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324    CHAPTER 9 Design Principles of Photovoltaic Irrigation Systems




                         where the diffuse and direct components are:
                                                                                       (9.39)
                                                      I d ¼ r d H d
                                                   I b ¼ðrH   r d H d Þ                (9.40)

                         4.1.3.1 Irradiance on a Fixed or Tracked Collector Plane
                         To calculate the irradiance on a collector plane, direct, diffuse, and global irradiance
                         must be calculated on a horizontal surface every short period of time on a character-
                         istic day of each month. The following input parameters must be defined to perform
                         these calculations: Julian day, latitude, irradiation (H), and timer. The global irradi-
                         ance in a horizontal plane is the sum of direct irradiance and diffuse irradiance:
                            Then, both the direct and diffuse irradiance on the tilted PV modules must be
                                                                         !

                         calculated taking into account both the unit solar vector  s  and the unit vector
                         of the collector plane (n).

                         •  Direct irradiance received by the modules I bb : The most widely accepted
                            approach for estimating the direct daily radiation on a sloped surface considers
                            the geometric position of the Sun and the collector and is based on the hy-
                            pothesis of proportionality between the fractions of direct and extraterrestrial
                            radiation.
                                                            cos q
                                                    I bb ¼ I b $                       (9.41)
                                                            cos q Z


                         •  Diffuse irradiance received by the modules  I db : The estimation of this
                            parameter is based on the isotropic model, which assumes that the distribution
                            of the diffuse radiation is independent of the azimuth and the zenith angle;
                            therefore radiation from any point in the celestial hemisphere has the same
                            intensity.


                                                          1 þ cos b
                                                  I db ¼ I d                           (9.42)
                                                             2

                         •  Reflected irradiance received by the modules I rb : It is usually assumed that the
                            terrain behaves as a horizontal and infinite surface that reflects radiation in an
                            isotropic way.

                                                              1   cos b
                                              I rb ¼ðI d þ I b Þ$r$                    (9.43)
                                                                 2
                            where r is the albedo of the ground, which is highly variable and depends on the
                            soil type. A constant value (r ¼ 0.2) is supposed in many works.
                         •  Total irradiance received by the modules (I b ): It is the sum of the three radiation
                            components:

                                                                                       (9.44)
                                                  I b ¼ I bb þ I db þ I rb
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