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38                                                Advanced Mine Ventilation

         mine airways. In these circumstances, a one-dimensional model of dispersion is
         considered quite accurate. The concentration is then a function of x and t alone
         as given below.

                                  "        2  #
                        Q            ðx   utÞ
             cðx; tÞ¼       0:5 exp                                      (3.4)
                     2Aðpε x tÞ        4ε x t

         where A is the cross-sectional area of the roadway. Calculations of the dispersion
         coefficients from experimental data can be done very simply as discussed in great
         detail by Airey [8] and Klebanov [9].





         3.4   Continuous Stationary Point Source

         This case is represented by a continuous source in the roadway often obtained in
         practice. It is also used for the experimental determination of the radial coefficient
         of turbulent dispersion. The mathematical model is obtained from Eq. (3.2) by simply
         dropping the  vc  term, that is,
                    vt
                                   2
               vc     1 v   vc    v c
             u   ¼ ε r     r    þ                                        (3.5)
               vx     r vr  vr    vx 2
            The boundary conditions for a source at the origin are

         1. C / 0as s /N
                           2 0.5
                       2
              where s ¼ (r þ x )
         2. c ¼Nas s / 0
            A third condition results from the conservation of mass, that is,

                       vc
                   2
                4ps ε r    ¼ Q at s/0
                       vs
                          x
            A solution of Eq. (3.5) with the above boundary conditions has been derived by
         Roberts [10] as given below:

                  Q         uðs   xÞ
             c ¼      exp                                                (3.6)
                 4pε r s      2ε r
            Taking logarithms on both sides of Eq. (3.6) and rearranging, the following
         relationship is obtained:

                Q            u
             ln     ¼ ln ε r þ  ðs   xÞ                                  (3.7)
               4psc         2ε r
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