Page 162 - Fundamentals of Reservoir Engineering
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DARCY'S LAW AND APPLICATIONS                               101



                                        constant rate
                                       water injection
                                          q cc/sec







                                                                  sand
                                                           l                  mercury
                                                                   pack
                                                                            manometers       h 1







                              water collection                                         h
                             and measurement                                            2






                     Fig. 4.1   Schematic of Darcy's experimental equipment

                                  h − h     ∆ h
                             uK    1   2  = K                                                        (4.1)
                              =
                                    I       I
                     where

                           u    =     flow velocity in cm/sec, which is the total measured flow rate q cc/sec,
                                      divided by the cross-sectional area of the sand pack
                           ∆h   =     difference in manometric levels, cm (water equivalent)

                           I    =     total length of the sand pack, cm, and

                           K    =     constant.

                     Darcy's only variation in this experiment was to change the type of sand pack, which
                     had the effect of altering the value of the constant K; otherwise, all the experiments
                     were carried out with water and therefore, the effects of fluid density and viscosity on
                     the flow law were not investigated. In addition the iron cylinder was always maintained
                     in the vertical position.


                     Subsequently, others repeated Darcy's experiment under less restrictive conditions,
                     and one of the first things they did was to orientate the sand pack at different angles
                     with respect to the vertical, as shown in fig. 4.2. It was found, however, that irrespective
                     of the orientation of the sand pack, the difference in height, ∆h, was always the same
                     for a given flow rate. Thus Darcy's experimental law proved to be independent of the
                     direction of flow in the earth's gravitational field.
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