Terroir 2010 banner
IVES 9 IVES Conference Series 9 Geology and landscape as determining factors in microfields and development of the different Spanish appellations of origin

Geology and landscape as determining factors in microfields and development of the different Spanish appellations of origin

Abstract

Dividing agrarian exploitations into microfields is a problem that influences the modern viticulture in a very important way. The aim of this work is the study of the influence of Geology and Geomorphology in agricultural structures, and more exactly applied to viticulture microfields, as determining factors in evolution and development of certain Appellation of Origin (AO). The field division of three AO in the Northwest of Spain (Toro, Bierzo, Arribes) is compared. These three regions were chosen because they have similar influence elements.
The Toro AO (total area 76.076,43 ha; vineyard area 4.887,12 ha) is located to the West of Duero river basin and it is formed with limestone and carbonated detritic materials from the tertiary series and with the materials from the glacis and the medium and low terraces of the own river. In this context the altitude difference is small (650-825 m) and the shapes are flat and smooth in the quaternary relieve and undulating in the link tertiary surfaces with slopes under 20%. There are neither rocky outcrops nor stoniness to block the crop technical development.
The Bierzo AO (total area 142.672,08 ha; vineyard area 3.785,33 ha) is located in a sinking intermontane depression basin that is filled up with terraces materials, plioquaternary piedmont which are locally linked through tertiary detritical series with quartzite and schist materials that end in the primary mountainous edges due to basin close. The difference among cotes is important (525-1100 m) and the slopes are very changeable; flat in the alluvials, medium and high in the tertiary relieves and very high in the mountainous ones. Only in the mountainous basin edges there are some zones with rocky outcrops that block the crop technical development.
The Arribes AO (total area 101.969,94 Ha, vineyard area 1.66679 Ha) is located in an erosive surface that includes a whole of deep incisions and canyons of the Duero and its associated systems. In this surface the granite materials and schist, gneiss and quartzite paleozoic materials are predominant. These materials are locally covered with rests of glacis and quaternary materials and these filled up some depressions. The relief is very varied, from soft undulating surfaces in the erosive zone to vertical walls related to the incisions. In the whole AO the rocky outcrops and the stoniness make up or have made up an obstacle to the crop technical development.
Even though in the three AO a selection of the medium size is appreciated, the vineyard medium size is more than two times smaller in Toro AO (2.84) and in Bierzo AO (2.84), but more than five times smaller (5.54) in Arribes AO. On the other hand, while in the Toro AO, the wine-grower can select the better quality zones and zones with a proper structure and a independent of the considered elements, in Bierzo AO and in Arribes AO the vine-growers election possibilities are much lower or there are problems with the slopes which are often in relationships to the soil small effective depth, or if these problems have been eliminated by the effort through centuries the microfields division impede the vineyard crop technical development; the vineyard medium size is more than ten times higher in Toro AO, than in Bierzo AO and Arribes AO.

DOI:

Publication date: December 3, 2021

Issue: Terroir 2010

Type: Article

Authors

Vicente GOMEZ-MIGUEL (1), Vicente SOTES (1)

(1) Universidad Politécnica de Madrid (UPM). Avda Complutense s/n. 28040-Madrid, Spain

Contact the author

Keywords

terroir, zoning, landscape, geology, microfield, Appellations of Origin, Spain

Tags

IVES Conference Series | Terroir 2010

Citation

Related articles…

Influence of withering on valpolicella docgs grapes volatile composition

The blend of grapes used in the production of the four Valpolicella PDOs red wines, namely Valpolicella, Valpolicella Classico Superiore, Recioto della Valpolicella and Amarone della Valpolicella is quite unique, and includes two main varieties Corvina and Corvinone, and other minor varieties. To a very large extent all these grapes are only grown in the province of Verona. One of the main characteristics of Valpolicella is the use of grapes that are submitted to post-harvest withering. The aim of this study was therefore to evaluate the evolution of the free and glycosidically-bound volatile compounds in Corvina and Corvinone grapes under real production conditions.

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.

Peptidomics in the wine industry: literature perspectives on functional importance and analytical methods

Winemaking is a globally significant industry in the field of food technology (218 mhL of wine estimated for 2024 harvest) [1], which activity produces tons of by-products annually, including pomace (pulp, stems, seeds, skins), lees, organic acids, CO2, and water [2].

Decline of rootstock-mediated physiological responses in Tempranillo grapevines by prolonged extreme conditions

Agriculture faces many global warming challenges especially in the Mediterranean region. Many strategies have been proposed in viticulture to manage global warming. Rootstocks are among them since they may affect water uptake and the scion’s performance.
The study conducted in La Rioja, Spain, aimed to investigate the impact of different rootstocks (1103P and 161-49C) on the performance of the Tempranillo grapevine scion over a three-day cycles under drought and extreme conditions, specifically during a heatwave in July 2022, with maximum air temperatures up to 40ºC and average daily temperatures of 29.1ºC.

Grapevine genotypes with potential for reducing the carbon footprint in the atmosphere and cultivation in a biological system

The concentration of CO2 in the atmosphere is increasing from year to year. Taking into account the calculations of the greenhouse gas inventory, it was found that approximately 70% of CO2 in the atmosphere is absorbed by vegetation (forests, agricultural land, etc.).