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Increase in the oxygen stable isotopic composition of water in wine with low ethanol yield. | LitMetric

AI Article Synopsis

  • The stable isotopic composition of oxygen (δO) in wine helps determine its geographic origin and water dilution levels, but little is known about how winemaking techniques like acidification and chaptalization affect these values.
  • The study finds that while acidification and chaptalization have minor direct impacts on δO, they cause indirect variations through changes in ethanol yield, potentially altering δO by up to 0.6‰.
  • It is revealed that lower ethanol yields during fermentation lead to higher δO values due to yeast releasing water with high δO, while also indicating that yeast growth reduces ethanol yield by consuming amino acids.

Article Abstract

The stable isotopic composition of oxygen (δO) in wine is often analysed to determine the geographic origin of the wine and the amount of water dilution. However, little is known regarding the effects of two major winemaking techniques (the addition of acid (acidification) and sugar (chaptalization)) on the δO value of water in wine. Here we show that acidification and chaptalization have minor direct effects on the δO value but indirect effects based on the ethanol yield, which causes isotopic variation of up to 0.6‰. During fermentation, δO values increase at low ethanol yields, suggesting that yeast release water with a high δO value into wine when consuming sugars. Additionally, the ethanol yield is negatively correlated with the consumption of amino acids by the yeast, indicating that yeast growth decreases the ethanol yield. We therefore identify ethanol yield, which is decreased by the consumption of sugars by yeast for non-alcohol-fermentation processes as a potential factor leading to variations in the δO value of water during the winemaking process.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6667440PMC
http://dx.doi.org/10.1038/s41598-019-47331-0DOI Listing

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