EGU26-10350, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-10350
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 16:15–18:00 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall X1, X1.163
High-Resolution Continuous Helium Measurement: A New Frontier in Volcanic and Seismic Monitoring Technology.
Fabio Vita1, Salvatore inguaggiato1, Andres Diaz2, Josef Grenz2, Devrim Ay2, Giovanni Schiera1, Giuseppe Passafiume1, and Lorenzo Calderone1
Fabio Vita et al.
  • 1INGV sez. Palermo, Vulcani, Palermo, Italy (fabio.vita@ingv.it)
  • 2INFICON GmbH Bonner Str. 498 50968 Köln Germany

The measurement of geochemical parameters such as He and CO2 concentrations are important and useful for the study of characterization of volcanic systems and seismically active areas. Furthermore, the He/CO2 ratio gives useful information on the depth of the outgassing origin. Finally, extensive parameters such as He and CO2 flux are even more binding in the interpretation and modeling of these systems in question.

In an ambitious move to volcanic risk mitigation, INFICON GmbH—a global leader in measurement and sensor technology—has partnered with premier scientific institutions (INGV_Italy) to monitor active volcanic centers on Italy’s Vulcano and Stromboli islands.

The research focuses on the characterization of natural volcanic emissions at Stromboli and Vulcano (Aeolian Archipelago, Italy), where an advanced geochemical monitoring network for deep-seated fluids is currently operational. A key development in this study involves the deployment of a high-resolution instrument for the continuous measurement of helium (He) concentrations. This device was strategically located with an existing station monitoring soil CO2 flux to investigate the temporal correlation between different volatile species. The 'He-Man' sensor is a cutting-edge helium detector designed for field deployment. It employs a selective helium-permeable membrane to isolate the analyte from the atmospheric matrix, followed by a Penning ionization process to quantify the gas. This setup allows for the detection of trace levels of helium, providing a high-fidelity proxy for the arrival of primitive, mantle-derived fluids within the volcanic plumbing system.

Two 'He-Man' instruments were successfully deployed across the Aeolian Archipelago to monitor high-frequency helium variations. The first unit was installed at Vulcano Island, positioned in a target area characterized by anomalous diffuse soil degassing. The second unit was deployed on Stromboli Island, integrated within a thermal well monitoring system. In the latter configuration, the sensor is coupled with a specialized sampling interface designed for the real-time analysis of dissolved gases in the hydrothermal aquifer. These dual installations enable a comparative study of helium behavior in both sub-aerial and sub-aqueous volcanic environments.

Soils anomalous degassing:

By coupling the 'He-Man' instrument with a high-precision infrared CO2 detector, we are able to determine the He/CO2 concentration ratio within a sub-surface probe (sampling pipe) installed at the Palizzi site. This monitoring point is strategically located adjacent to the Palizzi station, which provides continuous measurements of diffuse CO2 soil fluxes. Utilizing this integrated setup, the helium soil flux (JHe) is indirectly quantified by scaling the measured He/CO2 ratio against the absolute CO2 flux (JCO2) according to the relation: JHe = ([He]/[CO2])*J(CO2)

 

Dissolved CO2 in natural waters:

By integrating this helium concentration sensor with an automated system for monitoring dissolved CO2 in a thermal well at Stromboli, we have successfully characterized the He/CO2 ratio within the hydrothermal environment. This setup targets the specific aquifer situated between the degassing magma body and the anomalous diffuse degassing areas of Scari. This integrated monitoring approach provides critical insights into the geochemical evolution of fluids as they migrate from the magmatic source through the island's groundwater system toward the surface.

 

How to cite: Vita, F., inguaggiato, S., Diaz, A., Grenz, J., Ay, D., Schiera, G., Passafiume, G., and Calderone, L.: High-Resolution Continuous Helium Measurement: A New Frontier in Volcanic and Seismic Monitoring Technology., EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-10350, https://doi.org/10.5194/egusphere-egu26-10350, 2026.