Page 413 - Petrophysics 2E
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EVALUATION OF WETTABILITY            381


                           thermodynamic work required for fluid displacements:




                                                                                        (6.30)



                             As an example, displacements from a Cottage Grove sandstone core
                           (Figure 5.16 in Chapter 5) were:

                           Curve 1 (oil displacing water from S, = 1 .0 to Si,)  = 0.165 joules/ml =
                             24.82 BTU/bbl
                           Curve  3  (water  displacing  oil  from  Si,   to   - waterflood)  =
                             0.0089 J/ml = 1.34 BTU/bbl
                           Curve  5  (oil  displacing  water  from  h0, to  Si,)   =  0.771J/ml  =
                             116.25 BTU/bbl
                             Less energy is required for displacement of water from 100% saturation
                           (Curve  1) than from S,,,   (Curve  5),  because a considerable amount
                           of  water  is displaced  at  low pressure after the  threshold pressure is
                           exceeded. A very small amount of energy is required for displacement of
                           oil because the Cottage Grove Sandstone exhibits a strong water-wetting
                           tendency;  consequently, some oil is displaced by  imbibition (at  zero
                           capillary pressure) upon initial contact  of  the oil-saturated core with
                           water.  Stating  this  in  another  way:  If  the  water-oil-rock system  is
                           water-wet,  A1 is a large positive value and, therefore, considerable work
                           must be done on the system to displace the water. On the other hand, the
                           area under the waterdisplacing-oil curve is a very small positive value;
                           hence, water will imbibe into the water-wet system spontaneously with
                           simultaneous displacement of oil.
                             When  a core  is  strongly water-wet (USBM  I,  > 0.7), the  core will
                           imbibe water  until  the  water  saturation is  essentially   and  the
                           area under the curve is almost zero; hence, the work required for oil
                           displacement is almost zero for a strongly water-wet system. The amount
                           and rate of  imbibition depend on a  number of  simultaneously acting
                           properties  of  the water-oil-rock system:  the  rock  and fluid  chemical
                           properties expressed as wettability, interfacial tension, saturation history
                           of the system, initial saturation, fluid viscosities, pore geometry, and pore
                           size distribution.
                             As  the  system  becomes  less  water-wet,  the  work  required  for
                           displacement of oil increases and, consequently, the amount and rate
                           of imbibition decreases. Thus, a smaller amount of water will imbibe at a
                           lower rate as the system becomes less water-wet. At neutral wettability,
                           water will not imbibe when the water saturation is at Si,  and oil will
                           not imbibe when the water saturation is at S,,,.   Thus, a positive initial
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