Excess degassing drives long-term volcanic unrest at Nevado del Ruiz

Abstract This study combines volcanic gas compositions, SO2 flux and satellite thermal data collected at Nevado del Ruiz between 2018 and 2021. We find the Nevado del Ruiz plume to have exhibited relatively steady, high CO2 compositions (avg. CO2/ST ratios of 5.4 ± 1.9) throughout. Our degassing mod...

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Main Authors: João Lages, Zoraida Chacón, Julian Ramirez, Alessandro Aiuppa, Santiago Arellano, Marcello Bitetto, Julián O. Peña, Diego Coppola, Marco Laiolo, Francesco Massimetti, Lina Castaño, Carlos Laverde, Giancarlo Tamburello, Gaetano Giudice, Cristian Lopez
Format: Article
Language:English
Published: Nature Portfolio 2024-01-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-024-51380-5
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author João Lages
Zoraida Chacón
Julian Ramirez
Alessandro Aiuppa
Santiago Arellano
Marcello Bitetto
Julián O. Peña
Diego Coppola
Marco Laiolo
Francesco Massimetti
Lina Castaño
Carlos Laverde
Giancarlo Tamburello
Gaetano Giudice
Cristian Lopez
author_facet João Lages
Zoraida Chacón
Julian Ramirez
Alessandro Aiuppa
Santiago Arellano
Marcello Bitetto
Julián O. Peña
Diego Coppola
Marco Laiolo
Francesco Massimetti
Lina Castaño
Carlos Laverde
Giancarlo Tamburello
Gaetano Giudice
Cristian Lopez
author_sort João Lages
collection DOAJ
description Abstract This study combines volcanic gas compositions, SO2 flux and satellite thermal data collected at Nevado del Ruiz between 2018 and 2021. We find the Nevado del Ruiz plume to have exhibited relatively steady, high CO2 compositions (avg. CO2/ST ratios of 5.4 ± 1.9) throughout. Our degassing models support that the CO2/ST ratio variability derives from volatile exsolution from andesitic magma stored in the 1–4 km depth range. Separate ascent of CO2-rich gas bubbles through shallow (< 1 km depth), viscous, conduit resident magma causes the observed excess degassing. We infer that degassing of ~ 974 mm3 of shallow (1–4 km) stored magma has sourced the elevated SO2 degassing recorded during 2018–2021 (average flux ~ 1548 t/d). Of this, only < 1 mm3 of magma have been erupted through dome extrusion, highlighting a large imbalance between erupted and degassed magma. Escalating deep CO2 gas flushing, combined with the disruption of passive degassing, through sudden accumulation and pressurization of bubbles due to lithostatic pressure, may accelerate volcanic unrest and eventually lead to a major eruption.
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spelling doaj.art-14bc55ef4027416aa86ca70f13e74dc72024-01-14T12:20:19ZengNature PortfolioScientific Reports2045-23222024-01-0114111310.1038/s41598-024-51380-5Excess degassing drives long-term volcanic unrest at Nevado del RuizJoão Lages0Zoraida Chacón1Julian Ramirez2Alessandro Aiuppa3Santiago Arellano4Marcello Bitetto5Julián O. Peña6Diego Coppola7Marco Laiolo8Francesco Massimetti9Lina Castaño10Carlos Laverde11Giancarlo Tamburello12Gaetano Giudice13Cristian Lopez14Dipartimento DiSTeM, Università Degli Studi Di PalermoServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesDipartimento DiSTeM, Università Degli Studi Di PalermoDepartment of Space, Earth and Environment, Chalmers University of TechnologyDipartimento DiSTeM, Università Degli Studi Di PalermoServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesDipartimento Di Scienze Della Terra, Università Di TorinoDipartimento Di Scienze Della Terra, Università Di TorinoDipartimento Di Scienze Della Terra, Università Di TorinoServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesIstituto Nazionale Di Geofisica E Vulcanologia, Sezione Di BolognaIstituto Nazionale Di Geofisica E Vulcanologia, Osservatorio EtneoServicio Geológico Colombiano, Observatorio Vulcanológico y Sismológico de ManizalesAbstract This study combines volcanic gas compositions, SO2 flux and satellite thermal data collected at Nevado del Ruiz between 2018 and 2021. We find the Nevado del Ruiz plume to have exhibited relatively steady, high CO2 compositions (avg. CO2/ST ratios of 5.4 ± 1.9) throughout. Our degassing models support that the CO2/ST ratio variability derives from volatile exsolution from andesitic magma stored in the 1–4 km depth range. Separate ascent of CO2-rich gas bubbles through shallow (< 1 km depth), viscous, conduit resident magma causes the observed excess degassing. We infer that degassing of ~ 974 mm3 of shallow (1–4 km) stored magma has sourced the elevated SO2 degassing recorded during 2018–2021 (average flux ~ 1548 t/d). Of this, only < 1 mm3 of magma have been erupted through dome extrusion, highlighting a large imbalance between erupted and degassed magma. Escalating deep CO2 gas flushing, combined with the disruption of passive degassing, through sudden accumulation and pressurization of bubbles due to lithostatic pressure, may accelerate volcanic unrest and eventually lead to a major eruption.https://doi.org/10.1038/s41598-024-51380-5
spellingShingle João Lages
Zoraida Chacón
Julian Ramirez
Alessandro Aiuppa
Santiago Arellano
Marcello Bitetto
Julián O. Peña
Diego Coppola
Marco Laiolo
Francesco Massimetti
Lina Castaño
Carlos Laverde
Giancarlo Tamburello
Gaetano Giudice
Cristian Lopez
Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
Scientific Reports
title Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
title_full Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
title_fullStr Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
title_full_unstemmed Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
title_short Excess degassing drives long-term volcanic unrest at Nevado del Ruiz
title_sort excess degassing drives long term volcanic unrest at nevado del ruiz
url https://doi.org/10.1038/s41598-024-51380-5
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