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contributor authorHusar, R. B.
contributor authorShu, W. R.
date accessioned2017-06-09T17:38:25Z
date available2017-06-09T17:38:25Z
date copyright1975/12/01
date issued1975
identifier issn0021-8952
identifier otherams-8995.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232433
description abstractIt has been shown by earlier studies on the formation of the Los Angeles smog aerosol, that a significant fraction of the particulate matter in the visible size range is made by secondary gas-particle conversion processes, and that it consists mainly of liquid matter. In this study the volatility was studied quantitatively by heating the smog aerosol up to 250°C and simultaneously measuring the scattering coefficient using a nephelometer and the change of size distribution by an optical counter. The thermal analyses revealed that 50?80% of the submicron aerosol mass is volatile at 220°C. Inspection of the shapes of thermo-nephelograms (bscat vs temperature) also revealed that photochemically formed aerosols have distinctly different thermo-nephelograms than those obtained on humid ?hazy? days. Thus it is suggested that thermal analyses may at least in some instances provide the means of on-line monitoring the origin of the ambient aerosol.
publisherAmerican Meteorological Society
titleThermal Analyses of the Los Angeles Smog Aerosol
typeJournal Paper
journal volume14
journal issue8
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1975)014<1558:TAOTLA>2.0.CO;2
journal fristpage1558
journal lastpage1565
treeJournal of Applied Meteorology:;1975:;volume( 014 ):;issue: 008
contenttypeFulltext


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