By Thomas T. Mercer
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Extra info for Aerosol Technology in Hazard Evaluation
31) where N is the number of ions of one sign per cubic centimeter. This formula refers to the droplet volume while still in the bulk liquid. As it is being formed into a droplet, however, there may be time for it to discharge partially. As the ionic strength increases, the discharge rate increases. At the same time, interionic forces tend to reduce the net charge in a given element of volume before it is detached, so that the charge carried away by the droplet is less than that given by Eq. 31).
Information concerning the fluid resistance acting on bodies of other nonspherical shapes, even regular, isometric solids, comes from experimental studies. 1b A+B i 1 EXP(- - i i l l i i ! 00 y. / ^5? 95 / / KNUDSEN-WEBER _, MlLLIKAN MATTAUCH J EQUATION 8 / 1 I I 10 I 20 I 50 I I 100 200 1 ! 500 1000 λ/α FIG. 4. 091 //m). Courtesy of Institute of Physics and The Physical Society. 01 - Ref.          a KR = FRI^U(nS)ll2\ FR is the experimental resistance force. *C R -R.
3) The relationship between the resistance force and velocity for these two special cases is Newton's law : FR oc U2 Stokes's law : FR oc U. Stokes's law applies when viscous resistance is sufficiently large that flow about the sphere shows front and back symmetry; Newton's law applies when inertial effects are very much greater than viscous resistance. In between, there is a wide range in which FR is proportional to Un, where 1 < n < 2. This variation of FR with velocity requires some criterion for comparing the 26 Properties of Aerosols 2 significance of each effect under a given set of conditions.
Aerosol Technology in Hazard Evaluation by Thomas T. Mercer