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Reservoir Properties of Coal Seams                                237
























           Figure 14.6 Permeability versus closure pressure.

              The closure pressure, P C , is 1050 psi. It is roughly equal to the lower principal, hor-
           izontal stress (s h ) and is linearly related to the permeability of the coal matrix as shown
           in Fig. 14.6 for US coal seams.
              Mathematically,

                                                                         (14.12)
               ln k ¼ a þ bP C
           where k is the permeability in md; a and b are constants for the coal seam; and P C is the
           closure pressure in psi.
              Analyzing the data in Fig. 14.6,

               ln k ¼ 5:1   0:001485 P C                                 (14.13)

              For example, let us assume, P C ¼ 1500 psi.
              Hence,

               ln k ¼ 5:1   0:001485   1500

               or  k ¼ 17:6md

              Permeability of coal decreases with depth. Thakur [1] calculated the relationship
           between permeability and the depth of coal seam as

                       D
               k ¼ k O e                                                 (14.14)
                       a
           where k O is the assumed permeability of 100 md at 100 ft depth; a is a characteristic for
           the coal basin with a value of 700e1000 ft.
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