Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5537
AuthorsSpampinato, Letizia* 
Salerno, G.G.* 
Martin, R.S.* 
Sawyer, G.M.* 
Ramírez, C.* 
Ilyinskaya, E.* 
Oppenheimer, C.* 
TitleDegassing pathways through the shallow magmatic-hydrothermal system of Poás
Issue DateDec-2009
URIhttp://hdl.handle.net/2122/5537
KeywordsThermal imagery, SO2 flux traverses, FTIR measurements, Particle composition,
Poás volcano
Subject Classification03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systems 
AbstractWe report results from a multidisciplinary campaign carried out at Poás crater-lake (Costa Rica) on 17-18 March 2009. Thermal imagery of fumaroles on the north side of the dome and the lake surface revealed mean apparent temperatures of 25-40°C (maximum of 80°C), and 30-35°C (maximum of 48°C), respectively. Mean radiative heat output of the lake, uncorrected for downwelling flux, was estimated as ~230 MW. The mean SO2 flux emitted by the crater measured by walking-traverses was 76 tonnes day-1, with approximately equal contributions from both the dome and the lake and fumarole plumes. Gas measurements by active open-path FTIR spectroscopy indicated molar ratios of H2O/SO2 = 151 and CO2/SO2 = 1.56. HCl and HF were not detected in measured spectra but based on the detection limits of these species, we calculate SO2/HCl > 40, and SO2/HF > 200. Particles were sampled from the plume by air filtration. The filters were analysed using ion chromatography, which revealed an abundance of K+ and SO42-, with smaller amounts of Ca2+, Mg2+ and Cl-. We discuss here the implications of the results for degassing pathways through the shallow magmatic-hydrothermal system.
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