Terroir 2020 banner
IVES 9 IVES Conference Series 9 Effects of soil characteristics on manganese transfer from soil to vine and wine

Effects of soil characteristics on manganese transfer from soil to vine and wine

Abstract

Aim: In recent times the export of Beaujolais wines has been jeopardised due to a limit of manganese content (Mn) in wine implemented by China (2 mg/L), related to suspicions of potassium permanganate fraud. Nevertheless, soil Mn content may be high in some soil types in Beaujolais. The aim of this study was to improve knowledge of manganese transfer from soil to vine and wine because data on this subject is scarce.

Methods and Results: Recent pedologic mapping of Beaujolais vineyards has enabled a Mn monitoring network to be set up in order to study Mn transfer from soil to vine and wine. Three soil types were considered. Two of the soils can be very high in EDTA Mn: soils from clays with cherts (soil type 7) and former piedmont deposits with leached soils (soil type 8). The third soil, though low in Mn, is the most important and symbolic of Beaujolais: granitic soil. Fifteen plots of Gamay were monitored during 3 years (2015-2017). Besides soil analysis made from pedologic pits, Mn content of petiole, must and wine (red standard wine-making of 40 kg grapes) were determined, as well as grape yield and biomass (pruning weight). Results show that Mn in petioles is better correlated with Mn in wine than Mn in must. Mn content of wine is little in relation with EDTA Mn in soil. It increases when soil pH or cation exchange capacity decreases.

Conclusions: 

This study has shown that Mn concentration in wine can be naturally very high (maximum of 14.6 g/L in this study). Soils with low cation exchange capacity and/or low pH, i.e. soil types 1 and 8, resulted in higher Mn content in wine. Low cation exchange capacity does not allow a great Mn fixation on clay-humic complex and low pH soil solubilizes metal generally and Mn in particular, so it can be taken up by the vine. Mn petiole content is a very good indicator of Mn content in wine. Maceration in red wine-making is also an element to take into consideration.

Significance and Impact of the Study: Mn content in Beaujolais wine can be very high because of soil type, rather than fraud. It is important to highlight this for wine exportations. Mn content in wine can be reduced by correcting the soil pH.

DOI:

Publication date: March 17, 2021

Issue: Terroir 2020

Type: Video

Authors

Jean-Yves Cahurel1, Pierre Martini1*, B. Chatelet2, I. Letessier3

1Institut Français de la Vigne et du Vin, 210 boulevard Vermorel, CS 60320, 69661 Villefranche-sur-Saône, France
2Sicarex Beaujolais, 210 boulevard Vermorel, CS 60320, 69661 Villefranche-sur-Saône Cedex, France
3Sigales, 453 route de Chamrousse, 38410 St Martin d’Uriage, France

Contact the author

Keywords

Manganese, terroir, soil, Beaujolais, vine, wine

Tags

IVES Conference Series | Terroir 2020

Citation

Related articles…

AOC Saint-Romain, Hautes-Côtes-de-Beaune, Burgundy: analysis of a “terroir”

The aim of this study is to provide an overview of the terroir of Saint-Romain, Burgundy, based on three main information sources: official data relating to vines (CVI), soil cartography and a survey of winegrowers’ practices.

Effect of rising atmospheric CO2 levels on grapevine yield and composition by the middle of the 21st century: what can we learn from the VineyardFACE?

Atmospheric CO2 levels have been rising continuously since the industrial revolution, affecting crop physiology, yield and quality of harvest products, and grapevine is no exception [1]. Most of previously reported studies used potted plants in controlled environments, and explored grapevine response to relatively high CO2 levels, 700 ppm or more. The vineyardFACE, established in Geisenheim in 2012, uses a free air carbon dioxide enrichment (FACE) system to simulate a moderate (ambient +20%) increase in atmospheric CO2 in a vineyard planted with cvs. Cabernet-Sauvignon and Riesling grafted on rootstock 161-49 Couderc and SO4, respectively.

Valorisation agroviticole de l’effet terroir par l’enherbement des sols

The studies developed by INRA and UV, in Angers, concern wine-growing areas and their optimized management, both from an agro-viticultural and oenological point of view. Previous work (Morlat, 1989) made it possible to give a scientific dimension to the concept of viticultural terroir and demonstrated the considerable influence of this production factor on the quality and typicity of wines (Asselin et al, 1992 ) . A methodology for the integrated characterization of terroirs, based on the “Basic Terroir Natural Unit” (considered as the smallest spatial unit of territory usable in practice, and in which the response of the vine is homogeneous), has been development (Riou et al , 1995).

Intra-block variations of vine water status in time and space

Vine water status was measured on 96 plots of three vines inside a vineyard block of 0.28 ha during three years: 2003, 2004 and 2005. Three physiological indicators were implemented: stem water potential, carbon isotope discrimination measured on grape sugars at ripeness (δ13C) and canopy temperature measured by high resolution remote sensing. For stem water potential, measurements were taken on every single vine of each plot.

The environmental footprint of selected vineyard management practices: A case study from Logroño (La Rioja) Spain

Viticulture is globally important for socioeconomic and environmental reasons. The EU is globally leading grape and wine production, and Spain is among the top grape and wine producers. As climate change affects viticulture, mitigation and adaptation are crucial for protecting grape production. In this research work, data on viticultural management practices such as soil cultivation, irrigation, energy, machinery, plant protection and the use of fertilizers from vineyards located in Logroño (La Rioja) have been obtained.