Page 212 - Fundamentals of Reservoir Engineering
P. 212

OILWELL TESTING                                    150

                     mathematics and for this solution the boundary and initial conditions may be stated as
                     follows

                     a)    p =  p at t =  0, for all r
                                i

                     b)    p =  p at r = ∞ , for all t                                               (7.1)
                                i

                                 ∂ p  qµ
                     c)    lim r    =     , for t >  0
                                      π
                           r →  0  r ∂  2 kh

                     Condition (a) is merely the initial condition that, before producing, the pressure
                     everywhere within the drainage volume is equal to the initial equilibrium pressure p i.

                     Condition (b) ensures the condition of transience, namely that the pressure at the
                     outer, infinite boundary is not affected by the pressure disturbance at the wellbore and
                     vice versa.

                     Condition (c) is the line source inner boundary condition.

                     In addition, the assumptions made in deriving the radial diffusivity equation in
                     Chapter 5 are retained. That is, that the formation is homogeneous and isotropic, and
                     drained by a fully penetrating well to ensure radial flow; the fluid itself must have a
                     constant viscosity and a small and constant compressibility. The solution obtained will,
                     therefore, be applicable to the flow of undersaturated oil. Having developed the simple
                     theory of pressure analysis based on these assumptions, many of the restrictions will
                     be removed by considering, for instance, the effects of partial well completion, the flow
                     of highly compressible fluids, etc. These modifications to the basic theory will be
                     gradually introduced in this and the following chapter.

                     Under the above conditions the diffusivity equation


                           1  ∂     r  ∂ p    =  φµ c ∂ p                                           (5.20)
                           r ∂ r       r ∂       k   t ∂

                     can be solved by making use of Boltzmann's transformation

                                          r 2              φµ cr 2
                           s =                          =
                                4 (Diffusivity constant)t   4kt


                     so that

                           ∂ s    φµ  cr
                               =                                                                     (7.2)
                             t ∂   2k t

                     and


                           ∂ s    φµ  cr 2
                               =                                                                     (7.3)
                             r ∂   4k t 2
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