The limonene-derived mint aroma compounds in red wines. Recent advances on analytical, chemical aspects and sensory aspects

The addition of fungal chitosan in wine is allowed since 2009 to release some spoilage microorganisms such as Brettanomyces bruxellensis (OIV/OENO 338A/2009; EC 53/2011).

The evolution of wine during bottle ageing has been of great interest to ensure consistent quality over time. While the role of wine closures on the amount of oxygen is well-known [1], closures could also play other roles such as the scalping phenomenon of flavour compounds. Flavour scalping has been described as the sorption of flavour compounds by the packaging material, which could result in losses of flavour intensity. It has been reported in the literature that volatile sulphur compounds (VSC) can be scalped on wine closures depending on the type of closure (traditional and agglomerated cork, screw-cap, synthetic [2]).

Water nutrition is crucial for wine grape performance. Thus soil investigation aims at characterizing spatial and temporal variability of available water. A possible strategy

Besides location and microclimatic conditions, soil plays an important role in the quality of grapes and wine. Soil properties influence the soil water holding capacity, the vegetative growth and the vine water status. Moreover, it is known that the vine water status affects the grape quality, such as concentration and structural characteristics of phenols. In a relatively small area of the Vipava Valley, soil profiles were described on terraced and flat vineyards in the valley bottoms (n=5). Texture, pH, organic matter, available phosphorus, potassium and magnesium were determined for each soil horizon in the soil profile. Viticultural parameters (number of buds, clusters and leaf area) were standardised. Stem water potential (SWP) was measured during the growing season and grapes were randomly sampled during ripening in 2019. The content and structural characteristics of proanthocyanidins were determined in grape skins and seeds. On terraces, SWP was predominantly more negative than on flat vineyards, probably mainly due to the soil ability to retain water. Vineyards on flysch terrace soils consist of up to 90% coarse material and therefore contain less organic matter than the dense and largely non-skeletal loamy alluvial soils of flat vineyards. These two extreme groups of vineyards in the same vine-growing area differ considerably in morphology and soil profile characteristics, as well as microclimatic conditions and relief. The diversity of vineyards is reflected, among other things, in the grape quality. Higher concentration of anthocyanins in the skins and higher galloylation of seed proanthocyanidins was found in grapes from terraced vineyards. Understanding relationships between site, soil and the phenolic ripening of grapes is crucial for determining the best vineyard sites and thus for characterising terroirs suitable for high quality wines.

Yeast species S. cerevisiae, S. uvarum, S. kudriavzevii and their hybrids present clear metabolic differences, even when we compared S. cerevisiae wine versus wild strain. These species and hybrids produced significantly higher amounts of glycerol, organic acids, 2,3-butanediol, and 2-phenyl ethanol and a reduction of the ethanol yield, properties very interesting in the sector to deal with climate change effects. To understand the existing differences, we have used several omics techniques to analyze the dynamics of the (intra- and extracellular) metabolomes and/or transcriptomes of representative strains of S. cerevisiae, S. uvarum, S. kudriavzevii, and hybrids.