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    Measurements of the Particle Size Distribution of the Atmospheric Aerosol: II. Experimental Results and Discussion

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 005::page 577
    Author:
    Pasceri, Ralph E.
    ,
    Friedlander, S. K.
    DOI: 10.1175/1520-0469(1965)022<0577:MOTPSD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Distribution data obtained by sampling the Baltimore aerosol with a cascade impactor are reported for the range between 0.4 and 20 microns radius. Data for the range between 70 Å and 0.1 microns in radius were obtained in two runs with the rotating disk sampler. Greater variations were observed in the lower end of the spectrum than in the upper end. The theory of self-preserving size distributions was used with some success to correlate data obtained in this and other studies. When the theory applies and the r?4 subrange exists, the size distribution is given by n(r)=0.04?r?4 where ? is the volume fraction of aerosol material.
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      Measurements of the Particle Size Distribution of the Atmospheric Aerosol: II. Experimental Results and Discussion

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150774
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    contributor authorPasceri, Ralph E.
    contributor authorFriedlander, S. K.
    date accessioned2017-06-09T14:13:37Z
    date available2017-06-09T14:13:37Z
    date copyright1965/09/01
    date issued1965
    identifier issn0022-4928
    identifier otherams-15135.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150774
    description abstractDistribution data obtained by sampling the Baltimore aerosol with a cascade impactor are reported for the range between 0.4 and 20 microns radius. Data for the range between 70 Å and 0.1 microns in radius were obtained in two runs with the rotating disk sampler. Greater variations were observed in the lower end of the spectrum than in the upper end. The theory of self-preserving size distributions was used with some success to correlate data obtained in this and other studies. When the theory applies and the r?4 subrange exists, the size distribution is given by n(r)=0.04?r?4 where ? is the volume fraction of aerosol material.
    publisherAmerican Meteorological Society
    titleMeasurements of the Particle Size Distribution of the Atmospheric Aerosol: II. Experimental Results and Discussion
    typeJournal Paper
    journal volume22
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1965)022<0577:MOTPSD>2.0.CO;2
    journal fristpage577
    journal lastpage584
    treeJournal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 005
    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
    yabeshDSpacePersian