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…

Effect of the commercial inoculum of arbuscular mycorrhiza in the establishment of a commercial vineyard of the cultivar “Manto negro

The favorable effect of symbiosis with arbuscular mycorrhizal fungi (AMF) has been known and studied since the 60s. Nowadays, many companies took the chance to start promoting and selling commercial inoculants of AMF, in order to be used as biofertilizers and encourage sustainable biological agriculture. However, the positive effect of these commercial biofertilizers on plant growth is not always demonstrated, especially under field conditions. In this study, we used a commercial inoculum on newly planted grapevines of a local cultivar grafted on a common rootstock R110. We followed the physiological status of vines, growth and productivity and functional biodiversity of soil bacteria during the first and second years of 20 inoculated with commercial inoculum bases on Rhizophagus irregularis and Funeliformis mosseaeAMF at field planting time and 20 non-inoculated control plants. All the parameters measured showed a neutral to negative effect on plant growth and production. The inoculated plants always presented lower values of photosynthesis, growth and grape production, although in some cases the differences did not reach statistical significance. On the contrary, the inoculation supposed an increase of the bacterial functional diversity, although the differences were not statistically significant either. Several studies show that the effect of inoculation with AMF is context-dependent. The non-favorable effects are probably due to inoculation ineffectiveness under complex field conditions and/or that, under certain conditions, AMF presence may be a parasitic association. This puts into question the effectiveness of its application in the field. Therefore, it is recommended to only resort to this type of biofertilizer when the cultivation conditions require it (e.g., very low previous microbial diversity, foreseeable stress due to drought, salinity, or lack of nutrients) and not as a general fertilization practice.

De novo Vitis champinii whole genome assembly allows rootstock-specific identification of potential candidate genes for drought and salt tolerance

Vitis champinii cultivars Ramsey and Dog-ridge are main choices for rootstocks to adapt viticulture in semi-arid and arid regions thanks to their distinctive tolerance to drought and salinity. However, genetic studies on non-vinifera rootstocks have heavily relied on the grapevine (Vitis vinifera) reference genome, which difficulted the assessment of the genetic variation between rootstock species and grapevines. In the present study, this limitation is addressed by introducing a novo phased genome assembly and annotation of Vitis champinii. This new Vitis champinii genome was employed as reference for mapping RNA-seq reads from the same species under drought and salt stresses, and for comparison the same reads were also mapped to the Vitis vinifera PN40024.V4 reference genome. A significant increase in alignment rate was gained when mapping Vitis champinii RNA-seq reads to its own genome, compared to the Vitis vinifera PN40024.V4 reference genome, thus revealing the expression levels of genes specific to Vitis champinii. Moreover, differences in coding sequences were observed in ortholog genes between Vitis champinii and Vitis vinifera, which therefore challenges previous differential expression analyses performed between contrasting Vitis genotypes on the same gene from the Vitis vinifera genome. Genes with possible implications in drought and salt tolerance have been identified across the genome of Vitis champinii, and the same genomic data can potentially guide the discovery of candidate genes specific from Vitis champinii for other traits of interest, therefore becoming a valuable resource for rootstock breeding designs, specially towards increased drought and salinity due to climate change.

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.

δ13C : A still underused indicator in precision viticulture  

The first demonstration of the interest of carbon isotope composition of sugars in grapevine, as an integrated indicator of vineyard water status, dates back to 2000 (Gaudillère et al., 1999; Van Leeuwen et al., 2001). Thanks to the isotopic discrimination of Carbon that takes place during plant photosynthesis, under hydric stress conditions, it is possible to accurately estimate the photosynthetic activity. Ever since, δ13C has been widely applied with success to zonation, terroir studies and vine physiology research, but is still not widely used by viticulturists. This is quite astonishing by considering the impact of global warming on viticulture and the need to improve water management, that would justify a widespread use of δ13C.
The lack of private laboratories proposing the analysis, the cost of the technology, as well as the long analytical delays, have been detrimental to its development. Some laboratories tried to overcome the analytical difficulties of isotopic analysis by using fourier transformed infrared spectroscopy, as a fast and cheap alternative to the official OIV method (IRMS). These claimed FTIR models have never been published or peer reviewed and cannot be considered robust. In this work, thanks to the recent acquisition of IRMS technology, new modern and robust applications of δ13C for viticulture are proposed. This includes the use of the analysis to make parcel separations at harvesting, the possibility to increase the precision of hydric stress cartography and the potential cost reduction when compared with Scholander pressure bomb analysis.

Pruned vine biomass exclusion from a clay loam vineyard soil – examining the impact on physical/chemical properties

The wine industry worldwide faces increasing challenges to achieve sustainable levels of carbon emission mitigation. This project seeks to establish the feasibility of harvesting winter pruned vineyard biomass (PVB) for potential use in carbon footprint reduction, through its use as a renewable biofuel for energy production. In order to make this recommendation, technical issues such as the potential environmental impact, chemical composition and fuel suitability, and logistical challenges of harvesting biomass needs to be understood to compare with the results from similar studies. Of particular interest is the role PVB plays as a carbon source in vineyard soils and what effect annual removal might have on soil carbon sequestration. A preliminary trial was established in the Waite Campus vineyard (University of Adelaide) to test current management strategies. Vines are grown in a Eutrophic, Red Dermosol clay loam soil with well managed midrow swards. A comparison was undertaken of mid-row treatments in two 0.25 Ha blocks (Shiraz and Semillon), including annual cultivation for seed bed preparation, the deliberate exclusion of PVB (25 years) and incorporation of PVB (13 years) at an average of 3.4 and 5.5 Mg/Ha-1 for Shiraz and Semillon respectively. In both 0-10cm and 10-30cm soil core sample depths, combined soil carbon % measures in the desired range of 1.80 to 3.50, were not significantly different between treatments or cultivars and yielded an estimated 42 Mg/ha-1 of sequestered soil carbon. Other key physical and chemical measures were likewise not significantly different between treatments. Preliminary results suggest that in a temperate zone vineyard, managed such as the one used in this study, there is no long term negative impact on soil carbon sequestration through removing PVB. This implies that growers could confidently harvest PVB for use in several end fates including as a bio fuel.