Abstract − Analytical Sciences, 33(8), 979 (2017).
Stable Isotope Analysis of Hydrogen and Oxygen in a Traditional Japanese Alcoholic Beverage, Sake, from Niigata Prefecture in Japan and Other Countries
Takashi KURIBAYASHI,* Masamichi SUGAWARA,* Keigo SATO,* Yoshihito NABEKURA,* Toshio AOKI,* Naoki KANO,** Toshio JOH,*** and Mitsuoki KANEOKE*
*Niigata Prefectural Sake Research Institute, 2-5932-133 Suido-cho, Chuoh, Niigata, Niigata 951-8121, Japan
**Department of Chemistry and Chemical Engineering, Faculty of Engineering, Niigata University, 8050 Ikarashi 2-Nocho, Nishi, Niigata, Niigata 950-2181, Japan
***Department of Applied Biological Chemistry, Faculty of Agriculture, Niigata University, 8050 Ikarashi 2-Nocho, Nishi, Niigata, Niigata 950-2181, Japan
**Department of Chemistry and Chemical Engineering, Faculty of Engineering, Niigata University, 8050 Ikarashi 2-Nocho, Nishi, Niigata, Niigata 950-2181, Japan
***Department of Applied Biological Chemistry, Faculty of Agriculture, Niigata University, 8050 Ikarashi 2-Nocho, Nishi, Niigata, Niigata 950-2181, Japan
Stable hydrogen and oxygen isotopic compositions (δD and δ18O values, respectively) were analyzed for “sake,” a traditional Japanese alcohol beverage, to assess these values for the identification of its geographic origin. We collected sake (Junmai-shu; made of only rice, water, and koji) and its source water (i.e., brewing water) from breweries in Niigata Prefecture, Japan, and measured the isotopic compositions of water in these samples. The δD and δ18O values for the sake are well correlated with their respective values for the corresponding brewing water (δD; r = 0.92, δ18O; r = 0.80). Furthermore, based on the δD–δ18O cross plot, sake brewed in Niigata Prefecture is distinguishable from that brewed in countries other than Japan. These results imply that this dual isotope (δD and δ18O) analysis is potentially useful in identifying the geographic origin of sake.
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