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Mineralogy  and Mineral  Sensitivity of Petroleum-Bearing  Formations  29

                                               • Double  Layers  Overlap
                                               •——
                                              ©












                                                        Semipermeable
                                                  Membrane  Surrounding
                                                    Clay  Particles
             Figure  2-18.  Mechanism  of  osmotic  pressure  generation  between  two  clay
             particles  in  water  (after  C.  C.  Ladd,  1960; reprinted  by  permission  of  the
             Transportation  Research  Board,  the  National  Academies,  Washington, D.C.,
             from  C.  C.  Ladd,  "Mechanisms  of  Swelling  by  Compacted  Clay,"  in  Highway
             Research  Board  Bulletin  245, Highway  Research  Board,  National  Research
             Council,  Washington,  D.C., 1960,  pp. 10-26).


                                        Swollen
                                        region




                             Pore
                             surface

                         Pore
                         volume      Water
                                     absordtion














             Figure  2-19.  Mechanism  of  formation  swelling  by  water  absorption
             (after  Civan,  ©1999  SPE; reprinted  by  permission  of  the  Society  of  Petro-
             leum  Engineers).
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