COMPARISON AND COMBINATION OF AEROSOL-SIZE DISTRIBUTIONS MEASURED WITH A LOW-PRESSURE IMPACTOR, DIFFERENTIAL MOBILITY PARTICLE SIZER, ELECTRICAL AEROSOL ANALYZER, AND AERODYNAMIC PARTICLE SIZER
Tm. Peters et al., COMPARISON AND COMBINATION OF AEROSOL-SIZE DISTRIBUTIONS MEASURED WITH A LOW-PRESSURE IMPACTOR, DIFFERENTIAL MOBILITY PARTICLE SIZER, ELECTRICAL AEROSOL ANALYZER, AND AERODYNAMIC PARTICLE SIZER, Aerosol science and technology, 19(3), 1993, pp. 396-405
Data from a different mobility particle sizer (DMPS) or an electrical
aerosol analyzer (EAA) has been combined with data from an aerodynamic
particle sizer (APS) and converted to obtain aerosol mass distributio
n parameters on a near real-time basis. A low pressure impactor (LPI),
a direct and independent measure of this mass distribution, provided
information for comparison. The number distribution of particles withi
n the electrical measurement range was obtained with the DMPS and EAA.
Data from the APS for particles greater than that size were used to c
omplete the number distribution. Two methods of obtaining mass distrib
ution parameters from this number data were attempted. The first was t
o convert the number data, channel by channel, to mass data and then f
it a log-normal function to this new mass distribution. The second met
hod was to fit a log-normal function to the combined number distributi
on and then use the Hatch-Choate equations to obtain mass parameters.
Both the DMPS/APS and the EAA/APS systems were shown to successfully m
easure aerosol mass distribution as a function of aerodynamic diameter
. Careful operation of the measurement equipment and proper data manip
ulation are necessary to achieve reliable results. A channel-by-channe
l conversion from number to mass distribution provided the best compar
ison to the LPI measurement. The DMPS/APS combination furnishes higher
-size resolution and accuracy than the EAA/APS system. A small gap was
observed in the EAA/APS combined data; however, this did not seem to
adversely affect the determination of mass distribution parameters.