Terroir 1996 banner
IVES 9 IVES Conference Series 9 Settling precocity and growth kinetics of the primary leaf area: two indicative parameters of grapevine behaviour

Settling precocity and growth kinetics of the primary leaf area: two indicative parameters of grapevine behaviour

Abstract

[English version below]

Le comportement de la vigne en terme de fonctionnement thermique et hydrique, influe de manière directe sur la qualité des baies de raisin. L’effet du terroir peut être perçu à travers l’étude de paramètres tels que la précocité, la mise en place de la surface foliaire ou la vigueur. Une expérimentation a été conduite en Val de Loire sur le cépage chenin dans le but de mieux comprendre le rôle des variables liées au terroir sur la croissance et le développement de la vigne et in fine sur la qualité des baies. Le protocole, basé sur des mesures agro-viticoles et des analyses physico-chimiques réalisées entre 1997 et 2001 s’appuie sur un réseau de 5 parcelles expérimentales, établi en 1990. Ce réseau repose sur le modèle de milieu physique «roche-altération-altérite», élaboré par MORLAT (1998). Des résultats significatifs ont été mis en évidence quant à la précocité de mise en place du feuillage et la vitesse d’accroissement de la surface foliaire. La précocité d’apparition du feuillage diffère en fonction du milieu rencontré, roche, altération ou altérite, la précocité de mi-débourrement sur le milieu roche étant plus forte. La vitesse d’accroissement de la surface foliaire varie également en fonction du milieu. Les parcelles sur roche, plus précoces, ont leur vitesse d’accroissement du feuillage primaire la plus importante plusieurs semaines avant floraison. Sur milieu altérite, plus tardif, la vitesse d’installation du feuillage est significativement plus élevée quelques semaines avant la floraison, voire même durant la floraison; ce qui induit une plus forte concurrence entre le cycle végétatif et reproducteur de la vigne. Les terroirs les plus tardifs sont caractérisés par une teneur en sucres des baies plus faible. Il apparaît une corrélation négative entre une mise en place tardive du feuillage primaire, la vitesse d’accroissement de la surface foliaire et la qualité de la baie. En particulier, l’indice de maturité et le rapport acide tartrique/acide malique semblent bien discriminer les terroirs représentatifs de différents types de fonctionnement de la vigne.

The behavior of the grapevine, in terms of thermic and hydric functioning, has a direct effect on the composition of the berries at harvest time. The «terroir » effect on the vine can be approached through the study of some parameters such as the earliness of the phenological stages, the settling of the leaf area and the vigor. An experiment was conducted in the Mid- Loire valley, with the chenin variety, in order to understand better the role of the «terroir » variables on the growth and development of the vine, and in fine on the quality of the berries. The data were obtained over the period 1997-2001 out of a network of 5 experimental plots, characterized by the intensity of the weathering process of their bed-rock : from low (rock type soil) to high (weathered type soil), according to the model proposed by MORLAT (1998). All plots were managed the same way. Significative differences between terroirs were observed concerning the precocity of the establishment of the primary leaf area and its growth kinetics. The primary leaf area settled earlier on the rock type soils than on the weathered type soils. On the former, the growth kinetics reached its highest level several weeks before flowering, while on the latter; the quicker increase of the leaf area took place just a few weeks before or even during the flowering stage. On the weathered type terroirs, this late increase induces a stronger competition between the vegetative and the reproductive cycles for the photosynthetic metabolites; at that stage (fruit set), the grapevine needs still to spend much energy to build its leaf area. Regarding berry composition, terroirs corresponding to the weathered type soils were found to produce less sugars and more malic acid than the rock type terroirs. This experiment showed a negative correlation between a late settling of the leaf area, its rapid growth and the quality of the berries. Two particular indexes – the maturity index and the tartaric/malic acid ratio – seem able to discriminate the terroirs regarding their different functioning mode.

DOI:

Publication date: February 15, 2022

Issue: Terroir 2002

Type: Article

Authors

Laurence STEVEZ (1), Gérard BARBEAU (2), Yves CADOT (2), Marie-Hélène BOUVET (2), Michel COSNEAU (2), Christian ASSELIN (2)

(1) Ecole Supérieure d’ Agriculture, 55 rue Rabelais, 49007
(2) INRA-UVV, 42 rue Georges Morel, 49071 Beaucouzé Cedex

Contact the author

Keywords

vigne, surface foliaire primaire, précocité, vitesse de croissance, qualité
grapevine, ptimary leaf area, precocity, growth kinetics, quality

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Evaluation of climate change impacts at the Portuguese Dão terroir over the last decades: observed effects on bioclimatic indices and grapevine phenology

In the last decades the growers of the Portuguese Dão winegrowing region (center of Portugal) are experiencing changes in climate that are influencing either grape phenology berry health and ripening. Aiming to study the relationships between climate indices (CI), seasonal weather and grapevine phenology, in this work long-term climate and phenological data collected at the experimental vineyard of the Portuguese Dão research centre between 1958 and 2019 (61 years) for the red variety Touriga Nacional, was analyzed. The trends over time for the classical temperature-based indices (Growing Season Temperature – GST -, Growing Degree Days – GDD, Huglin Index – HI and Cool Night Index – CI) presented a significantly positive slope while the Dryness Index (DI) showed a negative trend over the last 61 years. Regarding grapevine phenology, an average advance of 4.5 days per decade in the harvest day was observed throughout the last 61 years. Consequently, the weather conditions during the ripening period have changed, showing an increasing trend over time in the average temperature (higher magnitude in the maximum than in the minimum temperature) and a decrease in the accumulated rainfall. A regression analysis showed that ~50% of harvest date variability over years was explained by the temperature-based indices variability. These observed effects of climate change on bioclimatic indices and corresponding anticipation of harvest date can still be considered advantageous for the Dão terroir as it allows to achieve an optimal berry ripening before the common equinox rains and, therefore, avoid the potential negative impacts of the rainfall on berry health and composition.

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.

Under-vine management effects on grapevine production, soil properties and plant communities in South Australia

Under-vine (UV) management has traditionally consisted of synthetic herbicide use to limit competition between weeds and grapevines. With growing global interest towards non-synthetic chemical use, this study aimed to capture the effects of alternative UV management at two commercial Shiraz vineyards in South Australia, where the sole management variables were UV management since 2016. In adjacent treatment blocks, cultivation (CU) was compared to spontaneous vegetation (SV) in McLaren Vale (MV), and herbicide was compared to SV in Eden Valley (EV). Soil water infiltration rates were slower and grapevine stem water potential was lower in CU compared to SV in MV, with the latter having a plant community dominated by soursob (Oxalis pes-caprae) during winter; while in EV, there was little separation between the treatments. Yields were affected at both sites, with SV being higher in MV and HE being higher in EV. In MV, the only effect on grape must was a lower 13C:12C isotope ratio in CU, indicating greater grapevine water stress. In the grape must at EV, SV had higher total soluble solids, total phenolics, anthocyanins, and yeast available nitrogen; and lower pH and titratable acidity. Pruning weights were not affected by the treatments in MV, while they were higher in HE at EV. Assessments revealed that the differing soil types at the two sites were likely the main determinants of the opposing production outcomes associated with UV management. In the silty loam soil of MV, the higher yields in SV were likely due to more plant-available water, as a potential result of the continuous soil bio-pores formed by winter UV vegetation. Conversely, in the loamy sand soils of EV with a lower cation exchange capacity, the lower yields and pruning weights in SV suggest the UV vegetation competed significantly with the grapevines for available water and nutrients.

Influence of a spontaneous cover crop on the vineyard and soil erosion under Mediterranean climate

Sixty five % of the agricultural area of the Basque Country located in the DO Ca Rioja corresponds to vineyards. More than 40% of it has an average slope greater than 10%, which makes it sensitive to erosive processes. Furthermore, it is foreseeable that extreme weather events (storms, hail, extreme heat and cold, etc.) will be favored due to climate change. Cover cropping can mitigate this risk, and therefore the objective of this work is to evaluate the impact that a vegetable cover has on the agronomic behavior of the vineyard, the quality of the grape and soil erosion. For this, a trial has been carried out with a Graciano variety vineyard with a slope between 10% -20% during the years 2020 and 2021. Conventional tillage management in the area has been compared (4-6 passes per year of tillage machinery) versus spontaneous vegetation cover management in the vineyard. This implies not tilling and allowing the grass of the land to colonize the range between the lines of vines, controlling their height through 1-3 mowing passes per year, always trying to affect the surface of the land as little as possible. The vegetative growth, yield and quality of the grape and wine was measured. Furthermore, erosion has been measured using Gerlasch boxes. The yield was lower in the second year of the trial in the cover crop treatment, but erosion was significantly reduced.

Late frost protection in Champagne

Probably one of the most counterintuitive impacts of climate change on vine is the increased frequency of late frost. Champagne, due to its septentrional position is historically and regularly affected by this meteorological hazard. Champagne has therefore developed a strong experience in frost protection with first experiments dating from the end of 19th century. Frost protection can be divided in two parts: passive and active. Passive protection includes all the methods that do not seek to modify the vine’s environment or resistance at the time of frost. The most iconic passive protection in Champagne is the establishment of the individual reserve. This reserve allows to stock a certain quantity of clear wine during a surplus year to compensate a meteorological hazard like frost during the following years. Other common passive methods are the control of planting area (walls, bushes, topography), the choice of grape variety, late pruning, or the impact of grass cover and tillage. Active frost protection is also divided in two parts. Most of the existing techniques tend to modify vine’s environment. Most of the time they provide warmth (candles, heaters, windmills, heating cables…), or stabilise bud’s temperature above a lethal threshold (water sprinkling). The other way to actively fight is to enhance the resistance of buds to frost (elicitors). The Comité Champagne evaluates frost protection methods following three main axes: the efficiency, the profitability, and the environmental impact through a lifecycle assessment. This study will present the results on both passive and active protection following these three axes.