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92   PORE GEOMETRY IN GAS SHALE RESERVOIRS

                                                       100,000     The total pore volume is derived from the amount of
                                                                 vapor adsorbed at a relative pressure close to unity, by
                                                       10,000    assuming that the pores are then filled with liquid adsorbate.
                             Data points                         The average pore size could be estimated from the total pore
                                                       1,000     volume determined at maximum pressure, by assuming that
                                             Threshold           the pores which would not be filled below a relative pressure
             P c  (psi)                      pressure  100       of 1 have a negligible contribution to the total pore volume.


                   Irreducible                                   For example, assuming cylindrical pore geometry, the
                  wetting phase                        10        average pore radius (r ) can be expressed as:
                                                                                  p
                    saturation
                                                       1                                2 V
                                                                                     r p  ads                (5.3)
                                                       0.1                                S
             100  90  80  70  60  50  40  30  20  10  0          where V  is the total amount of nitrogen adsorbed and S is
                                                                       ads
                               Shg (%)                           the surface area (Quantachrome Instruments, 2008).
                  FIGurE 5.3  Typical capillary pressure profile.  The distribution of pore volume with respect to pore size
                                                                 is called pore size distribution (PSD). Usually the BJH model
                                                                 (Barret et al., 1951) and DH model (Dollimore and Heal,
            incrementally into the porous media and recording the injected   1964) are used for determining PSD using nitrogen adsorp­
            volume at each step. This type of pressure‐controlled instru­  tion for the shale layers. The actual pore size in both of these
            ment measures the pore‐throat size (pore entry radii) and does   models is calculated using the thickness of the adsorbed layer
            not detect the size of the pore body behind the throats (Burdine   and the Kelvin equation (Gregg and Sing, 1991):
            et al., 1950; Churcher et al., 1991; Heath et al., 2011).

                                                                                    P   2  V m
            5.3.2  Nitrogen adsorption (N )                                     ln           cos             (5.4)
                                      2                                            P    RTr
                                                                                    0      K
            The low pressure adsorption measurement allows us to
            understand the PSD and study the parameters which control   where P is the gas vapor pressure, P  is the saturation pressure
                                                                                            0
            the adsorbed gas capacity, such as surface area and micropo­  of the adsorbent,  γ is the surface tension of nitrogen at its
            rosity. Low pressure adsorption measurement has been used   boiling point (77 K), θ is the contact angle between the adsor­
            extensively in surface chemistry analysis for characteriza­  bate (liquid nitrogen) and the adsorbent, V  is the molar volume
                                                                                                m
            tion of porous materials, and more recently has been adopted   of liquid nitrogen, R is the gas constant, T is the boiling point
            for characterization of the nanopores in the shale samples   of nitrogen (77 K), and r  is the Kelvin radius of the pore.
                                                                                    K
            (Chalmers et al., 2012; Kuila and Prasad, 2011; Ross and   Micromeritics TriStar II 3020 was used to determine the
            Marc Bustin, 2009)                                   quantity of nitrogen adsorbed. The samples were prepared by
              Low‐pressure nitrogen adsorption (LPNA) measurement   sieving crushed samples less than 250 µm. The samples were
            is used to quantify the amount of gas adsorbed at different   initially treated with heat and vacuum to remove contami­
            relative pressures (P/P ), where P is the gas vapor pressure   nants. After cooling the sample under a vacuum, nitrogen was
                              0
            in the  system and  P  is the  saturation  pressure of  the   dosed into the sample at controlled increments. The total pore
                              0
            adsorbent. The Brunauer–Emmett–Teller (BET) method is   volume from the adsorption tests was found from the quantity
            the most widely used procedure for determination of the   of vapor adsorbed at relative pressure. An assumption here is
            surface area of porous samples (Brunauer et al., 1940).   that the pores were filled with liquid adsorbate. Average
            Equivalent surface area is calculated using the BET equation   pore size was then approximated by the total pore volume
            (Quantachrome Instruments, 2008):                    determined at maximum pressure, assuming that the unfilled
                                                                 pores below a very low relative pressure make a negligible
                                                                 contribution to the total pore volume.
                           1         1    C  1 P
                                                        (5.2)
                           /
                     W   P P 0  1   WC    WC P  0
                                     m
                                           m
                                                                 5.3.3  Low‐Field Nmr
            where W is the weight of gas adsorbed at a relative pressure   Low‐field NMR is a nondestructive technique that involves
            (P/P ) (P being the gas vapor pressure in the system and P    the motion of a proton (hydrogen 1H) occurring in water and
                                                           0
               0
            the saturation pressure of the adsorbent), W  is the weight of   hydrocarbon fluids relative to the porous rock. Utilizing
                                              m
            monolayer nitrogen adsorbed to the sample. The C constant   NMR to characterize fluid rock system properties, such as
            is related to the energy of adsorption and its value shows the   porosity, pore size distribution, and permeability, has become
            magnitude of the adsorbent/adsorbate interactions.   popular in the industry (Bowers et al., 1993; Coates et al.,
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