Gas Monitoring of Volcanic-Hydrothermal Plumes in a Tropical Environment: The Case of La Soufriere de Guadeloupe Unrest Volcano (Lesser Antilles)

Fumarolic gas survey of dormant volcanoes in hydrothermal activity is crucial to detect compositional and mass flux changes in gas emissions that are potential precursors of violent phreatic or even magmatic eruptions. Here we report on new data for the chemical compositions (CO2, H2S, SO2) and fluxes of fumarolic gas emissions (97-104 degrees C) from La Soufriere volcano in Guadeloupe (Lesser Antilles) obtained from both mobile MultiGas measurements and permanent MultiGas survey. This paper covers the period 2016-2020, encompassing a period of enhanced hydrothermal unrest including an abrupt seismic energy release (M 4.1) on April 27, 2018. Our dataset reveals fumarolic CO2/H2S and SO2/H2S gas trends correlated to the evolution of surface activity and to other geochemical and geophysical parameters. We demonstrate that, even under tropical conditions (high humidity and rainfall), MultiGas surveys of low-T fumarolic emissions permit to distinguish deeply sourced signals of volcanic unrest from secondary changes in degassing due to shallow forcing processes such as water-gas-rock interactions in the hydrothermal system and meteorological effects.

Automated summary

Fumarolic gas survey is crucial for detecting potential precursors of violent volcanic eruptions, and the data analysis in this study shows that the compositions and fluxes of fumarolic gas emissions are correlated with the evolution of volcanic activity and other parameters. The study also demonstrates that even under tropical conditions with high humidity and rainfall, multi-gas surveys can distinguish signals of volcanic unrest from secondary changes in degassing.