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Fluid-rock interactions                                      181














































              Figure 8.7 CT images of Mancos shale core under various icps (the CT cut face image at
              72 h was reconstructed using the all cross-section images).
                 From these three tests, the following observations can be made.
              (1) Under a lower confining pressure, more fractures were generated dur-
                 ing the initial water imbibition.
              (2) Generated fractures could be closed, reopened, closed and reopened .
                 In other words, opening or closing of a fracture was dynamic,
                 depending on the water concentration change rate and stress conditions
                 (Zhang and Sheng, 2017a; 2017b, 2017c, 2018).
              (3) At the end of each test, very few fractures remained open, regardless of
                 the magnitude of confining pressure, which were also observed earlier
                 (Zhang and Sheng, 2017a; 2017c).
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