词条 | Secondary organic aerosol |
释义 |
A secondary organic aerosol (SOA) is a molecule produced via oxidation over several generations of a parent organic molecule.[1] In contrast to primary organic aerosols, which are emitted directly from the biosphere, secondary organic aerosols are formed via homogeneous nucleation through the successive oxidation of gas-phase organic compounds. These gas-phase species exert high vapor pressures, meaning they are volatile and stable in the gas-phase, however, upon oxidation, the increased polarity of the molecules results in a reduction of vapor pressure. After sufficient oxidation, the vapor pressure is sufficiently low that the gas-phase compound partitions into the solid-phase, producing secondary organic matter. SOAs represent a significant proportion of aerosols contained in the troposphere.[1] A common misconception is that the aerosol refers to the solid phase of the compound, where in reality, by definition, it is the combination of the gas- and solid-phases which constitute the aerosol. References1. ^1 {{Cite journal|title = Secondary Organic Aerosol Formation from Low-NOx Photooxidation of Dodecane: Evolution of Multigeneration Gas-Phase Chemistry and Aerosol Composition|journal = The Journal of Physical Chemistry A|date = 2012-06-21|issn = 1089-5639|pages = 6211–6230|volume = 116|issue = 24|doi = 10.1021/jp211531h|pmid = 22424261|first = Lindsay D.|last = Yee|first2 = Jill S.|last2 = Craven|first3 = Christine L.|last3 = Loza|first4 = Katherine A.|last4 = Schilling|first5 = Nga Lee|last5 = Ng|first6 = Manjula R.|last6 = Canagaratna|first7 = Paul J.|last7 = Ziemann|first8 = Richard C.|last8 = Flagan|first9 = John H.|last9 = Seinfeld|bibcode = 2012JPCA..116.6211Y}} Bibliography
3 : Aerosols|Atmosphere of Earth|Atmospheric dynamics |
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