Page 174 - Formation Damage during Improved Oil Recovery Fundamentals and Applications
P. 174

150                                                 Thomas Russell et al.


             To incorporate this, we propose that the attached concentration is
          governed by:
                                                 0
                                                  ð
                              σ a x; tð  Þ 5 σ cr Ux; tÞ; γ x; tÞÞ:  (3.165)
                                           ð
                                         ð
                  0
          where γ is a new variable, referred to as the pseudo-salinity, which is
          related to the bulk fluid salinity by:
                                   0
                                               ð
                                  γ x; t 1 τð  Þ 5 γ x; tÞ:          (3.166)
             This parallels the initial introduction of delayed detachment given in
          Section 3.6.1. It follows that using a Taylor’s series expansion, a relation-
          ship can be derived for the pseudo-salinity:
                                     @γ  0
                                    τ    5 γ 2 γ :                   (3.167)
                                                0
                                      @t
             The Eqs. (3.165) and (3.167) satisfy the condition that changes to the
          fluid velocity result in an immediate change in the attached concentra-
          tion, while changes to the fluid salinity have a delayed effect according to
          a nonequilibrium relation.
             The full system of equations can then be given:
                             @                 αq @c
                               ð φc 1 σ s 1 σ a Þ 1  5 0;            (3.168)
                             @t               2πr @r
                                           αλcq
                                     @σ s
                                         5      ;                    (3.169)
                                      @t    2πr

                                            q
                                                0
                                  σ a 5 σ cr  ; γ ;                  (3.170)
                                           2πr
                                    @γ    q @γ
                                  φ    1       5 0;                  (3.171)
                                    @t   2πr @r
                                 q           k    @p
                                    52               :               (3.172)
                                2πr     μ 1 1 βσ s Þ @r
                                          ð
             Using the dimensionless coordinates outlined in Section 3.5,

                             2
                 qt        r         σ s     σ a      σ cr            πkp
           T-       ; X-      ; S s -  ; S a -  ; S cr -  ; Λ-λr w ; P-  ;
                πr φ       r e       φ       φ         φ              qμ
                  2
                  e
                 γ 2 γ       qτ
            Γ 5       J  ; ε-    :
                 γ 2 γ      πr φ
                              2
                  I    J      e
                                                                     (3.173)
   169   170   171   172   173   174   175   176   177   178   179