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Detection particle sizers

The condensation particle counter battery measurements are complemented by aerosol particle size distribution measurements using a dual differential mobility particle sizer system covering a size range of 3-900 nm, and an aerodynamic particle sizer covering aerosol particle sizes between 0.7 and 20 pm. In addition, air ions are detected using a balanced scanning mobility analyser and an air ion spectrometer. During the period of measurements, several new particle formation (nucleation) events occur in tropospheric air. [Pg.148]

Physical characterization of TBO includes particle size and size distribution measurement by laser diflraction (macroporosity) as well as specific surface area measurement (microporosity). Particle size measurement by FSSS (Fisher Sub-Sieve Sizer), as also sometimes used, is misleading, because of the porosity of the TBO particles. An empirical relationship between FSSS and particle size measured by laser scattering can, however, be detected if the microporosity of the samples is uniform (constant blueing conditions). [Pg.214]


See other pages where Detection particle sizers is mentioned: [Pg.85]    [Pg.305]    [Pg.425]    [Pg.425]    [Pg.305]    [Pg.155]    [Pg.413]    [Pg.173]    [Pg.179]    [Pg.131]    [Pg.200]    [Pg.131]    [Pg.475]    [Pg.131]   
See also in sourсe #XX -- [ Pg.425 ]




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