Paul A. Baron, Ph.D., NIOSH/DPSE

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Paul A. Baron, Ph.D., NIOSH/DPSE NIOSH Manual of Analytical Methods (1994)

For quantitative measurements, it is necessary to calibrate with an aerosol similar in refractive index and particle size to the one being measured. This is because aerosols with different refractive indices can produce photometer responses differing by more than a factor of ten. Since these instruments have specific size-dependent response to particles, the size distribution of dust particles is also important in evaluating the mass response of the instrument for a specific dust.
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Paul A. Baron, Ph.D., NIOSH/DPSE NIOSH Manual of Analytical Methods (1994)

An aerosol is a group of particles suspended in the air. Aerosols can be introduced into the body primarily through the respiratory system. Total dust measurements indicate concentrations that can enter the nose and mouth of a worker as well as that which can settle on the skin while the respirable fraction of dust is that portion which can reach the lower or gas exchange part of the respiratory system.
Source: Wikisource

Paul A. Baron, Ph.D., NIOSH/DPSE NIOSH Manual of Analytical Methods (1994)

The amount of light scattered by a particle into the detector is a complex function of the particle size, shape and refractive index. For spherical particles of known refractive index the instrument response can be calculated. However, in general, calibration must be carried out experimentally. An example of instrument response as a function of particle size for spherical particles of two different refractive indices is shown in Figure 1. It can be seen that there is a peak at approximately 0.6 mm and that there is a drop in instrument response to larger particles.
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