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…

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…

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.

The rootstock, the neglected player in the scion transpiration even during the night

Water is the main limiting factor for yield in viticulture. Improving drought adaptation in viticulture will be an increasingly important issue under climate change. Genetic variability of water deficit responses in grapevine partly results from the rootstocks, making them an attractive and relevant mean to achieve adaptation without changing the scion genotype. The objective of this work was to characterize the rootstock effect on the diurnal regulation of scion transpiration. A large panel of 55 commercial genotypes were grafted onto Cabernet Sauvignon. Three biological repetitions per genotype were analyzed. Potted plants were phenotyped on a greenhouse balance platform capable of assessing real-time water use and maintaining a targeted water deficit intensity. After a 10 days well-watered baseline period, an increasing water deficit was applied for 10 days, followed by a stable water deficit stress for 7 days. Pruning weight, root and aerial dry weight and transpiration were recorded and the experiment was repeated during two years. Transpiration efficiency (ratio between aerial biomass and transpiration) was calculated and δ13C was measured in leaves for the baseline and stable water deficit periods. A large genetic variability was observed within the panel. The rootstock had a significant impact on nocturnal transpiration which was also strongly and positively correlated with maximum daytime transpiration. The correlations with growth and water use efficiency related traits will be discussed. Transpiration data were also related with VPD and soil water content demonstrating the influence of environmental conditions on transpiration. These results highlighted the role of the rootstock in modulating water deficit responses and give insights for rootstock breeding programs aimed at identifying drought tolerant rootstocks. It was also helpful to better define the mechanisms on which the drought tolerance in grapevine rootstocks is based on.

Spatial variability of temperature is linked to grape composition variability in the Saint-Emilion winegrowing area

Elevated temperature during the grape maturation period is a major threat for grape quality and thus wine quality. Therefore, characterizing the grape composition response to temperature at a larger scale would represent a crucial step towards adaptation to climate change. In response to changes in temperature, various physiological mechanisms regulate grape composition. Primary and secondary metabolisms are both involved in this response, with well-known effects, for example on anthocyanins, and lesser known effects, for example on aromas or aroma precursors. At the field scale or at the regional scale, however, numerous environmental or plant-specific factors intervene to make the effects of temperature difficult to distinguish from overall variability. In this study, it was attempted to overcome this difficulty by selecting well-characterized situations with differing temperatures.
A long-term study of air temperature variability across several Merlot vineyards in the Saint-Emilion and Pomerol wine producing area found significant temperature differences and gradients at various time scales linked to environmental factors. From this study area, a few sites were selected with similar age, soil and training system conditions, and with repeated and contrasted temperature differences during the maturation period. The average temperature difference during the maturation period was about 2°C between cooler and warmer sites, a difference similar to that expected under future climate change scenarios. In close vicinity to the temperature sensors at each site, grape berries were sampled at different times until full maturity during 2019 and 2020. Also, berries from bunches on either side of the row were analyzed separately, allowing an investigation of bunch exposure effect associated with the coupling of berry temperature and solar radiation. Four replicates of pooled berries for each time – site – bunch exposure combination were obtained and analyzed for biochemical composition. Analyses of variance of the biochemical composition data collected at different sampling times reveal significant effects associated with temperature, site, and bunch azimuth. For instance, anthocyanins in grape skins are clearly influenced by temperature and solar radiation exposure, with up to 30% reduction in warmer conditions.

Use of multispectral satellite for monitoring vine water status in mediterranean areas

The development of new generations of multispectral satellites such as Sentinel-2 opens possibilities as to vine water status assessment (Cohen et al., 2019). Based on a three years field campaign, a model of Stem Water Potential (SWP) estimation on vine using four satellite bands in Red, Red-Edge, NIR and SWIR domains was developed (Laroche-Pinel et al., 2021). The model relies on SWP field measures done using a pressure chamber (Scholander et al., 1965), which is a common, robust and precise method to assess vine water status (Acevedo-Opazo et al., 2008). The model was mainly developed from from SWP measures on Syrah N (Laroche Pinel E., 2021).

A large scale monitoring was organized in different vineyards in the Mediterranean region in 2021. 10 varieties amongst the most represented in this area were monitored (Cabernet sauvignon N, Chardonnay B, Cinsault N, Grenache N, Merlot N, Mourvèdre N, Sauvignon B, Syrah N, Vermentino B, Viognier B). The model was used to produce water status maps from Sentinel-2 images, starting from the beginning of June (fruit set) up to September (harvest). The average estimated SWP for each vine was compared to actual field SWP measures done by wine growers or technicians during usual monitoring of irrigation programs. The correlations between mean estimated SWP and mean measured SWP were at the same level than expected by the model. (Laroche Pinel, 2021) The general SWP kinetics were comparable. The estimated SWP would have led to same irrigation decisions concerning the date of first irrigation in comparison with measured SWP.

Acevedo-Opazo, C., Tisseyre, B., Ojeda, H., Ortega-Farias, S., Guillaume, S. (2008). Is it possible to assess the spatial variability of vine water status? OENO One, 42(4), 203.
Cohen, Y., Gogumalla, P., Bahat, I., Netzer, Y., Ben-Gal, A., Lenski, I., … Helman, D. (2019). Can time series of multispectral satellite images be used to estimate stem water potential in vineyards? In Precision agriculture ’19, The Netherlands: Wageningen Academic Publishers, pp. 445–451.
Laroche-Pinel, E., Duthoit, S., Albughdadi, M., Costard, A. D., Rousseau, J., Chéret, V., & Clenet, H. (2021). Towards vine water status monitoring on a large scale using sentinel-2 images. remote sensing, 13(9), 1837.
Laroche-Pinel,E. (2021). Suivi du statut hydrique de la vigne par télédétection hyper et multispectrale. Thèse INP Toulouse, France.
Scholander, P.F., Bradstreet, E.D., Hemmingsen, E.A., & Hammel, H.T. (1965). Sap pressure in vascular plants: Negative hydrostatic pressure can be measured in plants. Science, 148(3668), 339–346.