelli, F. R. [1 ]
Leonardelli, S. [1 ]
Ducatti, C. [3 ]
Moreira, M. Z. [4 ]
Vanderlinde, R. [1 ,2 ]
机构
[1] Reference Lab Enol, IBRAVIN LAREN, BR-95084470 Caxias Do Sul, RS, Brazil
[2] UCS, Inst Biotechnol, BR-95070560 Caxias Do Sul, RS, Brazil
[3] Univ Estadual Paulista, Inst Biosci, Dept Phys & Biophys, Ctr Stable Isotopes Life Environm Sci, BR-18608000 Sao Paulo, Brazil
[4] Univ Sao Paulo, Ctr Nucl Energy Agr, Lab Isotope Ecol, BR-13400970 Sao Paulo, Brazil
关键词
Wine; Stable isotopes; Minerals; Geographical origin; DATA-BANK WINES; CLASSIFICATION; DIFFERENTIATION; SPECTROMETRY; AUTHENTICITY; FRANCE; SPAIN; NMR;
D O I
10.1007/s00216-011-5181-2
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
In the present research, we studied wines from three different south Brazilian winemaking regions with the purpose of differentiating them by geographical origin of the grapes. Brazil's wide territory and climate diversity allow grape cultivation and winemaking in many regions of different and unique characteristics. The wine grape cultivation for winemaking concentrates in the South Region, mainly in the Serra GaA(0)cha, the mountain area of the state of Rio Grande do Sul, which is responsible for 90% of the domestic wine production. However, in recent years, two new production regions have developed: the Campanha, the plains to the south and the Serra do Sudeste, the hills to the southeast of the state. Analysis of isotopic ratios of O-18/O-16 of wine water, C-13/C-12 of ethanol, and of minerals were used to characterize wines from different regions. The isotope analysis of delta O-18 of wine water and minerals Mg and Rb were the most efficient to differentiate the regions. By using isotope and mineral analysis, and discrimination analysis, it was possible to classify the wines from south Brazil.
引用
收藏
页码:1571 / 1576
页数:6
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