 IVES 9 IVES Conference Series 9 Inhibition of reductive characters in wine by cu-organic acids: predicting the duration of protection

Inhibition of reductive characters in wine by cu-organic acids: predicting the duration of protection

Abstract

Cu organic acid complexes efficiently bind hydrogen sulfide in wine and therefore prevent its accumulation and subsequent reductive off-flavour [1]. This fraction of Cu can also bind methanethiol, the other main contributor to reductive wine characters, albeit with less efficient binding than for hydrogen sulfide [1]. However, during bottle aging of wine, the concentration of Cu organic acid complexes gradually decline and the sulfide-bound form of Cu increases. The point at which the Cu organic acid concentration is depleted signifies a potential for reductive aroma development to occur. The aim of this study is ascertain how long Cu organic acid complexes in wine can offer a protection against the reductive aroma compounds. High (0.6 mg/L), medium (0.3 mg/L) and no (0 mg/L) Cu(II) additions were made to Pinot Grigio and Chardonnay wines at bottling, and the bottled wines were then stored at 14 °C in darkness. Analysis was performed on the wines at 0, 2, 4, 8 and 12-14 months after bottling. Throughout bottle ageing process, the concentrations of three different Cu fractions, attributed to Cu organic acid complexes, Cu thiol complexes and sulfide-bound Cu, were monitored by stripping potentiometry and colorimetric methods. The free and salt-releasable concentration of hydrogen sulfide and methanethiol were determined by gas chromatography with chemiluminescene detection. Sensorial analysis was also performed on the wines after 12 months. During the first 2-months of bottle aging of all wines, the Cu-organic acid concentrations initially remained stable or increased, as total packed oxygen was consumed. Afterwards, during the low oxygen aging phase of the wines, the Cu-organic acid concentration declined exponentially with a concomitant increase in sulfide-bound Cu. These changes in sulfide-bound Cu were matched by an increase the salt-releasable hydrogen sulfide concentrations of the wines during aging. Free concentrations of hydrogen sulfide and methanethiol were only found to accumulate in wines without any Cu-organic acid present at bottling. For the Pinot Grigio without Cu-organic acid present at bottling (i.e., the no Cu addition treatment), the free methanethiol concentrations in the wine were above the aroma threshold and this wine was assessed as reductive. Alternatively, for the Pinot Grigio with Cu-organic acid complexes at bottling, only concentrations of free methanethiol below the aroma threshold were measured and the wine was not reductive. The decay in Cu-organic acid complexes, in the low oxygen aging phase of the wines, were found to follow first order kinetics that were similar for the Chardonnay and the Pinot Grigio. These results enable determination of the time-frame that Cu-organic acids can offer white wine protection against the potential accumulation of reductive aroma compounds.

DOI:

Publication date: September 14, 2021

Issue: Macrowine 2021

Type: Article

Authors

Xinyi Zhang

National Wine and Grape Industry Centre, Charles Sturt University, Wagga Wagga, Australia,Nikolaos KONTOUDAKIS (Laboratory of Enology and Alcoholic Drinks, Department of Food Science and Human Nutrition, Agricultural University of Athens) John W. BLACKMAN (National Wine and Grape Industry Centre, Charles Sturt University) Andrew C. CLARK (National Wine and Grape Industry Centre, Charles Sturt University)

Contact the author

Keywords

cu organic acid complexes, hydrogen sulfide accumulation, white wine bottle ageing

Citation

δ¹³C : A still underused indicator in precision viticulture

The first demonstration of the interest of carbon isotope composition of sugars in grapevine, as an integrated indicator of vineyard water status, dates back to 2000 (Gaudillère et al., 1999; Van Leeuwen et al., 2001). Thanks to the isotopic discrimination of Carbon that takes place during plant photosynthesis, under hydric stress conditions, it is possible to accurately estimate the photosynthetic activity. Ever since, δ13C has been widely applied with success to zonation, terroir studies and vine physiology research, but is still not widely used by viticulturists. This is quite astonishing by considering the impact of global warming on viticulture and the need to improve water management, that would justify a widespread use of δ13C.
The lack of private laboratories proposing the analysis, the cost of the technology, as well as the long analytical delays, have been detrimental to its development. Some laboratories tried to overcome the analytical difficulties of isotopic analysis by using fourier transformed infrared spectroscopy, as a fast and cheap alternative to the official OIV method (IRMS). These claimed FTIR models have never been published or peer reviewed and cannot be considered robust. In this work, thanks to the recent acquisition of IRMS technology, new modern and robust applications of δ13C for viticulture are proposed. This includes the use of the analysis to make parcel separations at harvesting, the possibility to increase the precision of hydric stress cartography and the potential cost reduction when compared with Scholander pressure bomb analysis.

Climate, Viticulture, and Wine … my how things have changed!

The planet is warmer than at any time in our recorded past and increasing greenhouse emissions and persistence in the climate system means that continued warming is highly likely. Climate change has already altered the basic framework of growing grapes for wine production worldwide and will likely continue to do so for years to come. The wine sector can continue to play an important role in leading the agricultural sector in addressing climate change. From developing on…

Making sense of available information for climate change adaptation and building resilience into wine production systems across the world

Effects of climate change on viticulture systems and winemaking processes are being felt across the world. The IPCC 6thAssessment Report concluded widespread and rapid changes have occurred, the scale of recent changes being unprecedented over many centuries to many thousands of years. These changes will continue under all emission scenarios considered, including increases in frequency and intensity of hot extremes, heatwaves, heavy precipitation and droughts. Wine companies need tools and models allowing to peer into the future and identify the moment for intervention and measures for mitigation and/or avoidance. Previously, we presented conceptual guidelines for a 5-stage framework for defining adaptation strategies for wine businesses. That framework allows for direct comparison of different solutions to mitigate perceived climate change risks. Recent global climatic evolution and multiple reports of severe events since then (smoke taint, heatwave and droughts, frost, hail and floods, rising sea levels) imply urgency in providing effective tools to tackle the multiple perceived risks. A coordinated drive towards a higher level of resilience is therefore required. Recent publications such as the Australian Wine Future Climate Atlas and results from projects such as H2020 MED-GOLD inform on expected climate change impacts to the wine sector, foreseeing the climate to expect at regional and vineyard scale in coming decades. We present examples of practical application of the Climate Change Adaptation Framework (CCAF) to impacts affecting wine production in two wine regions: Barossa (Australia) and Douro (Portugal). We demonstrate feasibility of the framework for climate adaptation from available data and tools to estimate historical climate-induced profitability loss, to project it in the future and to identify critical moments when disruptions may occur if timely measures are not implemented. Finally, we discuss adaptation measures and respective timeframes for successful mitigation of disruptive risk while enhancing resilience of wine systems.

Climate projections over France wine-growing region and its potential impact on phenology

Climate change represents a major challenge for the French wine industry. Climatic conditions in French vineyards have already changed and will continue to evolve. One of the notable effects on grapevine is the advancing growing season. The aim of this study is to characterise the evolution of agroclimatic indicators (Huglin index, number of hot days, mean temperature, cumulative rainfall and number of rainy days during the growing season) at French wine-growing regions scale between 1980 and 2019 using gridded data (8 km resolution, SAFRAN) and for the middle of the 21th century (2046-2065) with 21 GCMs statistically debiased and downscaled at 8 km. A set of three phenological models were used to simulate the budburst (BRIN, Smoothed-Utah), flowering, veraison and theoretical maturity (GFV and GSR) stages for two grape varieties (Chardonnay and Cabernet-Sauvignon) over the whole period studied. All the French wine-growing regions show an increase in both temperatures during the growing season and Huglin index. This increase is accompanied by an advance in the simulated flowering (+3 to +9 days), veraison (+6 to +13 days) and theoretical maturity (+6 to +16 days) stages, which are more noticeable in the north-eastern part of France. The climate projections unanimously show, for all the GCMs considered, a clear increase in the Huglin index (+662 to 771 °C.days compared to the 1980-1999 period) and in the number of hot days (+5.6 to 22.6 days) in all the wine regions studied. Regarding rainfall, the expected evolution remains very uncertain due to the heterogeneity of the climates simulated by the 21 models. Only 4 regions out of 21 have a significant decrease in the number of rainy days during the growing season. The two budburst models show a strong divergence in the evolution of this stage with an average difference of 18 days between the two models on all grapevine regions. The theoretical maturity is the most impacted stage with a potential advance between 40 and 23 days according to wine-growing regions.

Legacy of land-cover changes on soil erosion and microbiology in Burgundian vineyards

Soils in vineyards are recognized as complex agrosystems whose characteristics reflect complex interactions between natural factors (lithology, climate, slope, biodiversity) and human activities. To date, most of the unknown lies in an incomplete understanding of soil ecosystems, and specifically in the microbial biodiversity even though soil microbiota is involved in many key functions, such as nutrient cycling and carbon sequestration. Soil biological properties are indicative of soil quality. Therefore, understanding how soil communities are related to soil ecosystem functioning is becoming an essential issue for soil strategy conservation. Here, we propose to assess the importance of land-cover history on the present-day microbiological and physico-chemical properties. The studied area was selected in the Burgundian vineyards (Pernand-Vergelesses, Burgundy, France) where land occupation has been reconstructed over the last 40 years. Soil samples were collected in five areas reflecting various land cover history (forest, vineyards, shifting from forest to vineyards). For each area, physico-chemical parameters (pH, C, N, P, grain size) were measured and DNA was extracted to characterize the abundance and diversity of microbial communities. The obtained results show significant differences in the five areas suggesting that present-day microbial molecular biomass and bacterial taxonomic is partly inherited from past land occupation. Over longer period of time, such study of land-uses legacies may help to better assess ecosystem recovery and the impact of management practices for a better soil quality and vineyards sustainability.