Page 189 - Fundamentals of Reservoir Engineering
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CHAPTER 5


                         THE BASIC DIFFERENTIAL EQUATION FOR RADIAL FLOW IN A POROUS
                                                           MEDIUM


              5.1    INTRODUCTION

                     In this chapter the basic equation for the radial flow of a fluid in a homogeneous porous
                     medium is derived as

                           1 ∂     kρ ∂ p    =  φρ ∂ p                                               (5.1)
                                             c
                                    r
                           r ∂ r       µ  r ∂       t ∂

                     This equation is non-linear since the coefficients on both sides are themselves
                     functions of the dependent variable, the pressure. In order to obtain analytical
                     solutions, it is first necessary to linearize the equation by expressing it in a form in
                     which the coefficients have a negligible dependence upon the pressure and can be
                     considered as constants. An approximate form of linearization applicable to liquid flow
                     is presented at the end of the chapter in which equ. (5.1) is reduced to the form of the
                     radial diffusivity equation. Solutions of this equation and their applications for the flow
                     of oil are presented in detail in Chapters 6 and 7. For the flow of a real gas, however, a
                     more complex linearization by integral transformation is required which will be
                     presented separately in Chapter 8.

              5.2    DERIVATION OF THE BASIC RADIAL DIFFERENTIAL EQUATION


                     The basic differential equation will be derived in radial form thus simulating the flow of
                     fluids in the vicinity of a well. Analytical solutions of the equation can then be obtained
                     under various boundary and initial conditions for use in the description of well testing
                     and well inflow, which have considerable practical application in reservoir engineering.
                     This is considered of greater importance than deriving the basic equation in cartesian
                     coordinates since analytical solutions of the latter are seldom used in practice by field
                     engineers. In numerical reservoir simulation, however, cartesian geometry is more
                     commonly used but even in this case the flow into or out of a well is controlled by
                     equations expressed in radial form such as those presented in the next four chapters.
                     The radial cell geometry is shown in fig. 5.1 and initially the following simplifying
                     assumptions will be made.

                     a)   The reservoir is considered homogeneous in all rock properties and isotropic with
                           respect to permeability.

                     b)   The producing well is completed across the entire formation thickness thus
                           ensuring fully radial flow.

                     c)   The formation is completely saturated with a single fluid.
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