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…

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.

VineyardFACE: Investigation of a moderate (+20%) increase of ambient CO2 level on berry ripening dynamics and fruit composition

Climate change and rising atmospheric carbon dioxide concentration is a concern for agriculture, including viticulture. Studies on elevated carbon dioxide have already been on grapevines, mainly taking place in greenhouses using potted plants or using field grown vines under higher CO2 enrichment, i.e. >650 ppm. The VineyardFACE, located at Hochschule Geisenheim University, is an open field Free Air CO2 Enrichment (FACE) experimental set-up designed to study the effects of elevated carbon dioxide using field grown vines (Vitis vinifera L. cvs. Riesling and Cabernet Sauvignon). As the carbon dioxide fumigation started in 2014, the long term effects of elevated carbon dioxide treatment can be investigated on berry ripening parameters and fruit metabolic composition.
The present study aims to investigate the effect on fruit composition under a moderate increase (+20%; eCO2) of carbon dioxide concentration, as predicted for 2050 on both Riesling and Cabernet Sauvignon. Berry composition was determined for primary (sugars, organic acids, amino acids) and secondary metabolites (anthocyanins). Special focus was given on monitoring of berry diameter and ripening rates throughout three growing seasons. Compared to previous results of the early adaptative phase of the vines [1], our results show little effect of eCO2 treatment on primary metabolites composition in berries. However, total anthocyanins concentration in berry skin was lower for eCO2 treatment in 2020, although the ratio between anthocyanins derivatives did not differ.
[1] Wohlfahrt Y., Tittmann S., Schmidt D., Rauhut D., Honermeier B., Stoll M. (2020) The effect of elevated CO2 on berry development and bunch structure of Vitis vinifera L. cvs. Riesling and Cabernet Sauvignon. Applied Science Basel 10: 2486

Adaptability of grapevines to climate change: characterization of phenology and sugar accumulation of 50 varieties, under hot climate conditions

Climate is the major factor influencing the dynamics of the vegetative cycle and can determine the timing of phenological periods. Knowledge of the phenology of varieties, their chronological duration, and thermal requirements, allows not only for the better management of interventions in the vineyard, but also to predict the varieties’ behaviour in a scenario of climate change, giving the wine producer the possibility of selecting the grape varieties that are best adapted to the climatic conditions of a certain terroir. In 2014, Symington Family Estates, Vinhos, established two grape variety libraries in two different places with distinctive climate conditions (Douro Superior, and Cima Corgo), with the commitment of contributing to a deeper agronomic and oenological understanding of some grape varieties, in hot climate conditions. In these research vineyards are represented local varieties that are important in the regional and national viticulture, but also others that have over time been forgotten — as well as five international reference cultivars. From 2017 to 2021, phenological observations have been made three times a week, following a defined protocol, to determine the average dates of budbreak, flowering and veraison. With the climate data of each location, the thermal requirements of each variety and the chronological duration of each phase have been calculated. During maturation, berry samples have been gathered weekly to study the dynamics of sugar accumulation, between other parameters. The data was analysed applying phenological and sugar accumulation models available in literature. The results obtained show significant differences between the varieties over several parameters, from the chronological duration and thermal requirements to complete the various stages of development, to the differences between the two locations, confirming the influence of the climate on phenology and the stages of maturation, in these specific conditions.

Bioclimatic shifts and land use options for Viticulture in Portugal

Land use, plays a relevant role in the climatic system. It endows means for agriculture practices thus contributing to the food supply. Since climate and land are closely intertwined through multiple interface processes, climate change may lead to significant impacts in land use. In this study, 1-km observational gridded datasets are used to assess changes in the Köppen–Geiger and Worldwide Bioclimatic (WBCS)

A blueprint for managing vine physiological balance at different spatial and temporal scales in Champagne

In Champagne, the vine adaptation to different climatic and technical changes during these last 20 years can be seen through physiological balance disruptions. These disruptions emphasize the general grapevine decline. Since the 2000s, among other nitrogen stress indicators, the must nitrogen has been decreasing. The combination of restricted mineral fertilizers and herbicide use, the growing variability of spring rainfall, the increasing thermal stress as well as the soil type heterogeneity are only a few underlying factors that trigger loss of physiological balance in the vineyards. It is important to weigh and quantify the impact of these factors on the vine. In order to do so, the Comité Champagne uses two key-tools: networking and modelization. The use of quantitative and harmonized ecophysiological indicators is necessary, especially in large spatial scales such as the Champagne appellation. A working group with different professional structures of Champagne has been launched by the Comité Champagne in order to create a common ecophysiology protocol and thus monitor the vine physiology, yearly, around 100 plots, with various cultural practices and types of soil. The use of crop modelling to follow the vine physiological balance within different pedoclimatic conditions enables to understand the present balance but also predict the possible disruptions to come in future climatic scenarios. The physiological references created each year through the working group, benefit the calibration of the STICS model used in Champagne. In return, the model delivers ecophysiology indicators, on a daily scale and can be used on very different types of soils. This study will present the bottom-up method used to give accurate information on the impacts of soil, climate and cultural practices on vine physiology.