Page 220 - Fundamentals of Enhanced Oil and Gas Recovery
P. 220

208                                                                    Mohammad Ali Ahmadi


                water from left to right. The rate the water enters to the medium element from
                left-hand side is
                                 q t 3 f w 5 water flow rate entering the element
                   The rate of water leaving element from the right-hand side is


                              q t 3 f w 1 Δf w 5 water flow rate leaving the element
                   The change in water flow rate across the element is found by performing a mass
                balance. The movement of mass for an immiscible, incompressible system gives

                         Change in water flow rate 5 water entering 2 water leaving
                                                                                       (7.1)

                                                 5 q t 3 f w 2 q t f w 1 Δf w 52 q t 3 Δf w
                   This is equal to the change in element water content per unit time (see Fig. 7.1).
                Let S w be the water saturation of the element at time t. Then, if oil is being displaced
                from the element, at the time (t 1 Δt), the water saturation will be (S w 1 ΔS w ).
                Therefore, water accumulation in the element per unit time is
                                                              ΔS w 3 A 3 φ 3 Δx
                            water accummulation per unit time 5                        (7.2)
                                                                     Δt
                where φ is porosity; equating Eqs. (7.1) and (7.2) results
                            ΔS w 3 A 3 φ 3 Δx                ΔS w    2 q t 3 Δf w
                                              52 q t 3 Δf w -     5                    (7.3)
                                   Δt                         Δt    A 3 φ 3 Δx

                   In the limit as Δt - 0 and Δx - 0 (for the water phase):

                                            ΔS w      2 q t  df w
                                                  5                                    (7.4)
                                             Δt      A 3 φ  dx
                                                 x              t
                   The subscript x on the derivative indicates that this derivative is different for each
                element. It is not possible to solve for the general distribution of water saturation
                S w (x, t) in most realistic cases because of the nonlinearity of the problem. For exam-
                ple, water fractional flow is usually a nonlinear function of water saturation. It is,
                therefore, necessary to consider a simplified approach to solving Eq. (7.4).











                Figure 7.1 Horizontal bed containing oil and water.
   215   216   217   218   219   220   221   222   223   224   225