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 projections over France wine-growing region and its potential impact on phenology

Climate change represents a major challenge for the French wine industry. Climatic conditions in French vineyards have already changed and will continue to evolve. One of the notable effects on grapevine is the advancing growing season. The aim of this study is to characterise the evolution of agroclimatic indicators (Huglin index, number of hot days, mean temperature, cumulative rainfall and number of rainy days during the growing season) at French wine-growing regions scale between 1980 and 2019 using gridded data (8 km resolution, SAFRAN) and for the middle of the 21th century (2046-2065) with 21 GCMs statistically debiased and downscaled at 8 km. A set of three phenological models were used to simulate the budburst (BRIN, Smoothed-Utah), flowering, veraison and theoretical maturity (GFV and GSR) stages for two grape varieties (Chardonnay and Cabernet-Sauvignon) over the whole period studied. All the French wine-growing regions show an increase in both temperatures during the growing season and Huglin index. This increase is accompanied by an advance in the simulated flowering (+3 to +9 days), veraison (+6 to +13 days) and theoretical maturity (+6 to +16 days) stages, which are more noticeable in the north-eastern part of France. The climate projections unanimously show, for all the GCMs considered, a clear increase in the Huglin index (+662 to 771 °C.days compared to the 1980-1999 period) and in the number of hot days (+5.6 to 22.6 days) in all the wine regions studied. Regarding rainfall, the expected evolution remains very uncertain due to the heterogeneity of the climates simulated by the 21 models. Only 4 regions out of 21 have a significant decrease in the number of rainy days during the growing season. The two budburst models show a strong divergence in the evolution of this stage with an average difference of 18 days between the two models on all grapevine regions. The theoretical maturity is the most impacted stage with a potential advance between 40 and 23 days according to wine-growing regions.

Protected Designation of Origin (D.P.O.) Valdepeñas: classification and map of soils

The objective of the work described here is the elaboration of a map of the different types of vineyard soils that to guide the famers in the choice of the most productive vine rootstocks and varieties. 90 vineyard soils profiles were analysed in the entire territory of the Origen Denominations of Valdepeñas. The sampling was carried out in 2018 (June to October) by making a sampling grid, followed by photointerpretation and control in the field. The studied soils can be grouped into 9 different soil types (according to FAO 2006 classification): Leptosols, Regosols, Fluvisols, Gleysols, Cambisols, Calcisols, Luvisols and Anthrosols. A map showing the soil distribution with different type of soils has been made with the ArcGIS program. Regarding to the choice of rootstock, Calcisoles are soils with a high active limestone content, so the rootstocks used in these soils must be resistant to this parameter; Luvisols are deep soils with high clay content, so they will support vigorous rootstocks. Because the cartographic units are composed of two or more subgroups, with are associated in variable proportions, 9 different soil associations have been established; Unit 1: Leptosols, Cambisols and Luvisols (80%, 15% and 5% respectively); Unit 2: Cambisols with Regosols and Luvisols (40%, 30% and 30% respectively); Unit 3: Cambisols and Gleysols with Regosols (40%, 40% and 20% respectively); Unit 4: Regosols with Cambisols, Leptosols and Calcisols (40%, 30%, 15% and 15% respectively); Unit 5: Cambisols, Leptosols, Calcisols and Regosols (25% each of them); Unit 6: Luvisols with Cambisol and Calcisols (80%, 10% and 10% respectively); Unit 7: Luvisols and Calcisols with Cambisols (40%, 40% and 20% respectively); Unit 8: Calcisols with, Cambisols and Luvisols (80%, 10% and 10% respectively); Unit 9: Anthrosols. These study allow to elaborate the first map of vineyard soils of this Protected Designation of Origin in Castilla-La Mancha.

Updating the Winkler index: An analysis of Cabernet sauvignon in Napa Valley’s varied and changing climate

This study aims to create an updated, agile viticultural climate index (similar to the Winkler Index) by performing in-depth analyses of current and historical data from industry partners in several major winegrowing regions. The Winkler Index was developed in the early twentieth century based on analysis of various grape-growing regions in California. The index uses heat accumulation (i.e. Growing Degree Days) throughout the growing season to determine which grape varieties are best suited to each region. As viticultural regions are increasingly subject to the complexity and uncertainty of a changing climate, a more rigorous, agile model is needed to aid grape growers in determining which cultivars to plant where. For the first phase of this study, 21 industry partners throughout Napa Valley shared historical phenology, harvest, viticultural practice, and weather data related to their Cabernet sauvignon vineyard blocks. To complement this data, berry samples were collected throughout the 2021 growing season from 50 vineyard blocks located throughout 16 American Viticultural Areas that were then analyzed for basic berry chemistry and phenolics. These blocks have been mapped using a Geographic Information System (GIS), enabling analysis of altitude, vineyard row orientation, slope, and remotely sensed climate data. Sampling sites were also chosen based on their proximity to a weather station. By analyzing historical data from industry partners and data specifically collected for this study, it is possible to identify key parameters for further analysis. Initial results indicate extreme variability at a high spatial resolution not currently accounted for in modern viticultural climate indices and suggest that viticultural practices play a major role. Using the structure of data collection and analyses developed for the first phase, this project will soon be expanded to other wine regions globally, while continuing data collection in Napa Valley.

Making sense of available information for climate change adaptation and building resilience into wine production systems across the world

Effects of climate change on viticulture systems and winemaking processes are being felt across the world. The IPCC 6thAssessment Report concluded widespread and rapid changes have occurred, the scale of recent changes being unprecedented over many centuries to many thousands of years. These changes will continue under all emission scenarios considered, including increases in frequency and intensity of hot extremes, heatwaves, heavy precipitation and droughts. Wine companies need tools and models allowing to peer into the future and identify the moment for intervention and measures for mitigation and/or avoidance. Previously, we presented conceptual guidelines for a 5-stage framework for defining adaptation strategies for wine businesses. That framework allows for direct comparison of different solutions to mitigate perceived climate change risks. Recent global climatic evolution and multiple reports of severe events since then (smoke taint, heatwave and droughts, frost, hail and floods, rising sea levels) imply urgency in providing effective tools to tackle the multiple perceived risks. A coordinated drive towards a higher level of resilience is therefore required. Recent publications such as the Australian Wine Future Climate Atlas and results from projects such as H2020 MED-GOLD inform on expected climate change impacts to the wine sector, foreseeing the climate to expect at regional and vineyard scale in coming decades. We present examples of practical application of the Climate Change Adaptation Framework (CCAF) to impacts affecting wine production in two wine regions: Barossa (Australia) and Douro (Portugal). We demonstrate feasibility of the framework for climate adaptation from available data and tools to estimate historical climate-induced profitability loss, to project it in the future and to identify critical moments when disruptions may occur if timely measures are not implemented. Finally, we discuss adaptation measures and respective timeframes for successful mitigation of disruptive risk while enhancing resilience of wine systems.

Traditional agroforestry vineyards, sources of inspiration for the agroecological transition of viticulture

A unique “terroir” can be found in southern Bolivia, which combines the specific features of climate, topography and altitude of high valleys, with the management of grapevines staked on trees. It is one of the rare remnants of agroforestry viticulture. A survey was carried out among 29 grapegrowers in three valleys, to characterize the structure and management of these vineyards, and identify the services they expect from trees. Farms were small (2.2 ha on average) and 85% of vineyards were less than 1 ha. Viticulture was associated with vegetable, fruit and fodder production, sometimes in the same fields. Molle trees were found in all plots, together with one or two other native tree species. Traditional grapevine varieties such as Negra Criolla, Moscatel de Alejandría and Vicchoqueña were grown with a large range of densities from 1550 to 9500 vines ha-1. From 18 to 30% of them were staked on trees, with 1.2 to 4.9 vines per tree. The management of these vineyards (irrigation, fertilization and grapevine protection) was described, the most particular technical operation being the coordinated pruning of trees and grapevines. Three types of management could be identified in the three valleys. Grapegrowers had a clear idea of the ecosystem services they expected from trees in their vineyards. The main one was protection against climate hazards (hail, frost, flood). Then they expected benefits in terms of pest and disease control, improvement of soil fertility and resulting yield. At last, some producers claimed that tree-staking was quicker and cheaper than conventional trellising. It can be hypothesized then that agroforestry is a promising technique for the agroecological transition of viticulture. Its contribution to the “terroir” of the high valleys of southern Bolivia and its link with the specificities of the wines and spirits produced there remain to be explored.