Diurnal changes in volcanic plume chemistry observed by lunar and solar occultation spectroscopy

We report the first spectroscopic measurements of volcanic gas emissions by lunar occultation. The experiment was carried out at Masaya volcano, Nicaragua in 1998 using a portable Fourier transform infrared spectrometer. Both SO2 and HCl column concentrations were determined to yield a SO2/HCl molar...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Burton, M R, Oppenheimer, C, Horrocks, L A, Francis, P W
Format: Article in Journal/Newspaper
Language:English
Published: 2001
Subjects:
infrared-spectroscopy
remote measurements
ftir-spectroscopy
masaya-volcano
light-source
polar night
gas
temperature
nicaragua
moon
Online Access:https://research.manchester.ac.uk/en/publications/05408520-9a20-482d-820f-4b61113944a5
https://doi.org/Doi 10.1029/2000gl008499
http://onlinelibrary.wiley.com/store/10.1029/2000GL008499/asset/grl13593.pdf?v=1&t=idq1xxn9&s=a5e8349f64429d93b741d11cffa7f9a92c9a87a1
Description
Summary:We report the first spectroscopic measurements of volcanic gas emissions by lunar occultation. The experiment was carried out at Masaya volcano, Nicaragua in 1998 using a portable Fourier transform infrared spectrometer. Both SO2 and HCl column concentrations were determined to yield a SO2/HCl molar ratio of 2.2 +/- 0.28 (+/-1 sigma). This is significantly greater than the equivalent ratio of 1.6 +/- 0.02 (+/-1 sigma) derived from solar occultation measurements of the volcanic plume. We propose that the cause of the nocturnal increase in SO2/HCl ratio is dissolution of HCl into volcanic water droplets within the plume. This arises because the low saturated vapour pressure of water by night results in strong condensation of plume water vapour whereas by day only negligible plume water vapour condenses.

Similar Items