Terroir 1996 banner
IVES 9 IVES Conference Series 9 Étude de la composante climatique du terroir viticole en Val de Loire : relation avec les facteurs physiques du milieu

Étude de la composante climatique du terroir viticole en Val de Loire : relation avec les facteurs physiques du milieu

Abstract

Les recherches conduites par l’U.R.V.V. du centre I.N.R.A. d’Angers ont pour but d’élaborer une méthodologie de caractérisation intégrée des facteurs naturels des terroirs viticoles, représentative des conditions de fonctionnement de la vigne et des différences sensorielles des vins. Dans ce cadre, le concept d’Unité Terroir de Base (U.T.B.) a été développé. L’U.T.B. représente une surface viticole d’extension géographique variable, définie comme l’association en un lieu donné d’une composante géologique, pédologique et paysagère, Morlat (1989), Riou et al. (1995).

La géopédologie oriente la morphologie et les conditions nutritionnelles du système racinaire, (Morlat et Jacquet, 1993), et influence profondément le fonctionnement de la vigne, (Morlat, 1989). Parallèlement, on ne peut ignorer l’effet du climat sur la qualité du raisin dans une étude globale des terroirs viticoles (Branas, 1946 ; Nigond, 1957 ; Huglin, 1978 ; Riou et al., 1994). L’environnement paysager d’un terroir peut engendrer des variations locales du climat régional (mésoclimat), suffisantes pour modifier la réponse de la vigne. Cette hypothèse a été testée avec succès par Nigond (1971) et Lebon (1993) pour des reliefs accentués ou semi-montagneux soumis à des climats tranchés (semi-continental pour Lebon, méditerranéen pour Nigond).

La plupart des éléments constitutifs d’un terroir, potentiellement modificateurs du climat, ont été étudiés isolément et le plus souvent en zones accidentée. Les effets des brise-vent ont été largement analysés et décrits par Guyot (1963) et Guyot et al. (1976). le rôle de la nature de la surface du sol sur les températures a été abordé (Branas, 1946 ; Verbrugghe, 1991). Godard (1949), Guyot et al (1976), Varlet Grancher (1975) se sont intéressés aux effets climatiques des versants, des pentes et de l’altitude. Tous ces auteurs sont d’accord sur le fait que les mésoclimats se forment principalement par ciel clair et temps calme.

La transposition de leurs résultats, indispensable pour comprendre les phénomènes climatiques locaux, est insuffisante pour prédire un mésoclimat, car celui qui se forme en un endroit résulte de l’action conjointe (convergente ou opposée) de ces multiples variables. Il est donc important d’inclure à la même échelle, et en lui donnant une dimension spatiale, la composante climatique du terroir viticole, au même titre que la composante édaphique (sol, roche géologique).

Ce travail devrait aider à hiérarchiser les facteurs locaux du climat, en vue de déceler les variables utilisables pour une cartographie climatique applicable aux zones tempérées de faible altitudes dont le relief est peu accidenté. Ce dernier objectif est fondamental pour la caractérisation intégrée des terroirs et comme outil de gestion agroviticole des vignobles.

DOI:

Publication date: March 25, 2022

Type: Poster

Issue: Terroir 1996

Authors

A. JACQUET (1), (2), R. MORLAT (1)

(1) I.N.R.A.. U.R.V.V., Angers, France
(2) Adresse actuelle : INRA – L.A.P.B.V., Université de Caen, esplanade de la paix, 14032 Caen cedex. France

Tags

IVES Conference Series | Terroir 1996

Citation

Related articles…

Phenological characterization of a wide range of Vitis Vinifera varieties

In order to study the impact of climate change on Bordeaux grape varieties and to assess the adaptation capacities of candidates to the grape varieties of this wine region to the new climatic conditions, an experimental block design composed of 52 grape varieties was set up in 2009 at the INRAE Bordeaux Aquitaine center. Among the many parameters studied, the three main phenological stages of the vine (budburst, flowering and veraison) have been closely monitored since 2012. Observations for each year, stage and variety were carried out on four independent replicates. Precocity indices have been calculated from the data obtained over the 2012-2021 period (Barbeau et al. 1998). This work allowed to group the phenological behaviour of the grapevine varieties, not only based on the timing of the subsequent developmental stages, but also on the overall precocity of the cycle and the total length of the cycle between budburst and veraison. Results regarding the variability observed among the different grape varieties for these phenological stages are presented as heat maps.

Downscaling of remote sensing time series: thermal zone classification approach in Gironde region

In viticulture, the challenges of local climate modelling are multiple: taking into account the local environment, fine temporal and spatial scales, reliable time series of climate data, ease of implementation and reproducibility of the method. At the local scale, recent studies have demonstrated the contribution of spatialization methods for ground-based climate observation data considering topographic factors such as altitude, slope, aspect, and geographic coordinates (Le Roux et al, 2017; De Rességuier et al, 2020). However, these studies have shown questions in terms of the reproducibility and sustainability of this type of climate study. In this context, we evaluated the potential of MODIS thermal satellite images validated with ground-based climate data (Morin et al, 2020). Previous studies have been encouraging, but questions remain to be explored at the regional scale, particularly in the dynamics of the massive use of bioclimatic indices to classify the climate of wine regions. The results at the local scale were encouraging, but this approach was tested in the current study at the regional scale. Several objectives were set: 1) to evaluate the downscaling method for land surface temperature time series, 2) to identify regional thermal structure variations. We used weekly minimum and maximum surface temperature time series acquired by MODIS satellites at a spatial resolution of 1000 m and downscaled at 500 m using topographical variables. Two types of analyses were performed:

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.

The impact of leaf canopy management on eco-physiology, wood chemical properties and microbial communities in root, trunk and cordon of Riesling grapevines (Vitis vinifera L.)

In the last decades, climate change required already adaptation of vineyard management. Increase in temperature and unexpected weather events cause changes in all phenological stages requiring new management tools. For example, defoliation can be a useful tool to reduce the sugar content in the berries creating differences in the wine profiles. In a ten-year field experiment using Riesling (Vitis vinifera L, planted 1986, Geisenheim, Germany), various mechanical defoliation strategies and different intensities were trialed until 2016 before the vineyard was uprooted. Wood was sampled from the plant compartments root, trunk, cordon and shoot for analyses of physicochemical properties (e.g. lignin and element content, pH, diameter), nonstructural carbohydrates and the microbial communities. The aim of the study was to investigate the influence of reduced canopy leaf area on the sink-source allocation into different compartments and potential changes of the fungal and prokaryotic wood-inhabiting community using a metabarcoding approach. Severe summer pruning (SSP) of the canopy and mechanical defoliation (MDC) above the bunch zone decreased the leaf area by 50% compared to control (C). SSP reduced the photosynthetic capacity, which resulted in an altered source-sink allocation and carbohydrate storage. With lower leaf area, less carbohydrates are allocated. This for example resulted in a decreased trunk diameter. Further, it affected the composition of the grapevine wood microbiota. SSP and MDC management changed significantly the prokaryotic community composition in wood of the root samples, but had no effect in other compartments. In general, this study found strong compartment and less management effects of the microbial community composition and associated physicochemical properties. The highest microbial diversities were identified in the wood of the trunk, and several species were recorded the first time in grapevine.

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.