Theory of Operation
B-21
Note:
All of the experiments were performed using air at Standard
Temperature & Pressure (STP) as the working gas. Since diffusion
losses are a function of the particle diffusion coefficient D which is a
function of the working gas properties, the use of different working
gases and/or conditions will result in an error in the calculated
diffusion loss. It is possible to input gas properties in the software to
increase the Diffusion Loss Correction accuracy, but other working
gases and conditions have not been experimentally verified.
S e l e c t e d R e f e r e n c e s
The following list contains papers that are referenced in this chapter as well
as other references that may be interesting to the reader.
A
Adachi, M., K. Okuyama and Y. Kousaka [1985]
“Electrical Neutralization of Charged Aerosol Particles by Bipolar Ions.”
Journal of Chemical Engineering,
Japan, 16:229.
Agarwal J.K., and G.J. Sem [1978]
“Generating Submicron Monodisperse Aerosols for Instrument
Calibrations,”
TSI Quarterly,
May/June, p 5, TSI Incorporated, St. Paul,
MN.
Allen, M.D., and O.G. Raabe [1985].
“Slip Correction Measurements of Spherical Solid Aerosol Particles in an
Improved Millikan App
aratus,”
Aerosol Science and Technology
. 4:269-
286.
B
Birmili, W., Stratmann, F., Wiedensohler, A., Covert, D., Russell, L. M. and
Berg, O. (1997). Determination of Differential Mobility Analyzer Transfer
Functions Using Identical Instruments in Series.
Aerosol Science and
Technology
27
: 215-223.
Blackford, D.B., and G. Simons [1986]
“Particle Size Analysis of Carbon Black.” TSI Incorporated, St. Paul, MN.
Presented at Fine Particle Society Annual Meeting, San Francisco, CA,
July. (Unpublished)
C
Chen, D-R, D.Y.H. Pui, D. Hummes, H. Fissan, F.R. Quant, and G.J. Sem,
[1998]
“Design and Evaluation of a Nanometer Aerosol Differential Mobility
Analyzer (Nano-
DMA),” Journal of Aerosol Science 29/5:497-509.
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