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188                            Enhanced Oil Recovery in Shale and Tight Reservoirs


             Faulkner and Rutter (2000) also attributed the permeability reduction to
          the water adsorption on mineral surfaces so that the pores became smaller;
          the permeability reduction might not be caused by clay swelling. In other
          words, nonswelling minerals could also have lower water permeability.
          For this liquid adsorption mechanism to inhibit flow, the pores must be
          very small, probably few nanometers. Zhang and Sheng (2017a, 2018)
          also observed that the shale core permeability measured using water is several
          times up to 100 times lower than that measured using nitrogen, after the
          cores were hydrated. However, in their original paper, they attributed this
          difference to clay swelling, which is not. It is caused by liquid adsorption
          in small pores.
             Roshan et al. (2015) measured the upstream pressure (with the down-
          stream being atmospheric), when a fractured core (split into two halves)
          was flooded. The core was under 1000 psi (6.9 MPa) confining pressure.
          A 10 wt.% NaCl solution, followed by deionized (DI) water, was injected
          into the core for approximately 4 h. Fig. 8.13 shows the upstream pressures
          of the core when 10 wt.% NaCl solution and DI water were flooded. The
          upstream pressure maintained almost constant in the case of 10 wt.% NaCl






























          Figure 8.13 Upstream pressure measurements versus time during the fracture perme-
          ability test when (A) 10 wt.% NaCl solution was used, and (B) deionized water was used
          (Roshan et al., 2015).
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