Fig. 12From: Variation of volcanic gas composition during the eruptive period in 2014–2015 at Nakadake crater, Aso volcano, JapanSchematic diagrams showing the mechanism of the composition variation observed during the eruptive period. a On 12 January 2015, gases discharge during intensive ash eruptions are derived from a wide range of pressure from 20 to 0.2 MPa, causing a rapid and large variation in gas composition, in particular of CO2/SO2 and SO2/H2S ratios. The fumarolic gases likely be derived from gases separated at a high pressure. b On 17 March, the rapid and large variation of gas composition indicates bubble ascent from a wide range of pressure. But decrease in the composition range suggests decrease in the maximum degassing pressure and decrease in contribution of bubbles formed at a high pressure. c On May 2015, the stable gas composition implies degassing of a well-mixed magma under a stable conditionBack to article page