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Forms of Inorganics in. Tropospheric Particles

The discussion thus far has focused on the elemental composition of particles, which can be determined using such techniques as neutron activation or X-ray fluorescence analysis (see Chapter 11). One of the questions of increasing interest is the chemical form in [Pg.388]

FIGURE 9.39 Analysis of particles as a fraction of particle size in the Amazon Basin using factor analysis (adapted from Artaxo and Hansson, 1995). [Pg.389]

TABLE 9.16 Deliquescence Points of Some Salts Commonly Found in Ambient Air at 25°C  [Pg.389]

FIGURE 9.40 Calculated changes in particle size as a function of relative humidity at 25°C from particles with four different chemical compositions (adapted from Tang, 1980). [Pg.390]

FIGURE 9.41 Uptake of water by (NH4)S04 and its dlying as a function of relative humidity at 25b3C (adapted from Tang et al., 1995). [Pg.390]


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