Terroir 1996 banner
IVES 9 IVES Conference Series 9 Effect of terroir on the quality evolution of Cabernet-Sauvignon in Penedès A.0.C.

Effect of terroir on the quality evolution of Cabernet-Sauvignon in Penedès A.0.C.

Abstract

Le Cabernet-Sauvignon est un cépage très répandu dans la région du Penedès (Espagne) où cette variété peut bien s’adapter et donne des produits de haute qualité. La croissance végétative et la composition du fruit dépendront de la mosaïque de sols disponibles dans l’Appellation. Dans ce sens, la cartographie du sol est un des meilleurs outils pour déterminer le potentiel viticole d’une région: son utilisation permet d’évaluer les différents terroirs présents dans une région. Le but de ce travail est d’évaluer l’évolution de la qualité dès le début de la saison de croissance jusqu’au vin final, en comparant des vignes de Cabernet-Sauvignon situées sur différents types de sols. L’étude a été réalisée pendant la période 2000-2001, sur deux parcelles de Cabernet Sauvignon greffé sur 41 B et SO4, âgées de 26 et 13 ans respectivement. Les souches sont palissées et taillées en Cordon de Royat. Chaque parcelle est composée par deux types de sol très différenciés: sol profond avec du schiste sur un sol caillouteux argilo-calcaire, et un sol profond limoneux sur un sol limoneux peu profond limité par une couche pétrocalcique.
La comparaison se fait au niveau de la composition minérale des feuilles, de la qualité du raisin à maturité et des vins finis. Ces unités de sol ont été déterminées en utilisant une cartographie du sol très détaillée basée sur la méthodologie de la FAO.
Les résultats indiquent que le Cabernet-Sauvignon sur le sol profond avec du schiste montre une meilleure nutrition minérale sur les parties végétatives que celles du Cabernet-Sauvignon sur sols calcaires ou limoneux. Ce type de sol a une grande porosité et profondeur, ce qui permet une bonne croissance et distribution des racines et également un bon état sanitaire dans la zone des racines. L’évolution de la composition de raisin depuis la véraison jusqu’à la maturité suggère que les sols profonds du schiste et les sols peu profonds limoneux ont une corrélation avec la vigueur, le rendement, le poids de la baie et la couleur. La dynamique spécifique de l’eau dans le sol, la variation de la réserve hydrique utile à chaque stade phénologique peut déterminer l’amélioration de la qualité sur ces sols. D’autre part, les vins obtenus sur chaque terroir, après microvinifications, présentent des différences importantes dans l’arôme et la structure. Cela montre que la connaissance de la distribution du terroir dans de grandes régions d’Appellation d’Origine est essentielle pour optimiser les plantations en ce qui concerne la qualité.

Cabernet-Sauvignon has become a very common grapevine in the Penedès region (Spain) where this variety can be well adapted and produce high quality products. The vegetative growth and fruit composition will depend on the wide range of soils of the A.O.C. area. In this sense, soil cartography is one of the best tools to determine the viticulture potential of a region using soil mapping that quantify different terroirs presents in the area. The aim of this work is to evaluate the whole evolution quality, from beginning of growing season to final wine, comparing Cabernet-Sauvignon vineyards located in different types of soils. The study was conducted in 2000-2001 period in two Cabernet-Sauvignon vineyards grafted on 41B and SO4. Vines are 26 and 13 years old respectively and its trelling system was “cordon Royat”. Each vineyard was composed by two vastly different types of soil which effect was compared: slate-schist deep stony soil vs. lime stone clay soil and silt deep deposit vs. a shallow silt soil limited with a petrocalcic layer. Comparison refers to minera] composition of vegetative parts, grape quality in maturity and quality of wine resulting. These soil units have been determinate using very detailed soil cartography based on FAO methodology.
Results indicate that Cabernet-Sauvignon on slate-schist deep stony soil shows a better level of mineral nutrients on vegetative parts compared to calcareous or silties soils. This type of soil has large porous space and depth, allows a large root growth and distribution and also the maintenance of a good sanitary condition in the root zone. The evolution of grape composition from the veraison to harvest suggest that slate-schist deep stony soil and shallow silt soil have a correlation with vigour, yield, berry weight and colour degree. Specific dynamics of soil water, varying holding capacity and available water in each phenologic stage can determinate the increase in quality in these soils. Otherwise, wines obtained of each terroir, using microvinifications, show inportant differences in aroma and structure. That indicates that the knowledge of distribution of terroir in large A.O.C. areas is essential to optimise plantations in terms of quality.

DOI:

Publication date: February 15, 2022

Issue: Terroir 2002

Type: Article

Authors

X. SORT and A.ZAYAS

Viticulture Department. Miguel Torres S.A. C/ Comerç 22. 08720 Vilafranca del Penedès. Spain

Keywords

Cabernet sauvignon, qualité de ta vendange, A.O.C. Penedès, Cartographie du sol, terroir
cabernet sauvignon, harvest quality, Penedès A.O.C., soil cartography, terroir

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Frost risk projections in a changing climate are highly sensitive in time and space to frost modelling approaches

Late spring frost is a major challenge for various winegrowing regions across the world, its occurrence often leading to important yield losses and/or plant failure. Despite a significant increase in minimum temperatures worldwide, the spatial and temporal evolution of spring frost risk under a warmer climate remains largely uncertain. Recent projections of spring frost risk for viticulture in Europe throughout the 21st century show that its evolution strongly depends on the model approach used to simulate budburst. Furthermore, the frost damage modelling methods used in these projections are usually not assessed through comparison to field observations and/or frost damage reports.
The present study aims at comparing frost risk projections simulated using six spring frost models based on two approaches: a) models considering a fixed damage threshold after the predicted budburst date (e.g BRIN, Smoothed-Utah, Growing Degree Days, Fenovitis) and b) models considering a dynamic frost sensitivity threshold based on the predicted grapevine winter/spring dehardening process (e.g. Ferguson model). The capability of each model to simulate an actual frost event for the Vitis vinifera cv. Chadonnay B was previously assessed by comparing simulated cold thermal stress to reports of events with frost damage in Chablis, the northernmost winegrowing region of Burgundy. Models exhibited scores of κ > 0.65 when reproducing the frost/non-frost damage years and an accuracy ranging from 0.82 to 0.90.
Spring frost risk projections throughout the 21st century were performed for all winegrowing subregions of Bourgogne-Franche-Comté under two CMIP5 concentration pathways (4.5 and 8.5) using statistically downscaled 8×8 km daily air temperature and humidity of 13 climate models. Contrasting results with region-specific spring frost risk trends were observed. Three out of five models show a decrease in the frequency of frost years across the whole study area while the other two show an increase that is more or less pronounced depending on winegrowing subregion. Our findings indicate that the lack of accuracy in grapevine budburst and dehardening models makes climate projections of spring frost risk highly uncertain for grapevine cultivation regions.

Grape must quality and mesoclimatic variability in Fruška Gora wine-growing region, Serbia

The Fruška Gora mountain is a traditional wine-growing region in Serbia situated in the Pannonian Basin. Due to such a position, the vicinity of the Danube River and the presence of concave configuration, it is suitable for grape production. This paper provides analyses of spatial variations in meteorological parameters and grape juice quality within Fruška Gora wine region over three consecutive vintages (2018-2020). The examined period can be defined as warm with cool nights during September (AVG 18,9°C; GDD 1918°C; CI 12°CF) and with the presence of mesoclimatic variability. The East part of the study area was somewhat drier and hotter compared to other parts of the region. The analyses of grape must samples (190 in total) of five cultivars (Cabernet-Sauvignon, Merlot, Chardonnay, Sauvignon blanc and Grašac (Welschriesling)) commonly grown across the region (19 sites), were performed using Fourier Transform Infrared Technology (FTIR). Among all cultivars, Sauvignon blanc was harvested first in the East area (DOY=246±5, GDD at harvest=1552±74, 22.2±0.7 °Brix), while the latest harvest was recorded for Cabernet-Sauvignon in the West (DOY=283±5, GDD at harvest=1936±187, 23.4±1.0 °Brix ). Both the red and white cultivars had higher acidity and YAN in the grape must if the vines were grown in the North and East compared to South and West areas. According to PCA analysis, Grašac showed the lowest variation in grape must chemical composition. Thus, the results confirm that Grašac is the most stable cultivar in Fruška Gora. All monitored cultivars reached technological fruit ripeness by the end of the growing season. However, it was difficult to reach full ripeness of red cultivars, mostly beacuse of uncoupling of technolocical and phenolic ripeness. Thus, Cabernet-Sauvignon had higher variations in GDD sums at harvest compared to other cultivars, which probably increased variations in grape must quality.

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.

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.

Short-term relationships between climate and grapevine trunk diseases in southern French vineyards

[lwp_divi_breadcrumbs home_text="IVES" use_before_icon="on" before_icon="||divi||400" module_id="publication-ariane" _builder_version="4.19.4" _module_preset="default" module_text_align="center" module_font_size="16px" text_orientation="center"...