In this study we investigated the effect of the grape withering process occurring during the production of Italian passito wines on the variability of the (D/H)I, (D/H)II, δ13C, and δ18O of wine ethanol and the δ18O of wine water. The production of PDO Erbaluce di Caluso Passito in five different cellars in Piedmont (Italy) was considered in two successive years. Moreover, samples of 17 different traditional Italian passito wines taken at different stages of maturation were taken into account. We found that the δ18O of must and wine water and the δ18O of ethanol decrease in the case of passito wines produced in northern and central Italy using postharvest drying of the grapes in dedicated ventilated or unventilated fruit drying rooms ( f ruttaio), during autumn−winter. For passito wines produced in southern Italy, where the main technique involves withering on the plant (en plein air), δ18O tends to increase. The (DH)I of wine ethanol did not change during withering, whereas the (DH)II and δ13C values changed slightly, but without any clear trend. Particular attention must be therefore paid in the evaluation of the δ18O data of passito wines for fraud detection.

Perini, M., Rolle, L., Franceschi, P., Simoni, M., Torchio, F., Di Martino, V., Marianella, R. M., Gerbi, V., Camin, F., H, C, and O Stable Isotope Ratios of Passito Wine, <<JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY>>, 2015; 2015 (63): 5851-5857. [doi:10.1021/acs.jafc.5b02127] [http://hdl.handle.net/10807/68338]

H, C, and O Stable Isotope Ratios of Passito Wine

Marco; Torchio;
2015

Abstract

In this study we investigated the effect of the grape withering process occurring during the production of Italian passito wines on the variability of the (D/H)I, (D/H)II, δ13C, and δ18O of wine ethanol and the δ18O of wine water. The production of PDO Erbaluce di Caluso Passito in five different cellars in Piedmont (Italy) was considered in two successive years. Moreover, samples of 17 different traditional Italian passito wines taken at different stages of maturation were taken into account. We found that the δ18O of must and wine water and the δ18O of ethanol decrease in the case of passito wines produced in northern and central Italy using postharvest drying of the grapes in dedicated ventilated or unventilated fruit drying rooms ( f ruttaio), during autumn−winter. For passito wines produced in southern Italy, where the main technique involves withering on the plant (en plein air), δ18O tends to increase. The (DH)I of wine ethanol did not change during withering, whereas the (DH)II and δ13C values changed slightly, but without any clear trend. Particular attention must be therefore paid in the evaluation of the δ18O data of passito wines for fraud detection.
Inglese
Perini, M., Rolle, L., Franceschi, P., Simoni, M., Torchio, F., Di Martino, V., Marianella, R. M., Gerbi, V., Camin, F., H, C, and O Stable Isotope Ratios of Passito Wine, <<JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY>>, 2015; 2015 (63): 5851-5857. [doi:10.1021/acs.jafc.5b02127] [http://hdl.handle.net/10807/68338]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10807/68338
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