Jan 12, 2022 | Climate component of terroir (Terroir 2006), IVES Conference Series, Terroir 2006
Between 2002 and 2004 we studied the behaviour of two red grape varieties – Merlot and Cabernet Sauvignon – within the scope of an experimental protocol encompassing 14 plots, 7 of which had not been cultivated, situated in geographically distant locations representing different terroirs of Castilla-La Mancha.
Jan 12, 2022 | Climate component of terroir (Terroir 2006), IVES Conference Series, Terroir 2006
The State Rio Grande do Sul is the main producer of Brazilian fine wines, with four viticultural regions. The objective is the characterization of the viticultural climatic potential of the State (total surface of 281.749 km2). The methodology use the Géoviticulture Multicriteria Climatic Classification System (Géoviticulture MCC System), based on three climatic indices – Dryness Index (DI), Heliotermal Index (HI) and Cool Night Index (CI).
Jan 12, 2022 | Climate component of terroir (Terroir 2006), IVES Conference Series, Terroir 2006
Climate is an important component or determinant of terroir, especially at the regional level. One can define three levels of terroir. These are the macro– or regional scale, which applies over tens of kilometres of the landscape. The second level is the meso- scale, which applies over kilometres or hundreds of meters, at the individual vineyard scale.
Jan 12, 2022 | Application of zoning to increase the value of terroirs (Terroir 2006), IVES Conference Series, Terroir 2006
The aim of this communication is the study of the Ronda and Arriate municipal territories environment in order to define and to establish the main physical factors in relation to vine-growing land use. The vine-growing zoning proposed is based on geopedological and climatic features.
Jan 12, 2022 | Application of zoning to increase the value of terroirs (Terroir 2006), IVES Conference Series, Terroir 2006
The vineyard of Bergerac, a guaranteed vintage, is situated in the mid-Lot valley, which has siliceous terraced rows on its hillsides, and on its bordering plateaux, composed of limestone and clay of the tertiary geological eras.