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…

Assessing the climate change vulnerability of European winegrowing regions by combining exposure, sensitivity and adaptive capacity indicators

Winegrowing regions recognized as protected designations of origin (PDOs) are closely tied to well defined geographic locations with a specific set of pedoclimatic attributes and strictly regulated by legal specifications. However, climate change is increasingly threatening these regions by changing local conditions and altering winegrowing processes. The vulnerability to these changes is largely heterogenous across different winegrowing regions because it is determined by individual characteristics of each region, including the capacity to adapt to new climatic conditions and the sensitivity to climate change, which depend not only on natural, but also socioeconomic and legal factors. Accurate vulnerability assessments therefore need to combine information about adaptive capacity and climate change sensitivity with projected exposure to new climatic conditions. However, most existing studies focus on specific impacts neglecting important interactions between the different factors that determine climate change vulnerability. Here, we present the first comprehensive vulnerability assessment of European wine PDOs that spatially combines multiple indicators of adaptive capacity and climate change sensitivity with high-resolution climate projections. We found that the climate change vulnerability of PDO areas largely depends on the complex interactions between physical and socioeconomic factors. Homogenous topographic conditions and a narrow varietal spectrum increase climate change vulnerability, while the skills and education of farmers, together with a good economic situation, decrease their vulnerability. Assessments of climate change consequences therefore need to consider multiple variables as well as their interrelations to provide a comprehensive understanding of the expected impacts of climate change on European PDOs. Our results provide the first vulnerability assessment for European winegrowing regions at high spatiotemporal resolution that includes multiple factors related to climate exposure, sensitivity, and adaptive capacity on the level of single winegrowing regions. They will therefore help to identify hot spots of climate change vulnerability among European PDOs and efficiently direct adaptation strategies.

Spatiotemporal patterns of chemical attributes in Vitis vinifera L. cv. Cabernet Sauvignon vineyards in Central California

Spatial variability of vine productivity in winegrapes is important to characterise as both yield and quality are relevant for the production of different wine styles and products. The objectives were to understand how patterns of variability of Cabernet Sauvignon fruit composition changed over time and space, how these patterns could be characterised with indirect measurements, and how spatial patterns of the variation in fruit compositional attributes can aid in improving management. Prior to the 2017 vintage, 125 data vines were distributed across each of four vineyards in the Lodi American Viticultural Area (AVA) of California. Each data vine was sampled at commercial harvest in 2017, 2018, and 2019. Yield components and fruit composition were measured at harvest for each data vine, and maps of yield and fruit composition were produced for eight ‘objective measures of fruit quality’: total anthocyanins, polymeric tannins, quercetin glycosides, malic acid, yeast assimilable nitrogen, β-damascenone, C6 alcohols and aldehydes, and 3-isobutyl-2-methoxypyrazine. Patterns of variation in anthocyanins and phenolic compounds were found to be most stable over time. Given this relative stability, management decisions focused on fruit quality could be based on zonal descriptions of anthocyanins or phenolics to increase profitability in some vineyards. In each vineyard, dormant season pruning weights and soil cores were collected at each location, elevation and soil apparent electrical conductivity surveys were completed, and remotely sensed imagery was captured by fixed wing aircraft and two satellite platforms at major phenological stages. The data collected were used to develop relationships among biophysical data, soil, imagery, and fruit composition. The standardised and aggregated samples from four vineyards over three seasons were included in the estimation of ‘common variograms’ to assess how this technique could aid growers in producing geostatistically rigorous maps of fruit composition variability without cumbersome, single season sampling efforts.

Mapping and tracking canopy size with VitiCanopy

Understanding vineyard variability to target management strategies, apply inputs efficiently and deliver consistent grape quality to the winery is essential. However, despite inherent vineyard variability, the majority are managed as if they are uniform. VitiCanopy is a simple, grower-friendly tool for precision/digital viticulture that allows users to collect and interpret objective spatial information about vineyard performance. After four years of field and market research, an upgraded VitiCanopy has been created to achieve a more streamlined, technology-assisted vine monitoring tool that provides users with a set of superior new features, which could significantly improve the way users monitor their grapevines. These new features include:
• New user interface
• User authentication
• Batch analysis of multiple images
• Ease the learning curve through enhanced help features
• Reporting via the creation of colour maps that will allow users to assess the spatial differences in canopies within a vineyard.
Use-case examples are presented to demonstrate the quantification and mapping of vineyard variability through objective canopy measurements, ground-truthing of remotely sensed measurements, monitoring of crop conditions, implementation of disease and water management decisions as well as creating a history of each site to forecast quality. This intelligent tool allows users to manage grapevines and make informed management choices to achieve the desired production targets and remain profitable.

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.

Impact on leaf morphology of Vitis vinifera L. cvs Riesling and Cabernet Sauvignon under Free Air Carbon dioxide Enrichment (FACE)

Atmospheric carbon dioxide (CO2) concentration has continuously increased since pre-industrial times from 280 ppm in 1750, and is predicted to exceed 700 ppm by the end of 21st century. For most of C3 plant species elevated CO2 (eCO2) improve photosynthetic apparatus results in an increased plant biomass production. To investigate the effects of eCO2 on morphological leaf characteristics the two Vitis vinifera L. cultivars, Riesling and Cabernet Sauvignon, grown in the Geisenheim VineyardFACE (Free Air Carbon dioxide Enrichment) system were used. The FACE site is located at Geisenheim University (49° 59′ N, 7° 57′ E, 94 m above sea level), Germany and was implemented in 2014 comparing future atmospheric CO2-concentrations (eCO2, predicted for the mid-21st century) with current ambient CO2-conditions (aCO2). Experiments were conducted under rain-fed conditions for two consecutive years (2015 and 2016). Six leaves per repetition of the CO2 treatment were sampled in the field and immediately fixed in a FAA solution (ethanol, H2O, formaldehyde and glacial acetic acid). After 24 h leaf samples were transferred and stored in an ethanol solution. Subsequently, leaf tissue was dehydrated using ethanol series and embedded in paraffin. By using a rotary microtomesections of 5 µm were prepared and fixed on microscopic slides. Subsequent the samples were stained using consecutive staining and washing solutions. Afterwards pictures of the leaf cross-sections were taken using a light microscope and consecutive measurements were conducted with an open source image software. Differences found in leaf cross-sections of the two CO2 treatments were detected for the palisade parenchyma. Leaf thickness, upper and lower epidermis and spongy parenchyma remained less affected under eCO2 conditions. The observed results within grapevine leaf tissues can provide first insights to seasonal adaptation strategies of grapevines under future elevated CO2 concentrations.