Heterogeneous Reaction Probabilities, Solubilities, and the Physical State of Cold Volcanic Aerosols

On 19 January 1992, heterogeneous loss of HNO$_3$, ClNO$_3$, and HCl was observed in part of the Mount Pinatubo volcanic cloud that had cooled as a result of forced ascent. Portions of the volcanic cloud froze near 191 kelvin. The reaction probability of ClNO$_3$ and the solubility of HNO$_3$ were c...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1993-08, Vol.261 (5125), p.1136-1140
Hauptverfasser: Toon, O., Browell, E., Gary, B., Lait, L., Livingston, J., Newman, P., Pueschel, R., Russell, P., Schoeberl, M., Toon, G., Traub, W., Valero, F. P. J., Selkirk, H., Jordan, J.
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Sprache:eng
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Zusammenfassung:On 19 January 1992, heterogeneous loss of HNO$_3$, ClNO$_3$, and HCl was observed in part of the Mount Pinatubo volcanic cloud that had cooled as a result of forced ascent. Portions of the volcanic cloud froze near 191 kelvin. The reaction probability of ClNO$_3$ and the solubility of HNO$_3$ were close to laboratory measurements on liquid sulfuric acid. The magnitude of the observed loss of HCl suggests that it underwent a heterogeneous reaction. Such reactions could lead to substantial loss of HCl on background sulfuric acid particles and so be important for polar ozone loss.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.261.5125.1136