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    Thermal Analyses of the Los Angeles Smog Aerosol

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 008::page 1558
    Author:
    Husar, R. B.
    ,
    Shu, W. R.
    DOI: 10.1175/1520-0450(1975)014<1558:TAOTLA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It 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.
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      Thermal Analyses of the Los Angeles Smog Aerosol

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4232433
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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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