Hydrogen emissions from Erebus volcano, Antarctica

The continuous measurement of molecular hydrogen (H2) emissions from passively degassing volcanoes has recently been made possible using a new generation of low-cost electrochemical sensors. We have used such sensors to measure H2, along with SO2, H2O and CO2, in the gas and aerosol plume emitted fr...

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Bibliographic Details
Published in:Bulletin of Volcanology
Main Authors: Moussallam, Y., Oppenheimer, C., Aiuppa, A., Giudice, G., Moussallam, M., Kyle, P.
Other Authors: Moussallam, Y.; Cambridge Univ, Oppenheimer, C.; Cambridge Univ, Aiuppa, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia, Giudice, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia, Moussallam, M.; Institut Telecom-Telecom ParisTech, Kyle, P.; Univ New Mexico, Cambridge Univ, #PLACEHOLDER_PARENT_METADATA_VALUE#, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia, Institut Telecom-Telecom ParisTech, Univ New Mexico
Format: Article in Journal/Newspaper
Language:English
Published: Springer Berlin Heidelberg 2012
Subjects:
Erebus volcano
Hydrogen
Lava lake
Magma redox conditions
Volcanic degassing
04. Solid Earth::04.08. Volcanology::04.08.01. Gases
Lava Lake
Antarc*
Antarctica
Online Access:http://hdl.handle.net/2122/8932
https://doi.org/10.1007/s00445-012-0649-2
Description
Summary:The continuous measurement of molecular hydrogen (H2) emissions from passively degassing volcanoes has recently been made possible using a new generation of low-cost electrochemical sensors. We have used such sensors to measure H2, along with SO2, H2O and CO2, in the gas and aerosol plume emitted from the phonolite lava lake at Erebus volcano, Antarctica. The measurements were made at the crater rim between December 2010 and January 2011. Combined with measurements of the long-term SO2 emission rate for Erebus, they indicate a characteristic H2 flux of 0. 03 kg s-1 (2. 8 Mg day-1). The observed H2 content in the plume is consistent with previous estimates of redox conditions in the lava lake inferred from mineral compositions and the observed CO2/CO ratio in the gas plume (~0. 9 log units below the quartz-fayalite-magnetite buffer). These measurements suggest that H2 does not combust at the surface of the lake, and that H2 is kinetically inert in the gas/aerosol plume, retaining the signature of the high-temperature chemical equilibrium reached in the lava lake. We also observe a cyclical variation in the H2/SO2 ratio with a period of ~10 min. These cycles correspond to oscillatory patterns of surface motion of the lava lake that have been interpreted as signs of a pulsatory magma supply at the top of the magmatic conduit. Published 2109 – 2120 5V. Sorveglianza vulcanica ed emergenze JCR Journal restricted

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