Enoforum 2021
IVES 9 IVES Conference Series 9 Enoforum Web 9 Enoforum Web Conference 2021 9 Cellar session 9 Adaptation of Lactobacilli towards low ph and SO2 to develop MLF in base musts for sparkling wines

Adaptation of Lactobacilli towards low ph and SO2 to develop MLF in base musts for sparkling wines

Abstract

In some white wines, malolactic fermentation (MLF) is very interesting, and for low pH wines this process is particularly difficult. Although MLF is generally not recommended for sparkling white wine, some winemakers prefer to promote MLF to contribute to organoleptic complexity. Oenococcus oeni is generally the bacterium of choice for MLF. However, people’s interest in other species (such as Lactobacillus) is increasing. However, one disadvantage of lactobacilli is that they are more sensitive to low pH and SO2, and some producers of starters inoculate high doses of non-growing bacteria in grape musts. This work aims to grow some selected strains of Lactobacillus in grape juice and perform early MLF. With this strategy, beyond performing the MLF homolactic bacteria can contribute clearly to maintain or even decrease the final pH in wines by producing lactic acid from sugars; they also produce more complex wines, and prevent the spoilage of an undesired late MLF in bottles. 

To perform this selection, twelve Lactobacillus strains were successively inoculated after adapting to the lowering of pH and the increasing concentration of SO2. The cell concentration of the inoculum was in the order of x 106 CFU/mL to allow growth and synthesis of lactic acid. All Lactobacillus strains gradually adapted to low pH and SO2 and could grow at pH 3.2 and the highest SO2 concentration, thereby maintaining or even increasing their final biomass. After 7 days, all strains always underwent MLF. Malic acid consumption rate and lactic acid production depend on the strain. The final pH of wines was maintained or even decreased, even when complete MLF was achieved. This strategy helps in biological acidification of wines against the loss of acidity derived from climate change.

DOI:

Publication date: April 23, 2021

Issue: Enoforum 2021

Type: Article

Authors

FERRER Sergi, POLO Lucía, ANDRÉS Lorena, PARDO Isabel

Institut de Biotecnologia i Biomedicina (BioTecMed), Universitat de València, Spain

Contact the author

Tags

Enoforum 2021 | IVES Conference Series

Citation

Related articles…

Studying PIWIs in three dimensions: agronomic, economic and ecological evaluation of 14 fungus-tolerant cultivars in Luxembourg

Growing fungus-tolerant cultivars (PIWIs) reduces the need of fungicide use by 50-80 %. PIWIs have the potential to address climate change adaptation and mitigation simultaneously.

Market analysis of Chilean Pinot noir, Carménère, and Cabernet-Sauvignon wines: A comparative study of chemical parameters across low, medium, and high price segments

Wine quality is a complex concept determined by multiple factors, including vineyard management, winemaking operations, and the sensory perception of key attributes.

INFLUENCE OF THE NITROGEN / LIPIDS RATIO OF MUSTS ON THE REVELATION OF AROMATIC COMPOUNDS IN SAUVIGNON BLANC WINE

Production of volatile compounds by yeast is known to be modulated by must nitrogen. Nevertheless, various parameter of must quality have an impact on yeast fermentation. In this study we propose to evaluate the impact of nitrogen / lipids balance on a Sauvignon Blanc grape juice (Val de Loire).
Must was prepared from the same grapes at pilot scale. Three modalities were carried out: direct pressing, direct pressing with a pre-fermentation cold stabulation and pellicular maceration before pressing.

A.O.C. huile d’olive de Nyons et olives noires de Nyons

A.O.C. huile d’olive de Nyons et olives noires de Nyons

Results of late-wurmian to present-day climatic-geological evolution on to spatial variability of pedologic-geological characters of the AOC Gaillac terroirs (Tarn, Midi-Pyrénées)

The AOC Gaillac area is divided into three main terroirs : « The left bank terraces », « The right bank coteaux » and
« The plateau Cordais ». This division is valid at a regional scale, but it suffers of a number of local-scale exceptions. This spatial variability of the pedologic-geologic characteristics at the plot scale has been derived mainly from the main late-Würmian solifluxion phase occurring at the transition between the peri-glacial climate and the Holocene temperate conditions (13,000-10,000 yrs BP).