Measurement of grape vine growth for model evaluation

Abstract

Within a research project for simulating the nitrogen turnover in vineyard soils and the nitrogen uptake by the grape vine, a previously developed plant growth model (Nendel and Kersebaum 2004) had to be evaluated. A dataset was obtained from a monitoring experiment at three vineyard sites with different soil types, conducted in the years 2003 and 2004. The annual plant growth was measured by collecting non-perennial organs of 10 plants at 5 growth stages (pre-blossoming, setting, bunches closed, veraison, and ready for picking). The dry matter content of leaves, flower/grape clusters, shoots, side shoots, and tipping shoots was determined separately. Leaf area was measured before drying. At one vineyard site the plant fresh weight was additionally recorded. Simultaneously, soil water and Nmin content were analysed in soil samples taken from 0-30 and 30-60 cm soil depth.

The weather conditions during the investigation were extreme. At all sites the long-term annual mean temperature was exceeded by more than 1°C, during the growth period even by more than 3°C. In the same time precipitation delivered only about 60% of the long-term average. Drought occurred especially during the spring months. Vitis vinifera commonly reacts to drought by producing abscisine acid which causes a growth reduction of the vegetative plant organs. The generative parts remain less strongly affected. At two of the monitoring sites these effects could be observed as expected, while at the third site plant growth was not limited because of permanent supply of ground water in the rooting zone. At the sites limited in water supply the shoot dry matter production was reduced to up to 48% of the production observed in the years 1999-2001. Grape dry matter was only reduced to up to 59% of the earlier recorded amount. The data were used to parameterise the model to be able to reproduce plant growth under drought conditions. A clear improvement compared to the previous plant growth model version could be achieved. Now, the biomass development of the vine is a new feature in the output of the extended version of N-VINO 2.0 simulating the nitrogen turnover in vineyard soils and completes the output data of Nmin, soil water content, and N-leaching. The results can be presented in a time scale, in relation to soil depth, or as a comparison of measured data versus simulated data.

DOI:

Publication date: January 12, 2022

Issue: Terroir 2006

Type: Article

Authors

Claas NENDEL (1) and Stephan REUTER (2)

(1) Institute of Vegetable and Ornamental Crops, Department of Modelling and Knowledge Transfer, Theodor Echtermeyer-Weg 1, D-14979 Großbeeren, Germany
(2) Rhineland-Palatinate AgroScience, Institute for AgroEcology, Breitenweg 71, D-67435 Neustadt, Germany

Contact the author

Tags

IVES Conference Series | Terroir 2006

Citation

Related articles…

La viticulture durable: concept et application aux terroirs viticoles

Evoquer la notion de durabilité pour la vigne, plante multimillénaire, et le vin, tous deux intimement liés aux origines de notre civilisation, peut paraître un non-sens.

The role of terroir in tourism led amenity migration: contrasting effects in Tuscany and the Okanagan valley of British Columbia

Definitions of terroir elude consistent agreement. As defined geographical space the common denominators of its conceptualization include natural and cultural elements of life

Influence of trellis system and shoot density in yield and grape composition of a vineyard of Cabernet Sauvignon, in warm climate

In vineyards grown in warm areas, it is usual that the stage of maturity of the grapes is fast and easily reach a high concentration of sugar and low acidity, but not a adequate phenolic maturation. The geometry of the trellis system and the shoot density can modify the microclimate of the cluster and, therefore, the maturation process.

Volatile analysis of Botrytis contaminated grapes using headspace solid phase microextraction GC-MS

Grapes infected with grey mould due Botrytis cinerea are widespread in vineyards during certain growing conditions.

Terroir analysis and its complexity

Terroir is not only a geographical site, but it is a more complex concept able to express the “collective knowledge of the interactions” between the environment and the vines mediated through human action and “providing distinctive characteristics” to the final product (OIV 2010). It is often treated and accepted as a “black box”, in which the relationships between wine and its origin have not been clearly explained. Nevertheless, it is well known that terroir expression is strongly dependent on the physical environment, and in particular on the interaction between soil-plant and atmosphere system, which influences the grapevine responses, grapes composition and wine quality. The Terroir studying and mapping are based on viticultural zoning procedures, obtained with different levels of know-how, at different spatial and temporal scales, empiricism and complexity in the description of involved bio-physical processes, and integrating or not the multidisciplinary nature of the terroir. The scientific understanding of the mechanisms ruling both the vineyard variability and the quality of grapes is one of the most important scientific focuses of terroir research. In fact, this know-how is crucial for supporting the analysis of climate change impacts on terroir resilience, identifying new promised lands for viticulture, and driving vineyard management toward a target oenological goal. In this contribution, an overview of the last findings in terroir studies and approaches will be shown with special attention to the terroir resilience analysis to climate change, facing the use and abuse of terroir concept and new technology able to support it and identifying the terroir zones.