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         Figure 14.3 Gas isotherms for US coal seams.


            It is to be noted that high-rank (low-volatile bituminous) coals contain more gas
         than the low-rank (high-volatile bituminous) coals (HVA, HVB, HVC) at the same
         confining pressure. It is also clear that the sorption capacity of all coal increases
         with pressure, but the increase occurs at an ever-decreasing rate as the sorption capac-
         ity reaches an asymptotic limitdthe saturation limit.
            A mathematical representation for these isotherms was given by Langmuir [11] and
         is expressed as

                       bP
             V ¼ V m                                                    (14.4)
                     1 þ bP
                                                         3
         where V is the volume of gas contained at pressure P, ft /t; V m is the maximum
                                 3
         sorption capacity of coal, ft /t; P is the pressure, psi; and b is the Langmuir
         constant, psi.  1
            For indirect determination of the gas content of coal at a given pressure, Eq. (14.4)
         can be rewritten as

             P    P     1
               ¼    þ                                                   (14.5)
             V   V m  bV m
   250   251   252   253   254   255   256   257   258   259   260