Terroir 1996 banner
IVES 9 IVES Conference Series 9 Evapotranspiración de viñedo en secano y evaporación de barbecho en “La Mancha”

Evapotranspiración de viñedo en secano y evaporación de barbecho en “La Mancha”

Abstract

Un 94 % del viñedo español se cultiva con métodos y técnicas propias de los sistemas agrícolas desarrollados en secano en regiones de clima semiárido, donde las precipitaciones anuales raramente exceden los 500 mm: reducida densidad de plantación, conducción en vaso, recolección manual, escaso uso de mano de obra cualificada, limitadas aportaciones de nutrientes, elevado número de labores para el manejo del suelo, y tratamientos fitosanitarios sólo en situaciones muy justificadas.
Castilla-La Mancha, con 593000 ha de viñedo, es la región que tiene la mayor superficie dedicada del mundo, representando el 8 % de la superficie vitícola mundial, el 11,4 % de la de Europa y el 50 % del viñedo nacional. Además de la manifiesta importancia socioeconómica, el viñedo castellano-manchego juega un papel ecológico de sumo interés dentro del concepto y fundamentos de la agricultura sostenible. Esta biomasa transpirante contribuye a mantener un ecosistema agrícola importante generado en condiciones limitantes, con un papel acusado en ralentizar el proceso de desertificación (de Juan et al., 1998).
Doorenbos y Kassam (1986) consideran que las necesidades estacionales de agua de la vid varían entre 660 y 1200 mm, dependiendo fundamentalmente del clima y de la duración de la estación de crecimiento y desarrollo. Williams y Matthews (1990) refieren consumos estacionales máximos que oscilan entre 660 y 800 mm, en zonas donde la ETo varió entre 1128 y 1231 mm. Alexandrescu et al. (1966) obtienen tasas máximas de evapotranspiración de 5,9 mmdía-1, mientras los valores dados por Hicks (1973) oscilaron entre 2 mmdía-1 (prefloración) hasta 4 mmdía-1 (postenvero).
El conocimiento de las relaciones hídricas de la vid no sólo es necesario para paliar el déficit hídrico a través de la programación del riego, sino también para un adecuado manejo del viñedo cultivado en secano. Sin embargo, bajo estos últimos sistemas de producción agrícola los estudios relacionados con el consumo de agua son mucho menos numerosos, al menos, en España. El largo periodo de extrema sequía padecido a principios de los años 90 en Castilla-La Mancha impulsó un elevado número de estudios multidisciplinares desarrollados dentro del Proyecto EFEDA (“ECHIVAL Field Experiment in a Desertification-threatened Area”) (Bolle et al., 1993), integrado en “The European Programme on Climate and Natural Hazards (EPOCH)”, y financiado por “The Commission of the European Communities (CEC)”. Por medio del Proyecto EFEDA, se ha podido conocer, mediante la utilización de métodos micrometeorológicos, que la evapotranspiración del viñedo durante los meses de junio y julio en regiones semiáridas puede llegar a ser de 1 mmdía-1 (6 lcepa-1), en un porcentaje superior al 95 % debido al proceso de transpiración de las plantas (Oliver y Sene, 1992; Sene, 1994). Estos investigadores estimaron un consumo estacional de la vid cultivada en secano de 150 mm.
El trabajo que se presenta aquí se desarrolló dentro del Programa EFEDA, y tuvo como objetivo el llegar a conocer la alimentación hídrica de la vid y poder cuantificar la contribución del perfil del suelo al proceso de evapotranspiración, en regiones que, como Castilla-La Mancha, se caracterizan por la existencia de déficits hídricos muy acusados en los meses de junio, julio y agosto, debido principalmente a que las precipitaciones son escasas o irregulares, de 300 a 400 mm anuales, con veranos largos, secos, muy calurosos y, en consecuencia, de alta demanda evaporativa por parte de la atmósfera.

DOI:

Publication date: February 25, 2022

Issue: Terroir 2000

Type: Article

Authors

Montero F.J., de Juan J.A., Sajardo E., Cuesta A. and Martínez E.

Tags

IVES Conference Series | Terroir 2000

Citation

Related articles…

Better understand the soil wet bulb formation with subsurface or aerial drip irrigation in viticulture

The gradual change in rainfall patterns experienced in the south of France vineyards, especially around the Mediterranean sea, means that the vines are increasingly subject to summer drought. The winegrowers developped the use of irrigation techniques to ensure the maintenance of competitive yields in the production of wines under Protected Geographical Indication label. In practice, drip irrigation pipes can be installed above the ground or buried into the soil as well as at different distances from the vine row. The objective of this study was to examine the profiles of the wet bulbs of the soil obtained from two drip irrigation systems : aerial drip located under the vine row and subsurface drip placed in the middle of the inter-row. This experiment took place over two consecutive seasons (2020-2021) on a 3.4 ha Viognier plot in the Mediterranean region (PGI Oc, France) on sandy clay soil. The annual rainfalls were less than 400 mm. Soil water content probes were installed at different depths (20 – 40 – 60 – 80 cm) and at different lateralities from the vine row (30 – 60 – 90 – 120 cm) to control the formation of the soil wet bulb during irrigation. The mapping and the analysis of the data allowed a better understanding and differentiation of the water percolation when irrigating with subsurface or aerial drip. For the same amount of water and without differences of vine water status, it is shown that in a subsurface drip irrigation situation, the size of the wet bulb formed is larger than in aerial drip irrigation system.

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.

Modulation of berry composition by different vineyard management practices

High concentration of sugars in grapes and alcohol in wines is one of the consequences of climate change on viticulture production in several wine-growing regions. In order to investigate the possibilities of adaptation of vineyard management practices aimed to reduce the accumulation of sugar during the maturation phase without reducing the accumulation of anthocyanins in grapes, a study with severe shoot trimming, shoot thinning, cluster thinning and date of harvest was conducted on Merlot variety in Istria region (Croatia), under the Mediterranean climate. Four factors which may affect grape maturation and its composition at harvest were investigated in a two-years experiment; severe shoot trimming applied at veraison when >80% of berries changed colour (in comparison to untreated control), shoot thinning (0 and 30%), cluster thinning (0 and 30%), and the date of harvest (early and standard harvest dates). Shoot thinning had no significant impact on berry composition, despite the obtained reduction in yield per vine. Lower Brix in grapes were obtained with earlier harvest date and if no cluster thinning was applied, although at the same time a reduction in the concentration of anthocyanins in berries was observed in these treatments. On the other hand, if severe shoot trimming was applied when >80% of berries changed colour, a reduction of Brix was obtained without a negative impact on berry anthocyanins concentration. We conclude that in cases when undesirably high sugar concentrations at harvest are expected, severe shoot trimming at 80% veraison may effectively be used in order to obtain moderate sugar concentration in berries together with the adequate phenolic composition.

Metabolomic discrimination of grapevine water status for Chardonnay and Pinot noir

Water status impact in viticulture has been widely explored, as it strongly affects grapevine physiology and grape chemical composition. It is considered as a key component of vitivinicultural terroir. Most of the studies concerning grapevine water status have focused on either physiological traits, or berry compounds, or traits involved in wine quality. Here, the response of grapevine to water availability during the ripening period is assessed through non-targeted metabolomics analysis of grape berries by ultra-high resolution mass spectrometry. The grapevine water status has been assessed during 2 consecutive years (2019 & 2020), through carbon isotope discrimination on juices from berries collected at maturity (21.5 brix approx.) for 2 Vitis vinifera cv. Pinot noir (PN) and Chardonnay (CH). A total of 220 grape juices were collected from 5 countries worldwide (Italy; Argentina; France; Germany; Portugal). Measured δ13C (‰) varied from -28.73 to -22.6 for PN, and from -28.79 to -21.67 for CH. These results also clearly revealed higher water stress for the 2020 vintage. The same grape juices have been analysed by Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FT-ICR-MS) and Liquid Chromatography coupled to Mass Spectrometry (LC-qTOF-MS), leading to the detection of up to 4500 CHONS containing elemental compositions, and thus likely tens of thousands of individual compounds, which include fatty acids, organic acids, peptides, phenolics, also with high levels of glycosylation. Multivariate statistical analysis revealed that up to 160 elemental compositions, covering the whole range of detected masses (100 –1000 m/z), were significantly correlated to the observed gradients of water status. Examples of chemical markers, which are representative of these complex fingerprints, include various derivatives of the known abscisic acid (ABA), such as phaesic acid or abscisic acid glucose ester, which are significantly correlated with higher water stress, regardless of the variety. Cultivar-specific behaviours could also be identified from these fingerprints. Our results provide an unprecedented representation of the metabolic diversity, which is involved in the water status regulation at the grape level, and which could contribute to a better knowledge of the grapevine mitigation strategy in a climate change context.

Modeling the suitability of Pinot Noir in Oregon’s Willamette Valley in a changing climate

Air temperature is the key driver of grapevine phenology and a significant environmental factor impacting yield and quality for a winegrape growing region. In this study the optimal downscaled CMIP5 ensemble for computing thegrowing season average temperature (GST) viticulture climate classification index was determined to spatially compute on a decadal basis predictions of the GST climate index and the grapevine sugar ripeness (GSR) model for Pinot Noir throughout the Willamette Valley (WV) American Viticultural Area (AVA). Forecasts for average temperature and a 220 g/L target sugar concentration level were computed using daily Localized Constructed Analogs (LOCA) downscaled CMIP5 historic and Representative Concentration Pathways (RCP) future climate projections of minimum and maximum daily temperature. We explore spatiotemporal trends of the GST climate classification index and Pinot Noir specific applications of the GSR phenology model for the WV AVA. Spatiotemporal computations of the GST climate index and Pinot Noir specific applications of the GSR model enable the opportunity to explore relationships between their computed values with one intent being to provide updated GST ranges that better align with current temperature-based modeling understanding of Pinot Noir grapevine phenology and the viticultural application of LOCA CMIP5 climate projections for the WV AVA. The Pinot Noir specific applications of the GSR model or the GST index with updated bounds indicate that the percent of the WV AVA area suitable for Pinot Noir production is currently at or near its peak value in the upper 80s to lower 90s of this century.