Escalating soil CO 2 degassing correlates with ground uplift and seismicity during the ongoing unrest of Campi Flegrei (2005–2025)

The mechanism driving accelerating unrest at the densely populated Campi Flegrei caldera since 2005 remains debated. Analyzing an unprecedented two-decade geochemical dataset, we show that escalating soil CO 2 fluxes closely tracks caldera uplift, revealing magmatic fluid pressurization at 3- to 4-kilometer depth and heating as the fundamental driver of the unrest. A critical magmatic gas pulse occurred between 2018 and 2022 specifically focused this outgassing beneath the Solfatara crater. Thermodynamic modeling demonstrates that an increasing mass of ascending fluid pressurizes the hydrothermal system, forcing vapor condensation within the upper kilometer. This condensation transfers latent heat to the crust. We calculate that this released thermal energy is an order of magnitude greater than that required for the 1.6-meter uplift since 2005. Ultimately, this fluid pressurization and heating drive accelerating deformation and seismicity; alongside the 2021 emergence of seismic sequences with short inter-event times, it directly signals an escalating phreatic or magmatic eruption risk.

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Publication Details

Journal
Science Advances
Published
2026-10-07
DOI
https://doi.org/10.1126/sciadv.aei8075
Primary Topic
earthquake and tectonic studies
Type
article
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article

Escalating soil CO 2 degassing correlates with ground uplift and seismicity during the ongoing unrest of Campi Flegrei (2005–2025)

Giancarlo Tamburello, Renato Palmieri, Stefano Caliro, Carmine Minopoli et al.
Science Advances
earthquake and tectonic studies
article

Escalating soil CO 2 degassing correlates with ground uplift and seismicity during the ongoing unrest of Campi Flegrei (2005–2025)

Giancarlo Tamburello, Renato Palmieri, Stefano Caliro, Carmine Minopoli, Giulio Bini, Tullio Ricci, Francesco Rufino, Raffaella Silvia Iovine, Carlo Cardellini, Emilio Cuoco, Dmitri Rouwet, Prospero De Martino, Giovanni Chiodini, Rosario Avino, Alessandra Sciarra, Alessandro Santi, Mauro Tieri, Antonio Carandente
article en

Abstract

The mechanism driving accelerating unrest at the densely populated Campi Flegrei caldera since 2005 remains debated. Analyzing an unprecedented two-decade geochemical dataset, we show that escalating soil CO 2 fluxes closely tracks caldera uplift, revealing magmatic fluid pressurization at 3- to 4-kilometer depth and heating as the fundamental driver of the unrest. A critical magmatic gas pulse occurred between 2018 and 2022 specifically focused this outgassing beneath the Solfatara crater. Thermodynamic modeling demonstrates that an increasing mass of ascending fluid pressurizes the hydrothermal system, forcing vapor condensation within the upper kilometer. This condensation transfers latent heat to the crust. We calculate that this released thermal energy is an order of magnitude greater than that required for the 1.6-meter uplift since 2005. Ultimately, this fluid pressurization and heating drive accelerating deformation and seismicity; alongside the 2021 emergence of seismic sequences with short inter-event times, it directly signals an escalating phreatic or magmatic eruption risk.

Science AdvancesVol. 12(41)
University of Campania "Luigi Vanvitelli" (IT), University of Perugia (IT), Istituto Nazionale di Geofisica e Vulcanologia (IT), INGV Sezione di Roma 1 (IT), INGV Sezione di Bologna, INGV Osservatorio Vesuviano
Openalex Percentile: Top 16%
earthquake and tectonic studies
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