Terroir 1996 banner
IVES 9 IVES Conference Series 9 From local classification to regional zoning. The use of a geographic information system (GIS) in Franconia / Germany. Part 3: classification of soil parameters in vineyards

From local classification to regional zoning. The use of a geographic information system (GIS) in Franconia / Germany. Part 3: classification of soil parameters in vineyards

Abstract

La conservation de la fertilité du sol est un aspect primordial dans la viticulture durable. Différents paramètres, comme par exemple la topographie, la composition du sol, les conditions climatiques, influencent la fertilité du sol des surfaces viticoes. En ce qui concerne ces paramètres, de nouvelles technologies, telle qu’un SIG, permettent de réunir digitalement les informations sur le sol et le climat. Une représentation cartographique sur un SIG permet l’analyse de contextes complexes, une classification locale et la détermination d’un zonage régional. L’ensemble de ces informations améliore la recherche et simplifie la gestion des surfaces viticoles. Environ 20 % des surfaces viticoles franconiennes se situent sur des pentes escarpées. Ici, la protection du sol est essentielle à la conservation de sa fertilité. De nombreux paramètre du sol, comme sa texture, sa composition, sa teneur en éléments grossiers, l’épaisseur des horizons, le type du paillage, sont saisis dans le SIG. Ensuite, un zonage régional peut être effectué grâce à des types et des groupes de sol permettant par exemple des évaluations régionales de la capacité de stockage de l’eau. L’inclination, l’exposition, la longueur et la forme des surfaces viticoles ainsi que la direction d’écoulement des eaux de surface peuvent être déterminés par une modélisation de terrain en trois dimensions. Combinant les données pluviométriques ce système d’information permet la création de cartes régionales et locales sur le danger d’érosion dans les régions viticoles. Grâce aux paramètres du sol et autres données saisies dans le SIG, comme par exemple les informations sur les précipitations ou la végétation, il est possible d’évaluer quantitativement le déblayage annuel sur les terroirs utilisant le modèle d’érosion PC-ABAG (équivalent de l’USLE = Universal Soif Lass Equation). Grâce à cela on peut classifier le potentiel érosif sur des pentes escarpées à l’aide de cartes du danger d’érosion générées par le SIG et mener une évaluation quantitative du déblayage dans ces terroirs. Ceci permet une planification des mesures de protection contre l’érosion. Pour cette raison, le SIG en viticulture est un excellent instrument de travail pour les chercheurs et conseillers, et les producteurs de raisins en vue de l’analyse, l’enregistrement et l’évaluation des paramètres du sol et du danger d’érosion dans des surfaces viticoles.

The conservation of soil fertility is the first objective in sustainable viticulture. Various parameters as e.g. slope and exposition of vineyards, soil composition, climatic conditions (precipitation), etc. influence the soil fertility of vineyard sites. Considering these parameters, new computer software such as a GIS enables the digital compilation of information on soil and climate. GIS-mapping allows the analysis of complex correlations, creation of local classifications and the establishment of a regional zoning. The synoptical compilation of information by a GIS improves the research and simplifies vineyard management.
About 20 % of the Franconian vineyards are planted on steep slopes. Here, soil conservation is important to preserve soil fertility. Many local soil parameters as type, composition and rock content, thickness of the soil horizon, type of soil covering, etc. are recorded in the GIS. Subsequently, a regional zoning of soil types and groups can be created with help of the GIS.

Besides that, slope, orientation, length and shape of vineyards are deterrnined by a three­dimensional terrain modelling with the GIS. Connected with precipitation data, this enables the generation of local and regional erosion risk maps of viticultural regions. Soil and topographie parameters combined with other data recorded in the GIS, e.g. information on precipitation, type of vineyard (productive/new) and vegetation, allow a quantitative estimation of the average soil erosion per year within vineyards by using the erosion model PC-ABAG (equivalent to the USLE = Universal Sail Lass Equation). Thus, the erosion risk potential of steep slopes can be classified regionally with the help of GIS-generated erosion risk maps and the local quantitative estimation of soil erosion within individual vineyards. This allows planning of erosion protection measures. Therefore, the viticultural GIS is an excellent aid to researchers arid consultants, grape producers and wine growing estates for recording, analysing and assessing soil parameters and erosion risk in vineyards.

 

 

 

DOI:

Publication date: February 16, 2022

Issue: Terroir 2002 

Type: Article

Authors

A. Schwab; S. Königer; S. Michel

Bayerische Landesanstalt für Weinbau und Gartenbau, Abt. Weinbau und Rebenzüchtung, Hermstr. 8, D-97209 Veitshochheim, Germany

Contact the author

Keywords

zonage régional, SIG, sol, fertilité, danger d’érosion
regional zoning, GIS, soil, fertility, erosion risk

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Climate change impacts: a multi-stress issue

With the aim of producing premium wines, it is admitted that moderate environmental stresses may contribute to the accumulation of compounds of interest in grapes. However the ongoing climate change, with the appearance of more limiting conditions of production is a major concern for the wine industry economic. Will it be possible to maintain the vineyards in place, to preserve the current grape varieties and how should we anticipate the adaptation measures to ensure the sustainability of vineyards? In this context, the question of the responses and adaptation of grapevine to abiotic stresses becomes a major scientific issue to tackle. An abiotic stress can be defined as the effect of a specific factor of the physico-chemical environment of the plants (temperature, availability of water and minerals, light, etc.) which reduces growth, and for a crop such as the vine, the yield, the composition of the fruits and the sustainability of the plants. Water stress is in many minds, but a systemic vision is essential for at least two reasons. The first reason is that in natural environments, a single factor is rarely limiting, and plants have to deal with a combination of constraints, as for example heat and drought, both in time and at a given time. The second reason is that plants, including grapevine, have central mechanisms of stress responses, as redox regulatory pathways, that play an important role in adaptation and survival. Here we will review the most recent studies dealing with this issue to provide a better understanding of the grapevine responses to a combination of environmental constraints and of the underlying regulatory pathways, which may be very helpful to design more adapted solutions to cope with climate change.

Teasing apart terroir: the influence of management style on native yeast communities within Oregon wineries and vineyards

Newer sequencing technologies have allowed for the addition of microbes to the story of terroir. The same environmental factors that influence the phenotypic expression of a crop also shape the composition of the microbial communities found on that crop. For fermented goods, such as wine, that microbial community ultimately influences the organoleptic properties of the final product that is delivered to customers. Recent studies have begun to study the biogeography of wine-associated microbes within different growing regions, finding that communities are distinct across landscapes. Despite this new knowledge, there are still many questions about what factors drive these differences. Our goal was to quantify differences in yeast communities due to management style between seven pairs of conventional and biodynamic vineyards (14 in total) throughout Oregon, USA. We wanted to answer the following questions: 1) are yeast communities distinct between biodynamic vineyards and conventional vineyards? 2) are these differences consistent across a large geographic region? 3) can differences in yeast communities be tied to differences in metabolite profiles of the bottled wine? To collect our data we took soil, bark, leaf, and grape samples from within each vineyard from five different vines of pinot noir. We also collected must and a 10º brix sample from each winery. Using these samples, we performed 18S amplicon sequencing to identify the yeast present. We then used metabolomics to characterize the organoleptic compounds present in the bottled wine from the blocks the year that we sampled. We are actively in the process of analysing our data from this study.

Impact of geographical location on the phenolic profile of minority varieties grown in Spain. II: red grapevines

Because terroir and cultivar are drivers of wine quality, is essential to investigate theirs effects on polyphenolic profile before promoting the implantation of a red minority variety in a specific area. This work, included in MINORVIN project, focuses in the polyphenolic profile of 7 red grapevines minority varieties of Vitis vinifera L. (Morate, Sanguina, Santafe, Terriza Tinta Jeromo Tortozona Tinta) and Tempranillo) from six typical viticulture Spanish areas: Aragón (A1), Cataluña (A2), Castilla la Mancha (A3), Castilla –León (A4), Madrid (A5) and Navarra (A6) of 2020 season. Polyphenolic substances were extracted from grapes. 35 compounds were identified and quantified (mg subtance/kg fresh berry) by HPLC and grouped in anthocyanins (ANT) flavanols (FLAVA), flavonols (FLAVO), hydroxycinnamic (AH), benzoic (BA) acids and stilbenes (ST). Antioxidant activity (AA, mmol TE /g fresh berry) was determined by DPPH method. The results were submitted to a two-way ANOVA to investigate the influence of variety, area and their interaction for each polyphenolic family and cluster analysis was used to construct hierarchical dendrograms, searching the natural groupings among the samples. Sanguina (A3) had the most of total polyphenols while Tempranillo (A5) those of ANT. Sanguina (A2) and (A3) reached the highest values of FLAVO, FLAVA and AA. These two last samples had also the maximum of AA. The effect cultivar and area were significant for all polyphenolic families analyzed. A high variability due to variety (>50%) was observed in FLAVA and the maximum value of variability due to growing area was detected in AA (86.41%), ANT and FLAVO (51%); the interaction variety*zone was significant only for ANT, FLAVO, EST and AA. Finally, dendrograms presented five cluster: i) Sanguina (A2); ii) Sanguina (A3); iii) Tempranillo (A5); iv) Tempranillo (A3); Terriza (A3,A5), Morate (A5,A6); v) Santafé (A1,A6); Tortozona tinta (A1,A3,A6); Tinta Jeromo (A3,A4).

Optimizing stomatal traits for future climates

Stomatal traits determine grapevine water use, carbon supply, and water stress, which directly impact yield and berry chemistry. Breeding for stomatal traits has the strong potential to improve grapevine performance under future, drier conditions, but the trait values that breeders should target are unknown. We used a functional-structural plant model developed for grapevine (HydroShoot) to determine how stomatal traits impact canopy gas exchange, water potential, and temperature under historical and future conditions in high-quality and hot-climate California wine regions (Napa and the Central Valley). Historical climate (1990-2010) was collected from weather stations and future climate (2079-99) was projected from 4 representative climate models for California, assuming medium- and high-emissions (RCP 4.5 and 8.5). Five trait parameterizations, representing mean and extreme values for the maximum stomatal conductance (gmax) and leaf water potential threshold for stomatal closure (Ψsc), were defined from meta-analyses. Compared to mean trait values, the water-spending extremes (highest gmax or most negative Ysc) had negligible benefits for carbon gain and canopy cooling, but exacerbated vine water use and stress, for both sites and climate scenarios. These traits increased cumulative transpiration by 8 – 17%, changed cumulative carbon gain by -4 – 3%, and reduced minimum water potentials by 10 – 18%. Conversely, the water-saving extremes (lowest gmax or least negative Ψsc) strongly reduced water use and stress, but potentially compromised the carbon supply for ripening. Under RCP 8.5 conditions, these traits reduced transpiration by 22 – 35% and carbon gain by 9 – 16% and increased minimum water potentials by 20 – 28%, compared to mean values. Overall, selecting for more water-saving stomatal traits could improve water-use efficiency and avoid the detrimental effects of highly negative canopy water potentials on yield and quality, but more work is needed to evaluate whether these benefits outweigh the consequences of minor declines in carbon gain for fruit production.

Influence of agronomic practices in soil water content in mid-mountain vineyards

In the context of LIFE project MIDMACC (LIFE18 CCA/ES/001099), several pilots have been installed in vineyards in mid mountain areas of Catalonia (NE Spain) to test well stablished agronomic practices to increase the adaptation of Mediterranean mid mountain to climate change. Soil water content (SWC) at three different depths (15, 30 and 45cm) was measured in continuum from August 2020. One pilot (WC) included a well-established green cover (GC), a new GC (NC) and a conventional soil management (CM, tilling+herbicides). NC presented an intermediate state between WC and CM, responding similarly to CM in autumn but quickly reaching similar SWC to WC, then following the same evolution till next spring, with CM presenting lower values along autumn and winter. Then vegetation activation decreased SWC in all plots, (much slower in CM, lacking GC). Sensibility to spring rains is again intermediate for NC, which joins SWC evolution of CM by the end of spring till next autumn. It is expected that NC will resemble WC more and more as its GC develops. In the pilot combining vine training (VSP vs Gobelet) and hillside management (slope vs terrace), no clear pattern could be related with these conditions. However, both terraces seem to be more sensitive to spring rains. A third pilot included new vineyards (7 and 1 year old). In the new vineyard (N), higher canopy development, a spontaneous green cover and row straw resulted in a slower SWC dynamic, not so sensitive to rains but conserving more soil water in spring and most of summer, even with presumably a higher water extraction by vines. In the newest vineyard (VN) the deepest sensor is still sensitive to rain events all over the year and SWC is always highest at this depth, revealing small water capture by vines.