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40                                                Advanced Mine Ventilation

                      2
         where a ¼ u þ 4ε x l  4ε x and erfc is the complimentary error function. By proper
         substitution in Eq. (3.9), the value of u and consequently the quantity of ventilating air
         required to meet a given health standard can readily be obtained.


         3.6   Dispersion in a Leaky Roadway

         In practice, there are air leaks in most of the airways in mines, and the air velocity is,
         therefore, nonuniform. The leakage factor is a function of the pressure gradient,
         mechanical design of stoppings, doors, air crossings, etc., and the fracture system
         in the strata. In many instances, the nonuniform velocity, u(x), can be approximated
         by u o expð  jxÞ, where u o is the velocity at the initial cross section, and j is the
         leakage factor.
            The one-dimensional model for a leaky roadway for the dispersion of a tracer is

                     2
             vc     v c              vc
                ¼ ε x    u o exp ð  jxÞ                                 (3.10)
             vt     vx 2             vx
            The boundary condition at x ¼ 0 depends on the mode of release of the tracer. In
         reality, it is a function of time, that is, cj  ¼ f (t) / o for large values of t.
                                          x¼o
            Assuming that cj x¼N  ¼ 0 and c ¼ 0at t ¼ 0, a solution of Eq. (3.10) is obtained
         after Grekov [12] as follows:
                       x   Z  t  f ðt   sÞ     x 2
              cðx; tÞ¼ p ffiffiffiffiffiffiffi  1;5  exp      ds
                     2 pε x  o  s          4 ε x s
                                      t
                                    Z
                      j x     u o      f ðt   sÞ
                1   e         p ffiffiffiffiffiffiffiffiffi  1;5
                         4 j e x p ε x  o  s
                    2     p ffiffiffiffiffiffiffiffiffi       2                 p ffiffiffiffiffiffiffi
                   x     j p ε x      jx   j ε x       x    j ε x s
               exp              exp      þ     s erfc  p ffiffiffiffiffiffiffi    ds
                  4 ε x s  2           2    4        2 ε x s   2
                                                                        (3.11)

            In practice, values of j are of the order of 10  3  to 10  4  m  1  and hence u(x) can be
         approximated by u o (1   jx). Under some mining conditions, a steady-state situation
         may develop and Eq. (3.10) then simplifies to:
                2
               v c            vc
             εx      u o ð1   jxÞ  ¼ 0                                  (3.12)
               vx 2           vx
            An approximate solution of Eq. (3.12) for very small values of j is obtained as:


                          u o ð1   jxÞ         u o ð1   jxÞ
             cðxÞ¼ A Exp            þ B Exp                             (3.13)
                             ε x                  ε x
         where A and B are constants and have to be determined from boundary conditions.
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