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13.3  Properties of Nanoaerosol                                 401

            13.3.3 Diffusion of Neutral Nanoaerosol

            The diffusion coefficient of uncharged nanoaerosol particles in the air can be
            determined by the Stokes-Einstein equation described in Eq. (13.4):

                                             kTC c
                                        D p ¼                            ð13:4Þ
                                             3pld p
            where k is the Boltzmann’s constant, T the temperature, μ the kinetic viscosity of
            the carrier gas. For smaller nanoparticles in the size range of 0.5–2 nm, the diffu-
            sivity can be calculated using the equation given by Ichitsubo et al. [21]as

                                                  r ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                       0:815c rms       M
                                D p ¼               1 þ                  ð13:5Þ
                                                  2
                                     12pNd g þ d p      M n
            where d g is the gas molecule diameter (0.37 nm for air), N is the number con-
                                               3
                                           25
            centration of gas molecules (2:45   10 =m for air at 293 K and 1 atm), M is the
            molar weight of the carrier gas (28.82 for air), M n is the molar weight of nano-
            aerosol particles, c rms is the root mean square velocity of the carrier gas molecules,
            which can be determined using Eq. (13.6).

                                                  1=2
                                             3RT
                                      c rms ¼                            ð13:6Þ
                                              M
            13.3.4 Electrical Properties of Nanoaerosol


            Nanoaerosol particles are primarily charged by diffusive charging. The number of
            ions charged to a nanoaerosol particle is calculated using Eq. (13.7)[63]
                                                       2
                                    d p kT     d p K E c i pe N i0
                             nðtÞ¼       ln 1 þ           t              ð13:7Þ
                                     2
                                   2e K E          2kT
            where c i is the mean thermal speed of ions (239 m/s at standard conditions
            T = 293 K, P = 1 atm), k is Boltzmann constant (1.38 × 10 −23  J/K), K E is a constant
                                             2
                                               2
                                        9
            of proportionality (1/4πε 0 =9 × 10 Nm /C ), N i0 is ion concentration.
              While micron particles may be charged with hundreds of ions, a nanoaerosol
            particle smaller than 20 nm will probably acquire only a couple of ions; in some
            cases it will not acquire any. If polydisperse nanoaerosol particles pass through a
            bipolar charger, two nanoparticles of the same size may obtain different charges
            [32]. Experimental data show that generally, after charging, sub-20 nm particles
            carry a negative charge while larger particles carry a positive charge [1].
              High concentration of ions and sufficient charging time allow particles to reach
            maximum charging. The maximum charging by unipolar charging enables the
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