Fig. 3From: Constraints on magma storage conditions based on geodetic volume change and erupted magma volume and application to the 2011 and 2018 eruptions at Kirishima Shinmoe-dake volcano, JapanSolubility of H\(_2\)O–CO\(_2\) mixture obtained by Iacono-Marziano et al. (2012) for \(T = 1303\) K and melt compositions of the Shinmoe-dake eruptions (Suzuki et al. 2013), with varying pressureBack to article page