Terroir 1996 banner
IVES 9 IVES Conference Series 9 La vinificación de las uvas aromáticas: Moscateles y Malvasías

La vinificación de las uvas aromáticas: Moscateles y Malvasías

Abstract

Las uvas aromáticas se pueden dividir en dos clases, Moscateles y Malvasías, dependiendo del hecho de que el linalol o el geraniol, respectivamente, sean los alcoholes terpénicos monohidroxilados que predominan en el jugo de la uva. Dentro de cada clase existen numerosas subclases que se diferencian por las relaciones entre los otros alcoholes terpénicos mono y dihidroxilados, en forma libre y glicosilada. Otra diferencia entre los Moscateles y las Malvasías es la cantidad de compuestos terpénicos libres del mosto, (los terpenos del hollejo, en las dos clases, se encuentran casi en su totalidad como formas glicosiladas) que puede ser alto como en el caso del Moscatel (linalol, óxido trans piránico del linalol, 2,6-dimetil-3,7-octadien-2,6-diol) o mas bién bajo como en el caso de las Malvasías (geraniol, 2,6-dimetil-3,7-octadien-2,6-diol), mientras que en los hollejos es una característica común a las dos clases la presencia de elevadas cantidades de nerol y de geraniol en forma glicosilada. La composición terpénica de las dos variedades condiciona, además del aroma del vino final, la tecnología de producción.En Italia con el “Moscato bianco” y con las Malvasías (“Malvasia di Casorzo”, “Malvasia di Castelnuovo don Bosco”, esta última en muchos aspectos parecida a los Moscateles, “Brachetto d’Acqui”, que son todas variedades tintas) se preparan dos tipos de vino: uno espumoso y uno no espumoso. El primero se caracteriza por un contenido alcohólico de aproximadamente un 7%y una concentración de azúcares de aproximadamente 70 g/L y el segundo por un grado alcohólico del 5 % y una cantidad de azúcares variable dependiendo de los gustos del productor.En la vinificación del “Moscato bianco” se utiliza solo el mosto (una eventual criomaceración no conlleva un aumento sensible en compuestos terpénicos), que es rico de linalol que no resulta ni absorbido ni metabolizado por las levaduras, mientras que en el caso de las Malvasías tintas, para cuya vinificación se utilizan también los hollejos, el geraniol, practicamente el único alcohol terpénico monohidroxilado presente en el mosto, es metabolizado parcialmente por las levaduras y en parte reducido a citronellol y estos dos compuestos, además del nerol, son transformados en derivados acetilados. Además, a causa de las elevadas cantidades de glucosa que se encuentran en el mosto durante toda la fase de preparación de los vinos de estas variedades, los enzimas glicosidásicos, del mosto o de las levaduras, no pueden transformar en los respectivos aglicones los glicósidos del nerol y del geraniol presentes en el mosto, que quedan, por lo tanto, en forma glicosilada, es decir, no aromática, en el vino final. Las técnicas tradicionales de vinificación establecen, para la extracción del color y de los compuestos terpénicos de los hollejos de las Malvasías tintas, continuos remontados cuando la fermentación todavía no ha empezado, o una fermentación parcial en presencia de los hollejos. Estas dos técnicas son insuficientes sea para extraer la gran cantidad de glicósidos del nerol y del geraniol de los hollejos, sea para hidrolizar los glicósidos terpénicos. En este trabajo se presenta una nueva técnica de vinificación, que favorece la extracción y la hidrólisis de los compuestos terpénicos de los hollejos de las Malvasías tintas y que incrementa sensiblemente la intensidad del aroma y la calidad de los vinos que se obtienen con esta variedad.

DOI:

Publication date: February 24, 2022

Issue: Terroir 2000 

Type: Article

Authors

Rocco Di Stefano*, Emilia García Moruno* and Monica Ribaldone**

*Istituto Sperimentale per l’Enologia, via P. Micca 35 — 14100 Asti (Italia)
**Consorzio per la tutela del Brachetto

Tags

IVES Conference Series | Terroir 2000

Citation

Related articles…

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.

Grapevine sugar concentration model in the Douro Superior, Portugal

Increasingly warm and dry climate conditions are challenging the viticulture and winemaking sector. Digital technologies and crop modelling bear the promise to provide practical answers to those challenges. As viticultural activities strongly depend on harvest date, its early prediction is particularly important, since the success of winemaking practices largely depends upon this key event, which should be based on an accurate and advanced plan of the annual cycle. Herein, we demonstrate the creation of modelling tools to assess grape ripeness, through sugar concentration monitoring. The study area, the Portuguese Côa valley wine region, represents an important terroir in the “Douro Superior” subregion. Two varieties (cv. Touriga Nacional and Touriga Franca) grown in five locations across the Côa Region were considered. Sugar accumulation in grapes, with concentrations between 170 and 230 g l-1, was used from 2014 to 2020 as an indicator of technological maturity conditioned by meteorological factors. The climatic time series were retrieved from the EU Copernicus Service, while sugar data were collected by a non-profit organization, ADVID, and by Sogrape, a leading wine company. The software for calibrating and validating this model framework was the Phenology Modeling Platform (PMP), version 5.5, using Sigmoid and growing degree-day (GDD) models for predictions. The performance was assessed through two metrics: Roots Mean Square Error (RMSE) and efficiency coefficient (EFF), while validation was undertaken using leave-one-out cross-validation. Our findings demonstrate that sugar content is mainly dependent on temperature and air humidity. The models achieved a performance of 0.65

Deconstructing the soil component of terroir: from controversy to consensus

Wine terroir describes the collectively recognized relation between a geographical area and the distinctive organoleptic characteristics of the wines produced in it. The overriding objective in terroir studies is therefore to provide scientific proof relating the properties of terroir components to wine quality and typicity. In scientific circles, the role of climate (macro-, meso- and micro-) on grape and wine characteristics is well documented and accepted as the most critical. Moreover, there has been increasing interest in recent years about new elements with possible importance in shaping wine terroir like berry/leaf/soil microbiology or even aromatic plants in proximity to the vineyard conferring flavors to the grapes. However, the actual effect of these factors is also dependent on complex interactions with plant material (variety/clone, rootstock, vine age) and with human factors.
The contribution of soil, although a fundamental component of terroir and extremely popular among wine enthusiasts, remains a much-debated issue among researchers. The role of geology is probably the one mostly associated by consumers with the notion of terroir with different parent rocks considered to give birth to different wine styles. However, the relationship between wine properties and the underlying parent material raises a lot of controversy especially regarding the actual existence of rock-derived flavors in the wine (e.g. minerality). As far as the actual soil properties are concerned, the effect of soil physical properties is generally regarded as the most significant (e.g sandy soils being associated with lighter wines while those on clay with colored and tannic ones) mostly through control of water availability which ultimately modifies berry ripening conditions either directly by triggering biosynthetic pathways, or indirectly by altering vigor and yield components. The role of soil chemistry seems to be weakly associated to wine sensory characteristic, although N, K, S and Ca, but also soil pH, are often considered important in the overall soil effect.
Recently, in the light of evidence provided by precision agriculture studies reporting a high variability of vineyard soils, the spatial scale should also be taken into consideration in the evaluation of the soil effects on wines. While it is accepted that soil effects become more significant than climate on a local level, it is not clear whether these micro-variations of vineyard soils are determining in the terroir effect. Moreover, as terroir is not a set of only natural factors, the magnitude of the contribution of human-related factors (irrigation, fertilization, soil management) to the soil effect still remains ambiguous. Lastly, a major shortcoming of the majority of works about soil effects on wine characteristics is the absence of connection with actual vine physiological processes since all soil effects on grape and wine chemistry and sensorial properties are ultimately mediated through vine responses.
This article attempts to breakdown the main soil attributes involved in the terroir effect to suggest an improved understanding about soil’s true contribution to wine sensory characteristics. It is proposed that soil parameters per se are not as significant determining factors in the terroir effect but rather their mutual interactions as well as with other natural and human factors included in the terroir concept. Consequently, similarly to bioclimatic indices, composite soil indices (i.e. soil depth, water holding capacity, fertility, temperature etc), incorporating multiple soil parameters, might provide a more accurate and quantifiable means to assess the relative weight of the soil component in the terroir effect.

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.

Modeling island and coastal vineyards potential in the context of climate change

Climate change impacts regional and local climates, which in turn affects the world’s wine regions. In the short term, these modifications rises issues about maintaining quality and style of wine, and in a longer term about the suitability of grape varieties and the sustainability of traditional wine regions. Thus, adaptation to climate change represents a major challenge for viticulture. In this context, island and coastal vineyards could become coveted areas due to their specific climatic conditions. In regions subject to warming, the proximity of the sea can moderate extremes temperatures, which could be an advantage for wine. However, coastal and island areas are particular prized spaces and subject to multiple pressures that make the establishment or extension of viticulture complex.
In this perspective, it seems relevant to assess the potentialities of coastal and island areas for viticulture. This contribution will present a spatial optimization model that tends to characterize most suitable agroclimatic patterns in historical or emerging vineyards according to different scenarios. Thanks to an in-depth bibliography a global inventory of coastal and insular vineyards on a worldwide scale has been realized. Relevant criteria have been identified to describe the specificities of these vineyards. They are used as input data in the optimization process, which will optimize some objectives and spatial aspects. According to a predefined scenario, the objectives are set in three main categories associated with climatic characteristics, vineyards characteristics and management strategies. At the end of this optimization process, a series of maps presents the different spatial configurations that maximize the scenario objectives.