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  5. Real-time quadrupole mass spectrometry of hydrothermal gases from the unstable Pisciarelli fumaroles (Campi Flegrei): Trends, challenges and processes
 
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Real-time quadrupole mass spectrometry of hydrothermal gases from the unstable Pisciarelli fumaroles (Campi Flegrei): Trends, challenges and processes

Author(s)
Fedele, Alessandro  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Pedone, Maria  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Moretti, Roberto  
Wiersberg, Thomas  
Somma, Renato  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Troise, Claudia  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
De Natale, Giuseppe  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Language
English
Obiettivo Specifico
4V. Dinamica dei processi pre-eruttivi
Status
Published
JCR Journal
JCR Journal
Journal
International Journal of Mass Spectrometry  
Issue/vol(year)
/415 (2017)
Pages (printed)
44-54
Date Issued
2017
DOI
10.1016/j.ijms.2017.02.006
URI
https://www.earth-prints.org/handle/2122/12154
Abstract
Volcanic gas sampling and post-collection chemical determination in a laboratory may preclude anyreal-time continuous monitoring of volcanic activity. We describe the development, and show the advan-tages, of a system used for the continuous monitoring of fumarolic gases discharged from the Pisciarellisite (Campi Flegrei, Southern Italy) based on a commercial quadrupole mass spectrometer (QMS-301OmnistarTM). Although numerous technical problems were addressed due to the ephemeral nature ofthe emission point and the harsh environment, we also report measurements of the chemical composi-tion of the major gas species emitted from the fumarole for two different periods (in 2009 and 2012). TheCO2/H2S, H2S/H2, He/CO2and CH4/CO2molar ratios were investigated in order to detect magmatic and/orhydrothermal components in the system, while the N2/O2ratio was adopted to infer other non-volcanicprocesses, such as air contamination and mixing with polluted surface waters. The presented method-ology allows continuous gas sampling and provides the first evidence of short-term gas variations notavailable by direct sampling, which is often impractical and hazardous. Compared to the current tech-niques that are used worldwide for the full characterization of gaseous emissions, i.e. chemical analysis oftraditional soda-filled under-vacuum bottles and MultiGAS surveys (laboratory-based and in situ, respec-tively), QMS-based monitoring is complementary and, in prospect, an alternative. With our method, thegeochemical monitoring benefits of the real-time analysis for high sampling rates that can be made com-parable to the continuous measurements of geophysical networks. This allows a better understandingof hydrothermal features, particularly of chemical fluctuations occurring on the very short-term, whichis fundamental for the evaluation of the evolution of unrest episodes at Campi Flegrei, one of the mosthazardous volcanic areas in the world.
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