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 |
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Hauptverfasser: | , , , , , , , , , , , , , |
Format: | Artikel |
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. |
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ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.261.5125.1136 |