Terroir 2004 banner
IVES 9 IVES Conference Series 9 Contribution of soil and atmospheric conditions to leaf water potential in grapevines

Contribution of soil and atmospheric conditions to leaf water potential in grapevines

Abstract

[English version below]

Etant lié au sol et aux conditions atmosphériques, le statut hydrique influence la physiologie de la vigne d’une part, mais joue aussi un role important en ce qui concerne la qualité du raisin et donc du vin d’autre part. Nous avons mesuré, dans la région de Stellenbosch, le statut hydrique sur des pieds de Sauvignon Blanc non irrigués, implantés sur 2 terroirs différents, l’un froid, l’autre plus chaud. D’après ces mesures, il semble que le potentiel hydrique foliaire (Ψl ) soit lié par une fonction logarithmique au potentiel hydrique du sol (Ψm). De plus, l’augmentation du stress hydrique du cep semble être plus lente lorsque Ψm descend en dessous de -0.3 MPa. Sous certaines conditions, le déficit en pression de vapeur ne semble pas influencer le Ψl (mesuré à l’aube), cependant lorsque les valeurs obtenues pour ce dernier sont combinées avec celles obtenues pour Ψm, alors 85% de la variabilité de Ψl mesuré à 14:00 peut être expliqué. A partir de ces résultats, nous pouvons donc conclure sur l’existence d’une fonction entre le statut hydrique de la vigne et les conditions atmosphériques ainsi qu’entre le statut hydrique et la teneur en eau du sol. Les résultats non linéaires du potentiel foliaire, caractérisés par des augmentations momentanées obtenus à différents moments de la journée peuvent être expliqués par une fermeture partielle des stomates. Les valeurs du flux de sève, observées pour des vignes cultivées sur les sols secs (Ψm = -0.75 MPa) du terroir plus froid, montrent de fortes diminutions pendant la journée, comparé à celles obtenues sur le terroir plus chaud où Ψm = -0.12 MPa. Ceci confirme bien que le statut hydrique de la vigne, situé sur le terroir plus froid, est régulé grâce à la fermeture partielle des stomates et ce, malgré le faible déficit en pression de vapeur enregistré sur cette même localité.
La linéarité de la relation entre Ψl et Ψm, sur vignes irriguées où Ψm était supérieur à -0.08 MPa, peut expliquer l’absence de contrôle stomatique significatif. Cependant, en mesurant Ψl toutes les 15 minutes, on peut observer la fermeture stomatique sur des vignes irriguées en climat semi-aride, où le déficit en pression de vapeur passe de 1.0 kPa à l’aube à 4.6 kPa dans l’après-midi, malgré une teneur en eau dans le sol proche de la capacité au champ (Ψm = ca -0.01 MPa). Le contrôle stomatique, une fois encore est à l’origine de la non- linéarité de la relation entre le déficit en pression de vapeur et Ψl. Ce dernier était, dans ces mêmes conditions, de –1.6 MPa. Ces résultats nous indiquent que là où la teneur en eau du sol n’est pas un facteur limitant, de difficiles conditions climatiques peuvent provoquer la fermeture des stomates, réduisant ainsi une chute trop sévère du potentiel hydrique foliaire. Le potentiel hydrique du sol, ainsi que le déficit en pression de vapeur, devraient donc permettre, par la suite, de quantifier l’effet du terroir sur le stress hydrique de la vigne.

Since grapevine water status, which is a function of soil and atmospheric conditions, affects grapevine physiology it will also play an important role in grape and wine quality. Water status in dry-land Sauvignon blanc was measured simultaneously both at a warm and a cool locality in the Stellenbosch region at different phenological stages during the growing season. Leaf water potential (Ψl) appeared to be a logarithmic function of soil matric potential (Ψm). Grapevine water stress tended to increase at a slower rate when Ψm dropped below ca -0.3 MPa. Under the given conditions, vapour pressure deficit (VPD) did not seem to have an effect on pre-dawn Ψl, but in combination with Ψm could explain 85% of the variation in Ψl measured at 14:00. These results indicated that grapevine water status was a function of atmospheric conditions as well as soil water content. The non-linear response of Ψl appeared to be the result of partial stomatal closure that increased Ψl at certain stages during the day. Sap flow rates in grapevines cultivated on the drier soil (i.e. Ψm = -0.75 MPa) showed pronounced reductions during the day at the cooler locality compared to those at the warmer one where Ψm was ca -0.12 MPa. This confirmed that grapevine water status was regulated via partial stomatal closure at the cooler locality, despite the lower VPD that was recorded at this particular locality.
In studies with irrigated grapevines, where Ψm was higher than -0.08 MPa, absence of significant stomatal control was probably the reason for the reported linear response between Ψl and Ψm. However, measuring Ψl at 15 minute intervals revealed that stomatal closure occurred in irrigated grapevines under semi-arid conditions where VPD increased from 1.0 kPa pre-dawn to 4.6 kPa in the afternoon despite soil water content being near field capacity (i.e. Ψm = ca -0.01 MPa). Due to stomatal control, the relationship between Ψl and VPD was also non-linear. Under these specific conditions, minimum Ψl was ca -1.6 MPa. These results showed that even where soil water content was not a limiting factor, harsh meteorological conditions were able to cause partial stomatal closure, thus preventing the evolution of extremely low Ψl values in grapevines. From the foregoing, it is suggested that Ψm as well as VPD should be considered for the quantification of terroir effects on grapevine water stress.

DOI:

Publication date: January 12, 2022

Issue: Terroir 2004

Type: Article

Authors

P.A. Myburgh and M. Laker

ARC Infruitec-Nietvoorbij, Private Bag X5026, 7599 Stellenbosch, Republic of South Africa

Contact the author

Keywords

Grapevine, leaf water potential, soil water, vapour pressure deficit, locality

Tags

IVES Conference Series | Terroir 2004

Citation

Related articles…

Soil, vine, climate change – what is observed – what is expected

To evaluate the current and future impact of climate change on Viticulture requires an integrated view on a complex interacting system within the soil-plant-atmospheric continuum under continuous change. Aside of the globally observed increase in temperature in basically all viticulture regions for at least four decades, we observe several clear trends at the regional level in the ratio of precipitation to potential evapotranspiration. Additionally the recently published 6th assessment report of the IPCC (The physical science basis) shows case-dependent further expected shifts in climate patterns which will have substantial impacts on the way we will conduct viticulture in the decades to come.
Looking beyond climate developments, we observe rising temperatures in the upper soil layers which will have an impact on the distribution of microbial populations, the decay rate of organic matter or the storage capacity for carbon, thus affecting the emission of greenhouse gases (GHGs) and the viscosity of water in the soil-plant pathway, altering the transport of water. If the upper soil layers dry out faster due to less rainfall and/or increased evapotranspiration driven by higher temperatures, the spectral reflection properties of bare soil change and the transport of latent heat into the fruiting zone is increased putting a higher temperature load on the fruit. Interactions between micro-organisms in the rhizosphere and the grapevine root system are poorly understood but respond to environmental factors (such as increased soil temperatures) and the plant material (rootstock for instance), respectively the cultivation system (for example bio-organic versus conventional). This adds to an extremely complex system to manage in terms of increased resilience, adaptation to and even mitigation of climate change. Nevertheless, taken as a whole, effects on the individual expressions of wines with a given origin, seem highly likely to become more apparent.

Combining effect of leaf removal and natural shading on grape ripening under two irrigation strategies in Manto negro (Vitis vinifera L.)

The increasingly frequent heat waves during grape ripening pose challenges for high quality wine grape production. Defoliation is a common practice that can improve the control of diseases in bunches, but also it increases the exposure to sunlight. Grapes exposed to solar radiation reach temperatures over the optimum for berry development and maturation. This makes the development of irrigation and canopy management techniques of great importance to maximize yield and grape quality. A field experiment was carried out during 2021 using Manto negro wine grapes to study the effect of applied irrigation and different light exposure levels on grape quality. Two irrigation treatments were imposed based on the frequency and amount of water doses in a four-block experimental vineyard at Bodega Ribas (Mallorca). Three light exposure treatments were randomly applied in each irrigation plot. The light treatments included exposed clusters from pea size, non-exposed clusters, and shaded clusters after softening. Leaf area index and canopy porosity was estimated every 2 weeks. Midday leaf water potential was measured weekly. Additionally, apparent electrical conductivity was measured between rows to estimate the soil water content variability. Light and temperature sensors were installed at the bunch level to quantify the differences in bunch temperature and light intensity among treatments. The effect of irrigation and cluster light exposure on berry weight, TSS, TA, malic acid, tartaric acid, K+, and pH were analysed at 5 moments along grape ripening. During different heat waves, the natural shading technique decreased the maximum bunch temperature around 10 °C respect to the exposed bunches in both irrigation strategies. The combination of defoliation and shading techniques after softening decreased TSS at harvest and affected most of the quality parameters during the last stages of ripening, showing an interesting technique to delay ripening in warm viticulture areas.

Variations of soil attributes in vineyards influence their reflectance spectra

Knowledge on the reflectance spectrum of soil is potentially useful since it carries information on soil chemical composition that can be used to the planning of agricultural practices. If compared with analytical methods such as conventional chemical analysis, reflectance measurement provides non-destructive, economic, near real-time data. This paper reports results from reflectance measurements performed by spectroradiometry on soils from two vineyards in south Brazil. The vineyards are close to each other, are on different geological formations, but were subjected to the same management. The objective was to detect spectral differences between the two areas, correlating these differences to variations in their chemical composition, to assess the technique’s potential to predict soil attributes from reflectance data.To that end, soil samples were collected from ten selected vine parcels. Chemical analysis yield data on concentration of twenty-one soil attributes, and spectroradiometry was performed on samples. Chemical differences significant to a 95% confidence level between the two studied areas were found for six soil attributes, and the average reflectance spectra were separated by this same level along most of the observed spectral domain. Correlations between soil reflectance and concentrations of soil attributes were looked for, and for ten soil traits it was possible to define wavelength domains were reflectance and concentrations are correlated to confidence levels from 95% to 99%. Partial Least Squares Regression (PLSR) analyses were performed comparing measured and predicted concentrations, and for fifteen out of 21 soil traits we found Pearson correlation coefficients r > 0.8. These preliminary results, which have to be validated, suggest that variations of concentration in the investigated soil attributes induce differences in reflectance that can be detected by spectroradiometry. Applications of these observations include the assessment of the chemical content of soils by spectroradiometry as a fast, low-cost alternative to chemical analytical methods.

Modeling island and coastal vineyards potential in the context of climate change

Climate change impacts regional and local climates, which in turn affects the world’s wine regions. In the short term, these modifications rises issues about maintaining quality and style of wine, and in a longer term about the suitability of grape varieties and the sustainability of traditional wine regions. Thus, adaptation to climate change represents a major challenge for viticulture. In this context, island and coastal vineyards could become coveted areas due to their specific climatic conditions. In regions subject to warming, the proximity of the sea can moderate extremes temperatures, which could be an advantage for wine. However, coastal and island areas are particular prized spaces and subject to multiple pressures that make the establishment or extension of viticulture complex.
In this perspective, it seems relevant to assess the potentialities of coastal and island areas for viticulture. This contribution will present a spatial optimization model that tends to characterize most suitable agroclimatic patterns in historical or emerging vineyards according to different scenarios. Thanks to an in-depth bibliography a global inventory of coastal and insular vineyards on a worldwide scale has been realized. Relevant criteria have been identified to describe the specificities of these vineyards. They are used as input data in the optimization process, which will optimize some objectives and spatial aspects. According to a predefined scenario, the objectives are set in three main categories associated with climatic characteristics, vineyards characteristics and management strategies. At the end of this optimization process, a series of maps presents the different spatial configurations that maximize the scenario objectives.

Drought effect on aromatic and phenolic potential of seven recovered grapevine varieties in Castilla-La Mancha region (Spain)

The effects of climate change are seriously affecting the quality of wine grapes. High temperatures and drought cause imbalances in the chemical composition of grapes. The result is overripe grapes with low acidity and high sugar content, which produce wines with excessive alcohol content, lacking in freshness and not very aromatic. As a consequence, the search of varieties with capacity of produce quality grapes in adverse climate conditions is a good alternative to preserve the sustainability of vineyards. In this work, quality parameters of seven Vitis vinifera L. cultivars (five whites and two reds) recently recovered from extinction and grown under two different hydric regimes (rainfed and irrigated) were analyzed during the 2020 vintage. At harvest time, weight of 100 berries, must physicochemical parameters (brix degree, total acidity, malic acid, pH), and carbon and oxygen isotope ratios (δ13C, δ18O) were determined. Subsequently, varietal aroma potential index (IPAv) and total polyphenol index (TPI) were analyzed. Quality parameters, IPAv and TPI, showed significant differences between varieties and water regimes. Both red varieties, Moribel and Tinto Fragoso, stood out for their high aromatic and phenolic potential, which was higher under rainfed regime. Regarding to white varieties, Montonera del Casar and Jarrosuelto stood out in terms of varietal aroma potential. Montonera del Casar high acidity in its musts and Jarrosuelto showed the highest berry weights.