Terroir 1996 banner
IVES 9 IVES Conference Series 9 Definition of functional indicators of the vine to characterize wine terroirs

Definition of functional indicators of the vine to characterize wine terroirs

Abstract

La caractérisation des terroirs viticoles est traditionnellement basée sur des descripteurs de la géologie et de la pédologie des différents milieux rencontrés, couplées à des données climatiques. Cette approche peut être efficacement complétée par une description fonctionnelle, basée sur des indicateurs d’état de la vigne. Les facteurs du milieu (somme de température, alimentation hydrique, richesse minérale … ) déterminent la phénologie et le niveau des productions végétales. Mais la connaissance des caractéristiques du milieu ne permet pas a priori de repérer la combinaison effectivement déterminante. Le potentiel d’un vignoble est évalué sur le produit final: la baie de raisin, et non par la seule caractérisation physique du sol (méthode nécessaire mais pas suffisante). L’utilisation de variables intermédiaires entre les facteurs du milieu et la caractérisation des raisins permet une meilleure appréciation des terroirs.
Nous proposons trois indicateurs pouvant servir à l’exploration de la qualité au sein d’une appellation: l’abondance en 13C naturel des sucres pour l’estimation de la contrainte hydrique, le dosage de l’azote dans les feuilles et les moûts pour l’estimation de la contrainte azotée, le poids de bois de taille directement relié à la surface foliaire (relations allométriques ), pour l’estimation de la vigueur de la plante. L’objectif est de disposer d’outils rapides et faciles d’accès, contribuant à une cartdgraphie fonctionnelle du vignoble. Ces outils permettent d’étudier la part prise par les différents facteurs impliqués dans la constitution de la qualité de la baie de raisin, au cours d’un cycle végétatif, pour le terroir considéré.

Characterization of terroirs is traditionally based on descriptors of the geology and pedology of various soils surrounding, coupled to climatic data. This approach can effectively be supplemented by a functional description, based on indicators of statè of the vineyard. The factors of the environment (thermal time, water availability, mineral richness … ) fix the phenology and the level of the productions. But the knowledge of the characteristics of the environment does not a priori allow to track down the effectively determining combination.
The potential of a vineyard is evaluated on the end product: the grape berry, and not by the only physics characterization of the soils (necessary but not sufficient method). The use of intermediate variables between the factors of the environment and the characterization of the grapes allows a better appreciation of the soils.

We propose three indicators being able to be used for the browsing of quality within, an appelation: the abundance in natural 13C of sugars for the estimate of the water restriction, the measurement of the amount of nitrogen in leaves and musts for estimate of the nitrogenous constraint, the pruning weights directly linked to the leaf aera (allometric relations), for estimate of the vigor of the plant. The objective is to have fast and easily accessible tools, contributing to a functional cartography of the vineyard. These tools make possible to study the share of the various factors implicated in the constitution of the grape berry quality, during a vegetative cycle, for the terroir considered.

 

 

 

DOI:

Publication date: February 15, 2022

Issue: Terroir 2002

Type: Article

Authors

GOUTOULY, J.-P. (1), SOYER, J.-P. (1), VAN LEEUWEN C. (2) and GAUDILLERE J.-P (1)

(1) INRA-AGRONOMIE, Ecophysiologie & Agronomie Viticole, 71, avenue Edouard Bourleaux – B.P.81 33883 Villenave d’Ornon cedex
(2) ENITA de Bordeaux, 1 cours du Général de Gaulle, BP 201, 33175 Gradignan cedex

Keywords

Vigne, déficit hydrique, discriminations isotopique, ?C13, biomasse, alimentation azotée, sol, terroir
Vine, water deficit, isotope discrimination,? C13, biomass, nitrogen supply, soil, terroir

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

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…

Assessment of climate change impacts on water needs and growing cycle on grapevine in three DOs of NE Spain

This study assessed the suitability of grapevine growing in three DOs (Empordà, Pla de Bages and Penedès) of Catalonia (NE Spain) over the 21st century. For this purpose, an estimation of water needs and agroclimatic and phenological indicators was made. Climate change impacts were estimated at 1 km pixel resolution using temperature and precipitation projections from several general circulation models (GCM) and two climate change scenarios: RCP 4.5 (stabilization scenario) and RCP 8.5 (worst-case scenario). Potential crop evapotranspiration (following FAO procedure) and a daily water balance considering soil water holding capacity were used to estimate actual evapotranspiration of vines and, finally, water needs. Dynamics would be similar in the three DOs studied although the magnitude of impact differs. Water needs would be 2 and 3 times greater (ranging from 0 to more than 1500 m3/ha) than current water needs at both climate change scenarios. Moreover, blooming date would advance from 3 to 6 weeks, harvest date from 1 to 2.5 months, resulting in growing cycles from 10 to 80 days shorter. It should also be noted that frost risk would decrease from 6 to 76%, the number of days with temperatures above 30ºC during ripening would rise from 48 to 500% and tropical nights (minimum temperature >20ºC) at ripening would increase from 28 to 150%, depending on the scenario and the DOs. The impacts of climate change in the three DOs could result in significant limitations for grapevine cultivation and wine production if adaptive strategies are not applied. This result could serve as a basis for the design of specific and particular adaptation strategies to improve and maintain vineyards in the DOs studied and could be extrapolated to similar DOs and regions.

Grapevine xylem embolism resistance spectrum reveals which varieties have a lower mortality risk in a future dry climate

Wine growing regions have recently faced intense and frequent droughts that have led to substantial economical losses, and the maintenance of grapevine productivity under warmer and drier climate will rely notably on planting drought-resistant cultivars. Given that plant growth and yield depend on water transport efficiency and maintenance of photosynthesis, thus on the preservation of the vascular system integrity during drought, a better understanding of drought-related hydraulic traits that have a significant impact on physiological processes is urgently needed. We have worked towards this end by assessing vulnerability to xylem embolism in 30 grapevine commercial varieties encompassing red and white Vitis vinifera varieties, hybrid varieties characterized by a polygenic resistance for powdery and downy mildew, and commonly used rootstocks. These analyses further allowed a global assessment of wine regions with respect to their varietal diversity and resulting vulnerability to stem embolism. Hybrid cultivars displayed the highest vulnerability to embolism, while rootstocks showed the greatest resistance. Significant variability also arose among Vitis vinifera varieties, with Ψ12 and Ψ50 values ranging from -0.4 to -2.7 MPa and from -1.8 to -3.4 MPa, respectively. Cabernet franc, Chardonnay and Ugni blanc featured among the most vulnerable varieties while Pinot noir, Merlot and Cabernet Sauvignon ranked among the most resistant. In consequence, wine regions bearing a significant proportion of vulnerable varieties, such as Poitou-Charentes, France and Marlborough, New Zealand, turned out to be at greater risk under drought. These results highlight that grapevine varieties may not respond equally to warmer and drier conditions, outlining the importance to consider hydraulic traits associated with plant drought tolerance into breeding programmes and modeling simulations of grapevine yield maintenance under severe drought. They finally represent a step forward to advise the wine industry about which varieties and regions would have the lowest risk of drought-induced mortality under climate change.

Rootstock regulation of scion phenotypes: the relationship between rootstock parentage and petiole mineral concentration

Grapevine is grown as a graft since the end of the 19th century. Rootstocks not only provide tolerance to Phylloxera but also ensure the supply of water and mineral nutrients to the scion. Rootstocks are an important mean of adaptation to environmental conditions, because the scion controls the typical features of the grapes and wine. However, among the large diversity of rootstocks worldwide, few of them are commercially used in the vineyard. The aim of this study was to investigate the extent to which rootstocks modify the mineral composition of the petioles of the scion. Vitis vinifera cvs. Cabernet-Sauvignon, Pinot noir, Syrah and Ugni blanc were grafted onto 55 different rootstock genotypes and planted in a vineyard as three replicates of 5 vines. Petioles were collected in the cluster zone with 6 replicates per combination. Petiolar concentrations of 13 mineral elements (N, P, K, S, Mg, Ca, Na, B, Zn, Mn, Fe, Cu, Al) at veraison were determined. Scion, rootstock and the interaction explained the same proportion of the phenotypic variance for most mineral elements. Rootstock genotype showed a significant influence on the petiole mineral element composition. Rootstock effect explained from 7 % for Cu to 25 % for S of the variance. The difference of rootstock conferred mineral status is discussed in relation to vigor and fertility. Rootstocks were also genotyped with 23 microsatellite markers. Data were analysed according to genetic groups in order to determine whether the petiole mineral composition could be related to the genetic parentage of the rootstock. Thanks to a highly powerful design, it is the first time that such a large panel of rootstocks grafted with 4 scions has been studied. These results give the opportunity to better characterize the rootstocks and to enlarge the diversity used in the vineyard.

Influence of agronomic practices in soil water content in mid-mountain vineyards

In the context of LIFE project MIDMACC (LIFE18 CCA/ES/001099), several pilots have been installed in vineyards in mid mountain areas of Catalonia (NE Spain) to test well stablished agronomic practices to increase the adaptation of Mediterranean mid mountain to climate change. Soil water content (SWC) at three different depths (15, 30 and 45cm) was measured in continuum from August 2020. One pilot (WC) included a well-established green cover (GC), a new GC (NC) and a conventional soil management (CM, tilling+herbicides). NC presented an intermediate state between WC and CM, responding similarly to CM in autumn but quickly reaching similar SWC to WC, then following the same evolution till next spring, with CM presenting lower values along autumn and winter. Then vegetation activation decreased SWC in all plots, (much slower in CM, lacking GC). Sensibility to spring rains is again intermediate for NC, which joins SWC evolution of CM by the end of spring till next autumn. It is expected that NC will resemble WC more and more as its GC develops. In the pilot combining vine training (VSP vs Gobelet) and hillside management (slope vs terrace), no clear pattern could be related with these conditions. However, both terraces seem to be more sensitive to spring rains. A third pilot included new vineyards (7 and 1 year old). In the new vineyard (N), higher canopy development, a spontaneous green cover and row straw resulted in a slower SWC dynamic, not so sensitive to rains but conserving more soil water in spring and most of summer, even with presumably a higher water extraction by vines. In the newest vineyard (VN) the deepest sensor is still sensitive to rain events all over the year and SWC is always highest at this depth, revealing small water capture by vines.