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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5537

Authors: Spampinato, Letizia*
Salerno, G.G.*
Martin, R.S.*
Sawyer, G.M.*
Ramírez, C.*
Ilyinskaya, E.*
Oppenheimer, C.*
Title: Degassing pathways through the shallow magmatic-hydrothermal system of Poás
Issue Date: Dec-2009
Keywords: Thermal imagery, SO2 flux traverses, FTIR measurements, Particle composition,
Poás volcano
Abstract: We 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.
Appears in Collections:Conference materials
03.04.06. Hydrothermal systems

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