Page 343 - Advances in Renewable Energies and Power Technologies
P. 343

316    CHAPTER 9 Design Principles of Photovoltaic Irrigation Systems




                         required by the distribution system to supply a discharge Q can be decomposed into
                         the following components:

                                                   H ¼ Dz þ hf þ h                     (9.17)
                         where Dz is a constant value that represents the elevation change from the reservoir
                         to the most restricted point in the irrigation subunits (in meters), hf is the estimated
                         head losses in the network path between the head of the system and the most
                         restricted point (in meters), and h is the average pressure head of the emitters of
                         the system (in meters). If the system is composed of several heterogeneous irrigation
                         subunits, a different system curve should be calculated for each irrigation subunit. If
                         the irrigation subunits are relatively homogeneous, the system curve can be valid for
                         all of them. Head losses in this simplified system scheme will able to be calculated
                         by using a general head loss equation as a function of the pump discharge, as
                         explained in Eq. (9.13).
                            The discharge in a noncompensating emitter varies according to its working
                         pressure. The relationship between these two variables is given by the discharge
                         equation of the emitter [50]:
                                                       q ¼ kh x                        (9.18)
                         where k is the emitter discharge coefficient, which is a constant dependent on the
                         unit system used, h is the working pressure head at the emitter (in meters), x is
                         the emitter discharge exponent (nondimensional), and q is the discharge of the
                         emitter. Conventional labyrinth-type emitters usually work in a turbulent regime;
                         therefore the value of their exponent is close to 0.5. In the simplified irrigation
                         scheme proposed, an average h value is considered and the hydraulic variability
                         in the irrigation unit is neglected.
                            The total discharge in the irrigation system can be calculated by multiplying the
                         number of emitters in operation by their average discharge, which can be calculated
                         with Eq. (9.19).
                                                                  x
                                                  Q ¼ q$n e ¼ n e $k$h                 (9.19)
                         Solving for the pressure head in Eq. (9.19), the average pressure at the emitters can
                         be expressed as a function of the total discharge of the system.
                                                          2
                                                      1      2      2
                                                h ¼        Q ¼ K$Q                     (9.20)
                                                     n e k
                         And finally, substituting h in Eq. (9.17), the following equation for the system curve
                         can be derived:

                                                 H ¼ Dz þðR s þ KÞ$Q 2                 (9.21)
                            Having identified the system curve (Eq. 9.21), the generalized H-Q performance
                         curve of the pump (Eq. 9.11), and the incoming power for the PV plant (Eq. 9.16),
                         the output frequency of the converter and the head and discharge of the pumping
   338   339   340   341   342   343   344   345   346   347   348