Page 137 - Reservoir Formation Damage
P. 137

Characterization of Reservoir  Rock  119



                                         Electrophoresis
                                         Streaming Potential






                              C
                              0)  -40-
                              O
                             0.



                                -60-
                                    10"               10 V
                                          Ionic Strength [M]
              Figure  6-12. Comparison  of  electrokinetic  measurement  methods  at various
              KCI  ionic  strengths  in  the  4.4-5.8  pH  range  (Johnson,  1999;  reprinted  by
              permission  of  the  author  and  Academic Press).







                                  20-                          .
                                       I   — • — Electrophoresis
                                  10-  I   — * — Streaming Potential -
                                       I
                                  0-
                                      I\
                             >   -10-
                             I—J       1                       :
                             Is  -20-   I
                             1   -30-   V
                              o
                             Q.          \\
                                          \\
                             ^   -40-
                                           ^V-i—.
                                                a
                                                   M:
                                 -50-         ^* *v" ,
                                                   ~-^^
                                 -60-               — *^^      _
                                   C    2   4    6    8   10   1:
                                                PH
              Figure  6-13. Comparison  of  electrokinetic  measurement  methods  at various
                                                  3
              pH  values,  with  the  initial  solution  of  1(T M  KCI  (Johnson,  1999; reprinted
              by  permission  of  the  author  and Academic  Press).
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