Page 190 - Percolation Models for Transport in Porous Media With
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188           CHAPTER 11  GAS COLMATATION IN ELECTRIC ACTION

         where Lp is the specific heat of liquid evaporation, we obtain

                                   R   dTs    1- pp(pp)fPJ(Pp)
                                    pPp dpp  =   "fpL*(pp)                 (11.24)

                        L  •  _   Lp(Pp)   ,._  _  c: _  c:                (11.25)
                           -            '   IP-  p  -  p
                              "fpRpTs(Pp)       Cv    Cp- Rp
            After substituting (11.24) in (11.22) and (11.19) and taking into account (11.23),
         we obtain the correlation between  Q~  and the change of pressure

                                            3
                                 q~ = (  4/3)1!'a (r:;- )dppf  dt          (11.26)
                                                 1
                              r. = ("'p -1)£*(1- PpfPJ)-1
            Since along the vapor isentrope (the entropy of the vapor is  Sp  =canst)




         and along the saturation line of the vapor, according to (11.24), (11.25),




         it follows that the quantity r. shows how close to isentropic is the behavior of the
         vapor, since
                                 r  _ (arp)  /(arp)

                                   •  -  opp  sp   opp  s
            When r. > 1 and  dppfdt  < 0,  it  follows  from  (11.26)  that  q~ > 0 and from
         (11.20} that 8Qp > 0.  This means that the vapor is receiving heat, while the pres-
         sure in the bubble grows.  At the same time, the temperature gradient oTpfor < 0,
         and  therefore  the temperature is  higher  in  the center of the  bubble  than on  its
         surface.  The latter fact  demonstrates the stability of the bubble growth.
            If  we differentiate the mass conservation equation for  the bubble




         and take into account the relationship




         where e12 is the mass flow of the bubble due to the phase transition in the boundary
         layer through a unit surface area, we obtain

                                                                          (11.27}
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