T94 Effects of Volcanic Eruptions on the Atmosphere and Climate (Posters)
PARTICLES IN TROPOSPHERIC VOLCANIC PLUMES: SIZE, COMPOSITION AND POTENTIAL ENVIRONMENTAL IMPACT
Paper number: T94-1
Program: Technical Sessions
Time: 1:30 PM – 4:30 PM
Authors
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Tamsin A. MatherUniv of Cambridge, Cambridge, N/A
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Andrew G. AllenUniv of Birmingham, Birmingham, N/A
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Clive OppenheimerUniv of Cambridge, Cambridge, N/A
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Andrew J.S. McGonigleUniv of Cambridge, Cambridge, N/A
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Peter BaxterUniv of Cambridge, Cambridge, N/A
Abstract
We present the first application of a multi-stage impactor to study volcanic particle emissions to the troposphere from Masaya volcano, Nicaragua. Concentrations of soluble cations and anions were determined in 12 size bins. The near-source size distributions showed major modes at 0.5 micron (sulfate, hydrogen and ammonium ions); 0.2 and 5.0 micron (chloride) and 2.0-5.0 micron (fluoride). Potassium and sodium ion distribution mirrored the sulfate size-resolved concentrations closely, suggesting that these were transported primarily as potassium sulfate and sodium sulfate in acidic solution, while magnesium and calcium ions peaked in size populations both less than, and greater than 1 micron. The estimated flux of volcanic sulfate leaving the crater was 0.07 kg per second. Effects of relative humidity were studied by comparing daytime (transparent plume) and nighttime (condensed plume) results. Enhanced particle growth rates were observed in the nocturnal plume as well as preferential scavenging of soluble gases, such as hydrogen chloride, by condensed water. Neutralization of the acidic aerosol by background ammonia was observed at the crater rim and to a greater extent 15 km downwind.
We discuss the implications of these results for the understanding of the chemistry of tropospheric volcanic plumes, and their potential environmental impact.