Articles | Volume 16, issue 6
https://doi.org/10.5194/se-16-551-2025
https://doi.org/10.5194/se-16-551-2025
Research article
 | 
30 Jun 2025
Research article |  | 30 Jun 2025

Time changes during the last 40 years in the Solfatara magmatic–hydrothermal system (Campi Flegrei, Italy): new conceptual model and future scenarios

Luigi Marini, Claudia Principe, and Matteo Lelli

Viewed

Total article views: 1,383 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
766 322 295 1,383 51 42 45
  • HTML: 766
  • PDF: 322
  • XML: 295
  • Total: 1,383
  • Supplement: 51
  • BibTeX: 42
  • EndNote: 45
Views and downloads (calculated since 22 May 2024)
Cumulative views and downloads (calculated since 22 May 2024)

Viewed (geographical distribution)

Total article views: 1,383 (including HTML, PDF, and XML) Thereof 1,383 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Jul 2025
Download
Short summary
We revised the conceptual model of the Solfatara magmatic–hydrothermal system and used new geothermometers and geobarometers, specifically calibrated for the Solfatara fluids, to monitor temperature, T, and total fluid pressure, P, in three distinct reservoirs at different depths, over ~40 years. The T and P changes in the intermediate reservoir (at 2.7–4 km depth) are of utmost interest because its pressurization–depressurization acts as the “engine” of bradyseism currently affecting the area.
Share