The body of information presented in this paper is directed towards the scientist or engineer who measures and interprets the physical characteristics of ambient air. This paper interprets measurements made with the Minnesota Aerosol Analyzing System (MAAS) in Denver, near Denver, and near Ft. Collins, Colo., and examines the measurements in the light of what has been learned from several thousand size distributions measured in the other parts of the United States. The origin and physical change of atmospheric particulates is examined through interpretation of modes occurring in the size distributions. The mode coined "AHken Nuclei Range" mode is a measure of aerosol generation, while aged aerosols show up in the "Accumulation Range" mode. Windblown dusts, sea sprays, and mechanically produced particles such as fly ash generate a "Coarse Particle Range" mode. The air environment is categorized into several types of background and urban aerosols whose physical characteristics are described by a limited number of parameters. These categories are exemplified and discussed.During the past few years several thousand in-situ aerosol particle size distributions were measured by the Minnesota Aerosol Analyzing System (MAAS) in a variety of urban and non-urban surface locations throughout the United States. We have shown that the size distribution of airborne particles is almost always multimodal in nature. In addition, we have now classified ambient air environments into several categories. In this paper we shall examine some of the data obtained in the Denver area with respect to these ambient air environment classifications.Much of our understanding of the physical characteristics of airborne particles, such as size distribution and concentration, has come through extended use of the Minnesota Aerosol Analyzing System. The MAAS, described in detail by Whitby et al. ,* measures the number concentration of particles over about four size decades. The three principal instruments in the system are an electrical aerosol analyzer for recording the smaller particle size spectrum, an optical single particle counter for recording the larger size spectrums, and a condensation nuclei counter for the total nuclei count.
May 1975Volume 25, No. 5 529 as in Figure 1, which shows the grand average for 236 runs at Denver's City Maintenance Yard from Oct. [26][27][28][29][30] 1971. Usually number has been plotted since it is the most common weighting measured. Junge observed-and it has been confirmed 3 -that the size distribution between about 0.1 and 5 iim when plotted as in Figure 1 may often be fitted approximately by a power function of the form A/V/Alog D p = KD p~k where K and k are constants. Generally k is between 2 and 4. Clark and Whitby 3 found that Minneapolis urban aerosol could be fitted reasonably well with K = 0.4 VT and k = 3, where VT is the total aerosol volume.However, from Figure 1 it is seen that the number distribution, while showing some intriguing bumps, does not show much detail because of the steep slope for ...