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…

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.

Copper contamination in vineyard soils of Bordeaux: spatial risk assessment for the replanting of vines and crops

Copper (Cu) is widely and historically used in viticulture as a fungicide against mildew. Cu has a strong affinity for soil organic matter and accumulates in topsoil horizons. Thus, Cu may negatively affect soil organisms and plants, consequently reducing soil fertility and productivity. The Bordeaux vineyards have the largest vineyard surfaces (26%) within French controlled appellation and a great proportion of French wine production (around 5 million hl per year). Considering the local context of vineyard surfaces decreasing (vine uprooting) and possible new crop plantation, the issue of Cu potential toxicity rises. Therefore, the aims of this work are firstly to evaluate the Cu contamination in vineyard soils of Bordeaux, secondly to produce a risk assessment map for new vine or crop plantation. We used soil analyses from several local studies to build a database with 4496 soil horizon samples. The database was enhanced by means of pedotransfer functions in order to estimate the bioaccessible (EDTA-extractable) Cu in soils of samples without measurements. From this database, 1797 georeferenced samples with CuEDTA concentrations in the topsoil (0-50 cm depth) were used for kriging interpolation in order to produce the spatial distribution map of CuEDTA in vineyard soils. Then, the spatial distribution of Cu was crossed with vine uprooting surfaces and municipality boundaries. CuEDTAconcentrations ranged from 0.52 to 459 mg/kg and showed clear anomalies. Our results from spatial analysis showed that almost 50% of vineyard soil surfaces have CuEDTA concentrations higher than 30 mg/kg (moderate risk for new plantation) and 20% with concentrations higher than 50 mg/kg (high risk for new plantation). A decision-support map based on municipalities was realised to provide a simple tool to stakeholders concerned by land use management.

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.

Influence of grapevine rootstock/scion combination on rhizosphere and root endophytic microbiomes

Soil is a reservoir of microorganisms playing important roles in biogeochemical cycles and interacting with plants whether in the rhizosphere or in the root endosphere. The composition of the microbial communities thus impacts the plant health. Rhizodeposits (such as sugar, organic and amino acids, secondary metabolites, dead root cells …) are released by the roots and influence the communities of rhizospheric microorganisms, acting as signaling compounds or carbon sources for microbes. The composition of root exudates varies depending on several factors including genotypes. As most of the cultivated grapevines worldwide are grafted plants, the aim of this study was to explore the influence of rootstock and scion genotypes on the microbial communities of the rhizosphere and the root endosphere. The work was conducted in the GreffAdapt plot (55 rootstocks x 5 scions), in which the 275 combinations have been planted into 3 blocks designed according to the soil resistivity. Samples of roots and rhizosphere of 10 scion x rootstock combinations were first collected in May among the blocks 2 and 3. The quantities of bacteria, fungi and archaea have been assessed in the rhizosphere by quantitative PCR, and by cultivable methods for bacteria and fungi. The communities of bacteria, fungi and arbuscular mycorrhizal fungi (AMF) was analyzed by Illumina sequencing of 16S rRNA gene, ITS and 28S rRNA gene, respectively. The level of mycorrhization was also evaluated using black ink coloration of newly formed roots harvested in October. The level of bacteria, fungi and archaea was dependent on rootstock and scion genotypes. A block effect was observed, suggesting that the soil characteristics strongly influenced the microorganisms from the rhizosphere and root endosphere. High-throughput sequencing of the different target genes showed different communities of bacteria, fungi and AMF associated with the scion x rootstock combinations. Finally, all the combinations were naturally mycorrhized. The root mycorrhization intensity was influenced by the rootstock genotype, but not by the scion one. Altogether, these results suggest that both rootstock and scion genotypes influence the rhizosphere and root endophytic microbiomes. It would be interesting to analyze the biochemical composition of the rhizodeposition of these genotypes for a better understanding of the processes involved in the modulation of these microbiomes. Moreover, crossing our data with the plant agronomic characteristics could provide insights into their roles on plant fitness.

Under-vine management effects on grapevine production, soil properties and plant communities in South Australia

Under-vine (UV) management has traditionally consisted of synthetic herbicide use to limit competition between weeds and grapevines. With growing global interest towards non-synthetic chemical use, this study aimed to capture the effects of alternative UV management at two commercial Shiraz vineyards in South Australia, where the sole management variables were UV management since 2016. In adjacent treatment blocks, cultivation (CU) was compared to spontaneous vegetation (SV) in McLaren Vale (MV), and herbicide was compared to SV in Eden Valley (EV). Soil water infiltration rates were slower and grapevine stem water potential was lower in CU compared to SV in MV, with the latter having a plant community dominated by soursob (Oxalis pes-caprae) during winter; while in EV, there was little separation between the treatments. Yields were affected at both sites, with SV being higher in MV and HE being higher in EV. In MV, the only effect on grape must was a lower 13C:12C isotope ratio in CU, indicating greater grapevine water stress. In the grape must at EV, SV had higher total soluble solids, total phenolics, anthocyanins, and yeast available nitrogen; and lower pH and titratable acidity. Pruning weights were not affected by the treatments in MV, while they were higher in HE at EV. Assessments revealed that the differing soil types at the two sites were likely the main determinants of the opposing production outcomes associated with UV management. In the silty loam soil of MV, the higher yields in SV were likely due to more plant-available water, as a potential result of the continuous soil bio-pores formed by winter UV vegetation. Conversely, in the loamy sand soils of EV with a lower cation exchange capacity, the lower yields and pruning weights in SV suggest the UV vegetation competed significantly with the grapevines for available water and nutrients.