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Particle chemistry impactor experimentPolar stratospheric cloud (PSC) particles are collected on impactors and studied with regard to physical and chemical properties to help explain the importance of heterogeneous chemical reactions for stratospheric ozone depletion. The nitric, hydrochloric, and sulfuric acid content of stratospheric aerosol particles collected at 18 km altitude was determined. It is suggested that nitric acid is a component of polar stratospheric clouds. This is important for two reasons: (1) it proves that chlorine activation takes place at the surface of PSC particles by converting chemically inert chlorine nitrate to chlorine radicals that can react with ozone; and (2) if the PSC particles are large enough to settle out from the stratosphere, the possibility of nitric acid removal can result in the denitrification of the stratosphere.
Document ID
19920005299
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Pueschel, R. F.
(San Jose State Univ. CA., United States)
Snetsinger, K. G.
(NASA Ames Research Center Moffett Field, CA, United States)
Ferry, G. V.
(NASA Ames Research Center Moffett Field, CA, United States)
Goodman, J. K.
(NASA Ames Research Center Moffett Field, CA, United States)
Verma, S.
(TMA/Norcal Richmond, CA., United States)
Date Acquired
September 6, 2013
Publication Date
January 1, 1990
Publication Information
Publication: NASA, Washington, NASA Upper Atmosphere Research Program: Research Summaries 1988-1989
Subject Category
Geophysics
Accession Number
92N14517
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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