Fig. 9From: Behavior of magmatic components in fumarolic gases related to the 2018 phreatic eruption at Ebinokogen Ioyama volcano, Kirishima Volcanic Group, Kyushu, Japana δD and δ18O of H2O in fumarolic gas with the calculated vapor phase (Vp) and liquid phase (Lp). Vp-100 and Vp-160 denote Vp of 100 °C and 160 °C, respectively. Lp-100 and Lp-160 denote Lp at the temperature of 100 °C and 160 °C, respectively. The broken lines annotated as Cd indicate the isotopic ratio of remaining water vapor after partial condensation. V-100, 150 and 200 are the isotopic ratios of water vapor equilibrated with liquid L at 100 °C, 150 °C, and 200 °C, respectively. b Magnified Ar fraction, mF(Ar), and δ18O of H2O in fumarolic gases with Vp-100 and Vp-160. vLW indicates the vapor phase generated from local meteoric water (LW)Back to article page