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Looking into the volcano with a Mid-IR DFB diode laser and Cavity Enhanced Absorption Spectroscopy
Optics Express
|June 17, 2009
Summary
This study demonstrates the first use of extended-wavelength diode lasers for in-situ monitoring of volcanic gases. Carbon monoxide (CO) and methane (CH4) were measured in geothermal emissions with high sensitivity.
Area of Science:
- Geochemistry
- Environmental Science
- Spectroscopy
Background:
- Volcanic emissions contain trace gases crucial for monitoring geological activity.
- Cavity-Enhanced Absorption Spectroscopy (CEAS) offers high sensitivity for gas analysis.
- Extended-wavelength diode lasers enable probing of specific absorption lines.
Purpose of the Study:
- To apply extended-wavelength Distributed Feed-Back (DFB) diode lasers to in-situ trace measurements of geothermal gases.
- To monitor carbon monoxide (CO) and methane (CH4) concentrations in volcanic emissions in real-time.
- To assess the potential for detecting other volcanic gas species.
Main Methods:
- Utilized a GaSb-based DFB diode laser emitting around 2.33 µm (4300 cm⁻¹).
- Employed Cavity-Enhanced Absorption Spectroscopy (CEAS) for trace gas analysis.
- Analyzed volcanic gas from the Solfatara volcano fumarole after drying and cooling.
Main Results:
- Simultaneously monitored CO and CH4 absorption lines using a single DFB laser.
- Measured CO concentration at approximately 3 ppm and CH4 at approximately 75 ppm.
- Achieved detection limits around 1 ppb, highlighting the system's high sensitivity.
Conclusions:
- Extended-wavelength DFB diode lasers are effective for in-situ trace gas monitoring in volcanic environments.
- The developed method allows for real-time analysis of key volcanic gas species.
- Further applications for monitoring other geochemically relevant gases are feasible.
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