G
Giovanni Chiodini
Researcher at National Institute of Geophysics and Volcanology
Publications - 218
Citations - 11892
Giovanni Chiodini is an academic researcher from National Institute of Geophysics and Volcanology. The author has contributed to research in topics: Volcano & Caldera. The author has an hindex of 61, co-authored 196 publications receiving 10123 citations. Previous affiliations of Giovanni Chiodini include University of Perugia.
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Magmas near the critical degassing pressure drive volcanic unrest towards a critical state
Giovanni Chiodini,Antonio Paonita,Alessandro Aiuppa,Alessandro Aiuppa,Antonio Costa,Stefano Caliro,Prospero De Martino,Valerio Acocella,Jean Vandemeulebrouck,Jean Vandemeulebrouck +9 more
TL;DR: It is proposed that magma could be approaching the CDP at Campi Flegrei, a volcano in the metropolitan area of Naples, one of the most densely inhabited areas in the world, and where accelerating deformation and heating are currently being observed.
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Carbon isotopic composition of soil CO2 efflux, a powerful method to discriminate different sources feeding soil CO2 degassing in volcanic-hydrothermal areas
Giovanni Chiodini,Stefano Caliro,Carlo Cardellini,Rosario Avino,Domenico Granieri,Anja Schmidt +5 more
TL;DR: In this article, a new method combining measurements of soil CO 2 flux and determinations of the carbon isotopic composition of CO 2 efflux was developed in order to qualitatively and quantitatively characterise the CO 2 source feeding the soil CO2 diffuse degassing.
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Early signals of new volcanic unrest at Campi Flegrei caldera? Insights from geochemical data and physical simulations
TL;DR: In this article, a physical model is used to derive a quantitative estimate of the evolution in time of magmatic gases that enter a hydrothermal system of an active volcano, which can be used to predict magmatic evolution and eruptive activity at volcanoes.
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Carbon dioxide degassing from the Albani Hills volcanic region, Central Italy
TL;DR: The Albani Hills are affected by strong CO2 degassing processes and the amount of CO2 which rises from the depths and subsequently dissolves into shallow groundwater has been estimated to be more than 4.2×109 mol year−1 as discussed by the authors.
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Dynamics of carbon dioxide emission at Mammoth Mountain, California
TL;DR: In this article, a detailed study of the degassing process at Mammoth Mountain has been conducted and the authors found that high coherence between variations in CO2 efflux and variations in atmospheric pressure and wind speed imply that meteorological parameters account for much, if not all, of the variability in CO 2 efflux rates.