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108                                        4 Properties of Aerosol Particles

              Equation (4.37) becomes,

                                               N 0
                                       NtðÞ ¼                            ð4:39Þ
                                             1 þ t=s
              Since N ¼ N 0 =2 when t ¼ s, s is also referred to as the half-value time, which is
            the time it takes for the particle number concentration to drop to half of its initial
            value.

            Example 4.6: Half value time of monodisperse aerosol
            Calculate the half-value time of spherical monodisperse aerosol with an initial
                                       3
                            3
            concentration of 10 particles/cm and an initial particle diameter of d p ¼ 1 nm.
            Assume standard condition and only Brownian coagulation is considered.
            Solution
            The Knudsen number of 1 nm particle is

                            Kn 1nmÞ ¼ 2   0:066=0:001 ¼ 132 [ 100
                              ð
              It is within the free molecule region. Therefore,

                                      s ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                           s ffiffiffiffiffiffiffiffiffi
                              kT        ð 1:38   10  23 Þ   298      7
                    K ¼ 9:8      ¼ 9:8                 9  ¼ 6:28   10
                                                ð
                              p
                             q d p       1;000   1   10 Þ
              Then the half-value time is
                         2                   2
                    s ¼     ¼                                 ¼ 0:003 s
                        KN 0  6:28   10  7    10 3  1  3   10 6 cm 3
                                              cm         m 3


              As seen from the result, particles at 1 nm do not have a great life time. While this
            is practically inaccurate, it does qualitatively show that aerosol particle diameter is a
            dynamic parameter.



            4.4.2 Polydisperse Coagulation


            Coagulation coefficients for different mechanisms have been summarized by Geng
            et al. [10]. Brownian motion is the dominating mechanisms for the coagulation of
            very fine particle under normal atmospheric condition; for this reason, our analysis
            is focused on Brownian coagulation.
              One of the widely used Brownian coagulation coefficients is the Fuchs (1964)
            equation for binary collision.
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