Abstract
Wine oxidation is catalysed by iron (Fe). Fe(II) is oxidized by oxygen to produce Fe(III), which oxidizes reductants, such as polyphenols, thereby returning to the ferrous state. Therefore, Fe redox cycles and the [Fe(III)]:[Fe(II)] ratio depends on the relative rates of Fe(II) oxidation and Fe(III) reduction. Under reducing conditions Fe(II) dominates but with increasing oxygen exposure the proportion of Fe as Fe(III) increases. Reduction potentials have been used for many years to determine the redox state of wines. However, it is now realized that these potentials are mainly due to oxidation of ethanol on platinum electrodes and not due to the oxidative processes that normally occur in wine. It is proposed that [Fe(III)]:[Fe(II)] ratios may provide an alternative way of estimating the redox state. These ratios have been obtained using Ferrozine to determine Fe(II) and total Fe concentration spectroscopically in white wines. However, Ferrozine cannot be used in red wine due to color interference. A similar method using Br-PAPS, which is water soluble and the Fe(II) complex of which absorbs outside the red wine absorption range, has therefore been developed with minimal wine disturbance so as not to alter ratios. High Fe(II) content (~97%) was observed in bottled wine with screwcap, technical and plastic closures. Lower proportions of Fe(II) were found with natural corks and wine boxes. [Fe(III)]: [Fe(II)] ratios increased on oxygen exposure. Calculated reduction potentials of the Fe-couple did not correspond to those that would be measured for wines, providing further evidence that these wine potentials are not true reduction potentials.
- Received September 2017.
- Revision received November 2017.
- Accepted November 2017.
- Published online December 2017
- ©2017 by the American Society for Enology and Viticulture
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