Changes in soil water availability in vineyards can be traced by the carbon and nitrogen isotope composition of dried wines

Jorge E Spangenberg; Vivian Zufferey

doi:10.1016/j.scitotenv.2018.04.078

Changes in soil water availability in vineyards can be traced by the carbon and nitrogen isotope composition of dried wines

Sci Total Environ. 2018 Sep 1:635:178-187. doi: 10.1016/j.scitotenv.2018.04.078. Epub 2018 Apr 13.

Authors

Jorge E Spangenberg¹, Vivian Zufferey²

Affiliations

¹ Institute of Earth Surface Dynamics (IDYST), University of Lausanne, CH-1015 Lausanne, Switzerland. Electronic address: Jorge.Spangenberg@unil.ch.
² Institute of Plant Production Sciences (IPV), Agroscope, CH-1009 Pully, Switzerland.

PMID: 29660721
DOI: 10.1016/j.scitotenv.2018.04.078

Abstract

The grapevine is one of the most important edible fruit plants cultivated worldwide, and it is highly sensitive to changes in the soil water content. We studied the total carbon and nitrogen contents and stable isotope compositions (C/N_WSR, δ¹³C_WSR and δ¹⁵N_WSR values) of the solid residues obtained by freeze-drying wines produced from two white grapevine cultivars (Vitis vinifera L. cv Chasselas and Petite Arvine) field grown under different soil water regimes while maintaining other climatic and ecopedological conditions identical. These experiments simulated the more frequent and extended climate change-induced periods of soil water shortage. The wines were from the 2009-2014 vintages, produced using the same vinification procedure. The plant water status, reflecting soil water availability, was assessed by the predawn leaf water potential (Ψ_pd), monitored in the field during the growing seasons. For both wine varieties, the δ¹³C_WSR values are highly correlated with Ψ_pd values and record the soil water availability set by soil water holding capacity, rainfall and irrigation water supply. These relationships were the same as those observed for the carbon isotope composition of fruit sugars (i.e., must sugars) and plant water status. In Chasselas wines, the nitrogen content and δ¹⁵N_WSR values decreased with soil water deficit, indicating control of the flux of soil-water soluble nutrients into plants by soil water availability. Such a correlation was not found for Petite Arvine, probably due to different N-metabolism processes in this genetically atypical cultivar. The results presented in this study confirm and generalize what was previously found for red wine (Pinot noir); the carbon isotope composition of wine solid residues is a reliable indicator of the soil and the plant water status and thus can be used to trace back local climatic conditions in the vineyard's region. In most wines (except Petite Arvine) the C/N_WSR and δ¹⁵N_WSR values are indicators of the origin of the nitrogen supplied to the plant's fruit (grape) that can be used to assess the N dynamics in the soil-water-plant system.

Keywords: Climate change; Plant water status; Soil-water status; Vineyards; Wine solid residues; δ(13)C; δ(15)N.