Terroir 1996 banner
IVES 9 IVES Conference Series 9 Efecto de distintos ambientes sobre las características físico – químicas y sensoriales del Montepulciano d’Abruzzo DOC

Efecto de distintos ambientes sobre las características físico – químicas y sensoriales del Montepulciano d’Abruzzo DOC

Abstract

La región de Abruzzo está situada entre los Apeninos y el mar Adriático, limitando al norte con el río Tronto y al sur con el Trigno. Desde un punto de vista físico se divide en dos franjas: una montañosa al oeste constituida por rocas calcáreas con frecuentes fenómenos de erosión debido a las corrientes de agua y a la naturaleza calcárea del terreno (“carsismo”) y otra al este, más cercana al mar, representada por una amplia zona de colinas constituida por terrenos arcilloso ​calcáreos y arenosos. Obviamente el clima está influido por la presencia de las grandes montañas del Gran Sasso y Maiella y también por la proximidad al mar Adriático. Así, en las cercanías de la zona montañosa, en la parte occidental, la temperatura difícilmente alcanza la media anual de 12°C, mientras que en la región mas cercana al mar la media anual oscila entre los 12° y los 16°C. Exponemos, a este respecto, las conclusiones de Matassa et al. (1992): “El clima de Abruzzo está influenciado fuertemente por la orografía montañosa y muestra una fuerte variabilidad, pasando de regiones templadas en la costa, a moderadamente templadas en los valles internos y las altas colinas litorales, a moderadamente frías y frías en las montañas”. Así que en general el clima se puede considerar apacible y a excepción de algunas zonas particularmente secas del sur de la región, se da un buen nivel de pluviosidad y es altamente soleado (Matassa et al., 1992). En el área observada por nosotros, en el territorio de Vasto, la pluviosidad, definida por los valores registrados en las estaciones del “Genio Civile” (ente estatal, perteneciente al ministerio italiano de obras públicas) durante el período 1965-93, muestra un aumento desde la costa hacia el interior, pasando de los 630 mm deVasto a los 850 mm de Montazzoli. La actividad vinícola juega un papel de primordial importancia en la economía agrícola del territorio de Vasto ya sea en términos de superficie cultivada como en términos de producción bruta a la venta. En dicha área, 6000 hectáreas están dedicadas al cultivo de la vid, de las cuales aproximadamente 480 (1.8 %) pertenecen a la colina del interior y la alta colina próxima a los montes, mientras que las restantes 5500 ha (92% del total) están localizadas en la colina litoral. La forma de cultivo mas difundida es el clásico emparrado con distancias de plantación de 2,5m x 2,5 m a pesar de que en los últimos años se han adoptado otros sistemas como el GDC.
La región de Abruzzo, a través del ARSSA (Agenzia Regionale per i Servizi di Sviluppo Agricolo), ha participado en el proyecto “Caracterización de vinos típicos” y ha seleccionado el territorio de Vasto para el programa de caracterización del vino Montepulciano d’Abruzzo a Denominación de Origen. El criterio que se ha adoptado para la división del territorio y para el muestreo, ha tenido en consideración esencialmente la disponibilidad térmica, definida a través de los índices bioclimáticos de Winkler e Huglin con referencia a un trabajo precedente que consideraba dichos parámetros a nivel regional (Matassa et al., 1992). Debemos considerar, además, que las características pedológicas cambian poco dentro de cada area examinada, y la forma de cultivo, el emparrado, es la única en todo el territorio. Se considera que la compleja orografía del territorio puede influir de forma notable sobre la distribución de la disponibilidad térmica, determinando una amplia posibilidad de condiciones ambientales dentro de cada zona DOC del vino.
Sobre la base de las consideraciones expuestas se han definido tres áreas a distinta distancia de la costa (fig.1) caracterizadas por disponibilidades térmicas en disminución. Dentro de cada una de ellas se han elegido 5 viñedos muestra (tab.1).
Area A: representativa de la colina litoral donde el cultivo vitícola es mayor. En esta zona el viñedo del ayuntamiento de Pollutri se diferencia de los otros (Casalbordino e Scerni) por la altitud de solamente 40 m sobre el nivel del mar.
Area B: representativa de la colina adyacente a la litoral. Los viñedos pertenecen a dos ayuntamientos , de los cuales uno (Furci) tiene una altitud 3 veces superior a los restantes.
Area C: representativa de la colina próxima a los montes. Los viñedos pertenecen a un solo ayuntamiento y la altitud de los viñedos va desde los 470 a los 555 m sobre el nivel del mar.

DOI:

Publication date: February 25, 2022

Issue: Terroir 2000

Type: Article

Authors

B.Di Lena (1), M. Ubigli (2), M.C. Cravero (2), D. Voerzio (2), M.C. Pazo-Alvarez (2)

(1) A.R.S.S.A. Centro Agrometeorologico Regionale ​Via Colle Comune 11, 66020 Scerni (CH)- Italia
(2) Istituto Sperimentale per l’Enologia, Via P. Micca 35, 14100 Asti (AT) – Italia

Tags

IVES Conference Series | Terroir 2000

Citation

Related articles…

How distinctive are single vineyard Gewürztraminer musts and wines from Alto Adige (Italy) based on untargeted analysis, sensory profiling, and chemometric elaboration?

Vitis vinifera L. ‘Gewürztraminer’ is a historical grape variety of Alto Adige (Südtirol), Italy, which is widely grown in the area of Tramin an der Weinstraße, but is also grown globally. It produces highly aromatic wines that are strongly influenced by the terroir of the vineyard sites where they are grown. This study looked at musts and young wines from ‘Gewürztraminer’ grapes harvested in seven distinct vineyards near Tramin and then processed at Cantina di Termeno, minimizing winemaking protocol variability. Samples were profiled using bidimensional gas chromatography–time-of-flight mass spectrometry, liquid chromatography coupled to electrochemical detection, and near-IR spectrometry. The data were subjected to Principle Component Analysis and Hierarchical Clustering Analysis. Sensory discriminant testing was undertaken using the sorting method with a semi-trained panel, and the data were processed using Multidimensional Scaling. Seven must/wine pairs could be distinguished based on their untargeted volatilome profiles and on sensory evaluation. As expected, there were greater differences in the volatile compounds between the wines than between the musts. The wines from vineyards 4 and 5 were nonetheless quite homogenous in terms of chemical and sensory analyses, as were the wines from vineyards 1 and 3. For the phenolic profile, differences were noted between the musts and wines of vineyards 2, 3, and 4, but the musts from vineyards 5 and 7 were similar. Sensory analysis showed the wines from vineyards 6 and 7 to be distinct from the rest. These results reinforce that the composition of ‘Gewürztraminer’ musts and wines is strongly determined by vineyard site, even in a small geographic area with high variability of the terroir (soil and microclimate), and that these differences are apparent in the flavours and aromas of the finished wines. Further confirmation would require a larger sample of wines, preferably from several vintages.

Adaptation to soil and climate through the choice of plant material

Choosing the rootstock, the scion variety and the training system best suited to the local soil and climate are the key elements for an economically sustainable production of wine. The choice of the rootstock/scion variety best adapted to the characteristics of the soil is essential but, by changing climatic conditions, ongoing climate change disrupts the fine-tuned local equilibrium. Higher temperatures induce shifts in developmental stages, with on the one hand increasing fears of spring frost damages and, on the other hand, ripening during the warmest periods in summer. Expected higher water demand and longer and more frequent drought events are also major concerns. The genetic control of the phenotypes, by genomic information but also by the epigenetic control of gene expression, offers a lot of opportunities for adapting the plant material to the future. For complex traits, genomic selection is also a promising method for predicting phenotypes. However, ecophysiological modelling is necessary to better anticipate the phenotypes in unexplored climatic conditions Genetic approaches applied on parameters of ecophysiological models rather than raw observed data are more than ever the basis for finding, or building, the ideal varieties of the future.

Variations of soil attributes in vineyards influence their reflectance spectra

Knowledge on the reflectance spectrum of soil is potentially useful since it carries information on soil chemical composition that can be used to the planning of agricultural practices. If compared with analytical methods such as conventional chemical analysis, reflectance measurement provides non-destructive, economic, near real-time data. This paper reports results from reflectance measurements performed by spectroradiometry on soils from two vineyards in south Brazil. The vineyards are close to each other, are on different geological formations, but were subjected to the same management. The objective was to detect spectral differences between the two areas, correlating these differences to variations in their chemical composition, to assess the technique’s potential to predict soil attributes from reflectance data.To that end, soil samples were collected from ten selected vine parcels. Chemical analysis yield data on concentration of twenty-one soil attributes, and spectroradiometry was performed on samples. Chemical differences significant to a 95% confidence level between the two studied areas were found for six soil attributes, and the average reflectance spectra were separated by this same level along most of the observed spectral domain. Correlations between soil reflectance and concentrations of soil attributes were looked for, and for ten soil traits it was possible to define wavelength domains were reflectance and concentrations are correlated to confidence levels from 95% to 99%. Partial Least Squares Regression (PLSR) analyses were performed comparing measured and predicted concentrations, and for fifteen out of 21 soil traits we found Pearson correlation coefficients r > 0.8. These preliminary results, which have to be validated, suggest that variations of concentration in the investigated soil attributes induce differences in reflectance that can be detected by spectroradiometry. Applications of these observations include the assessment of the chemical content of soils by spectroradiometry as a fast, low-cost alternative to chemical analytical methods.

Legacy of land-cover changes on soil erosion and microbiology in Burgundian vineyards

Soils in vineyards are recognized as complex agrosystems whose characteristics reflect complex interactions between natural factors (lithology, climate, slope, biodiversity) and human activities. To date, most of the unknown lies in an incomplete understanding of soil ecosystems, and specifically in the microbial biodiversity even though soil microbiota is involved in many key functions, such as nutrient cycling and carbon sequestration. Soil biological properties are indicative of soil quality. Therefore, understanding how soil communities are related to soil ecosystem functioning is becoming an essential issue for soil strategy conservation. Here, we propose to assess the importance of land-cover history on the present-day microbiological and physico-chemical properties. The studied area was selected in the Burgundian vineyards (Pernand-Vergelesses, Burgundy, France) where land occupation has been reconstructed over the last 40 years. Soil samples were collected in five areas reflecting various land cover history (forest, vineyards, shifting from forest to vineyards). For each area, physico-chemical parameters (pH, C, N, P, grain size) were measured and DNA was extracted to characterize the abundance and diversity of microbial communities. The obtained results show significant differences in the five areas suggesting that present-day microbial molecular biomass and bacterial taxonomic is partly inherited from past land occupation. Over longer period of time, such study of land-uses legacies may help to better assess ecosystem recovery and the impact of management practices for a better soil quality and vineyards sustainability.

Low-cost sensors as a support tool to monitor soil-plant heat exchanges in a Mediterranean vineyard

Mediterranean viticulture is increasingly exposed to more frequent extreme conditions such as heat waves. These extreme events co-occur with low soil water content, high air vapor pressure deficit and high solar radiant energy fluxes and result in leaf and berry sunburn, lower yield, and berry quality, which is a major constraint for the sustainability of the sector. Grape growers must find ways to proper and effectively manage heat waves and extreme canopy and berry temperatures. Irrigation to keep soil moisture levels and enable adequate plant turgor, and convective and evaporative cooling emerged as a key tool to overcome this major challenge. The effects of irrigation on soil and plant water status are easily quantifiable but the impact of irrigation on soil and canopy temperature and on heat convection from soil to cluster zone remain less characterized. Therefore, a more detailed quantification of vineyard heat fluxes is highly relevant to better understand and implement strategies to limit the effects of extreme weather events on grapevine leaf and berry physiology and vineyards performance. Low-cost sensor technologies emerge as an opportunity to improve monitoring and support decision making in viticulture. However, validation of low-cost sensors is mandatory for practical applicability. A two-year study was carried in a vineyard in Alentejo, south of Portugal, using low-cost thermal cameras (FLIR One, 80×60 pixels and FLIR C5, 160×120 pixels, 8-14 µm, FLIR systems, USA) and pocket thermohygrometers (Extech RHT30, EXTECH instruments, USA) to monitor grapevine and soil temperatures. Preliminary results show that low-cost cameras can detect severe water stress and support the evaluation of vertical canopy temperature variability, providing information on soil surface temperature. All these thermal parameters can be relevant for soil and crop management and be used in decision support systems.