Looking into the volcano with a Mid-IR DFB diode laser and Cavity Enhanced Absorption Spectroscopy
Résumé
We report on the first application of extended–wavelength DFB diode lasers to Cavity–Enhanced Absorption Spectroscopy in-situ trace measurements on geothermal gases. The emission from the most active fumarole at the Solfatara volcano near Naples (Italy) was probed for the presence of CO and CH4. After passing through a gas dryer and cooler, the volcanic gas flow (98% CO2) was analysed in real time for the concentration of these species, whose relatively strong absorption lines could be monitored simultaneously by a single Distributed Feed–Back (DFB) GaSb–based diode laser emitting around 2.33 μm (4300 cm−1) at room temperature. The concentrations were found to be about 3 ppm and 75 ppm, respectively, while actual detection limits for these molecules are around 1 ppb. We discuss the possibility of detecting other species of interest for volcanic emission monitoring