F
Francesco Frondini
Researcher at University of Perugia
Publications - 64
Citations - 3674
Francesco Frondini is an academic researcher from University of Perugia. The author has contributed to research in topics: Geothermal gradient & Groundwater. The author has an hindex of 26, co-authored 56 publications receiving 3186 citations. Previous affiliations of Francesco Frondini include Istituto Nazionale di Fisica Nucleare.
Papers
More filters
Journal ArticleDOI
Carbon dioxide Earth degassing and seismogenesis in central and southern Italy
Giovanni Chiodini,Carlo Cardellini,Alessandro Amato,Enzo Boschi,Stefano Caliro,Francesco Frondini,Guido Ventura +6 more
TL;DR: In this paper, the authors present a regional map of CO2 Earth degassing from a large area (most of central and south Italy) derived from the carbon of deep provenance dissolved in the main springs of the region.
Journal ArticleDOI
CO2 Degassing and Energy Release at Solfatara Volcano, Campi Flegrei, Italy
Giovanni Chiodini,Francesco Frondini,Carlo Cardellini,Domenico Granieri,Luigi Marini,Guido Ventura +5 more
TL;DR: In this article, the Solfatara volcano, 1 km far from Pozzuoli, releases 1500 t d−1 of hydrothermal CO2 through soil diffuse degassing from a relatively small area (0.5 km2).
Journal ArticleDOI
Application of stochastic simulation to CO2 flux from soil: Mapping and quantification of gas release
TL;DR: In this paper, conditional sequential Gaussian simulations (sGs) have been applied for the first time to the study of soil diffuse degassing from different volcanic and nonvolcanic systems.
Journal ArticleDOI
Rate of diffuse carbon dioxide Earth degassing estimated from carbon balance of regional aquifers : The case of central Apennine, Italy
TL;DR: In this paper, the authors estimate that 6.5×1010 mol yr−1 of inorganic carbon are dissolved in the studied aquifers and approximately 23% of this amount derives from biological sources active during the infiltration of the recharge waters, 36% comes from carbonate dissolution, while 41% is representative of deep carbon sources characterized by a common isotopic signature.
Journal ArticleDOI
Diffuse emission of CO 2 from the Fossa crater, Vulcano Island (Italy)
TL;DR: In this article, a comparison of the φCO2 maps with the soil temperature distribution, derived from both direct measurements and airborne infrared images, indicates the occurrence of extensive condensation of fumarolic steam within the upper part of the Fossa cone, whose total amount is comparable to the rainfall budget.