Journal Article10.1007/S00445-017-1105-0
Volcanic gas composition changes during the gradual decrease of the gigantic degassing activity of Miyakejima volcano, Japan, 2000-2015
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TL;DR: The composition of volcanic gases discharged from Miyakejima volcano has been monitored during intensive degassing activity that began after the eruption in 2000 and quickly decreased to 5kt/day by 2003.
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Abstract: The composition of volcanic gases discharged from Miyakejima volcano has been monitored during the intensive degassing activity that began after the eruption in 2000. During the 15 years from 2000 to 2015, Miyakejima volcano discharged 25.5 Mt of SO2, which required degassing of 3 km3 of basaltic magma. The SO2 emission rate peaked at 50 kt/day at the end of 2000 and quickly decreased to 5 kt/day by 2003. During the early degassing period, the volcanic gas composition was constant with the CO2/SO2 = 0.8 (mol ratio), H2O/SO2 = 35, HCl/SO2 = 0.08, and SO2/H2S = 15. The SO2 emission rate decreased gradually to 0.5 kt/day by 2012, and the gas composition also changed gradually to CO2/SO2 = 1.5, H2O/SO2 = 150, HCl/SO2 = 0.15, and SO2/H2S = 6. The compositional changes are not likely caused by changes in degassing pressure or volatile heterogeneity of a magma chamber but are likely attributed to an increase of hydrothermal scrubbing caused by large decrease of the volcanic gas emission rate, suggesting a supply of gases with constant composition during the 15 years. The intensive degassing was modeled based on degassing of a convecting magma conduit. The gradual SO2 emission rate that decrease without changes in volcanic gas composition is attributed to a reduction of diameter of the convecting magma conduit.
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Citations
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Magmatic Gas Composition Reveals the Source Depth of Slug-Driven Strombolian Explosive Activity
J. G. Wright,Michael J. Natan,Frederick M. MacDonnell,D. M. Ralston,M. Wilhelm +4 more
- 01 Jan 2007
TL;DR: In this article, the authors propose that access to coordination numbers greater than 2 promotes protolytic cleavage of the Hg-C bond and the liberation of RH at elevated temperatures.
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Equilibrium temperature and redox state of volcanic gas at Unzen volcano, Japan
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Conduit magma convection of a rhyolitic magma: Constraints from cosmic-ray muon radiography of Iwodake, Satsuma-Iwojima volcano, Japan
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