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194                            Enhanced Oil Recovery in Shale and Tight Reservoirs



               8.8 Further discussions and summary of views and
               hypotheses

               From the above discussions, we can conclude that if a clay-bearing rock
          is not confined, microfractures may be generated. More microfractures may
          be generated owing to shear failures under anisotropic stress conditions
          than under isotropic stress conditions. Fracture opening, closing, reopening,
          and reclosing are a dynamic process, as the hydration conditions are changed.
             The views on the interactions of water-clay bearing rock are not agreed in
          terms of microfractures or permeability. Clays are fine crystalline particles
          with two-dimensional arrays of either silicon/oxygen tetrahedral or
          aluminum (or magnesium)/oxygen hydroxyl octahedral. Clays can be classi-
          fied into five categories: montmorillonite, illite, kaolinite, chlorite, and atta-
          pulgite (van Olphen, 1977). All natural clays have hydrophilic surfaces that
          can adsorb water and some ion species. Hydration of clays in a suspension
          brings about a repulsive force between particles. In addition, the water being
          adsorbed on clays in a formation dissolves the existing salts and results in the
          increase of swelling pressure, which causes the particles clusters to be dispersed
          in the water medium. Therefore, when water contacts swelling clay, the rock
          will swell. But whether the swelling will generate microfractures or reopen
          existing natural fractures remains unconfirmed. Groisman and Kaplan
          (1994) studied the influence of the bottom friction on the size and pattern
          of created fractures during desiccation experiments. Fig. 8.20 shows the
          formed fractures. In their experiment, rock samples lost water and
          contracted, so that tension was reduced, and fractures were created. Such
          experiments are opposite to water imbibition and rock swelling. From their
          experiments, swelling may not create microfractures.

















          Figure 8.20 Pictures of experiment showing fracture creation during desiccation:
          (A) glass plate uncoated, (B) bottom coated with 2 mm of grease, and (C) bottom
          coated with 6 mm of Vaseline (Groisman and Kaplan, 1994).
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