Page 146 - Design of Solar Thermal Power Plants
P. 146

3.2 HELIOSTAT FIELD EFFICIENCY ANALYSIS    131

              above parts. Thus in the power tower plant with concentrators
              located far away from the receiver, influences of atmospheric
              humidity on radiation transmission shall be considered. It is
              suggested not to build up large-scale power tower plants in areas
              with high atmospheric humidity.
           2. Molecule scattering. There is always the statistical deviation of
              partial density from the mean density in the atmosphere, which is
              known as the density fluctuation. It ruins the optical uniformity of
              the atmosphere; partial solar radiation light will transmit toward
              other directions, which leads to the scattering of the solar radiation
              in various directions.
                 In visible light and near-infrared wave regions, radiation
              wavelength is always much greater than molecular dimensions.
              Under such conditions, scattering is referred to as the Rayleigh
              scattering. The intensity of Rayleigh scattering light is inversely
              proportional to the biquadratic value of wavelength l. The empirical
              equation of Rayleigh scattering coefficient is:

                                   s m ¼ 0:827 NA 3    l 4              (3.6)

              in which N refers to the quantity of molecules within a unit volume,
                 3
                                                            2
              cm ; A refers to the molecular scattering section, cm ; l refers to the
              length of the optical wave, cm. The bigger of wavelength l, the
              weaker of the scattering effect; the smaller of l, the stronger of the
              scattering effect.
                 When encountering atmospheric molecules or aerosols particles,
              the optical wave will interact with them and once again emit the
              light (called wavelet) of the same frequency and less intensity with
              the incident light in all directions, which is referred to as the optical
              scattering. The wavelet is called the scattering radiation;
              atmospheric molecules and aerosol particles that receive the original
              incident light and emit wavelets are called scattering particle. When
              scales of scattering particles are much smaller than the wavelength
              of incident light (for example, scattering effect of atmospheric
              molecules on visible light), it is called molecular scattering or
              Rayleigh scattering, in which scattering lights have been distributed
              on an even and symmetric basis.
                 As molecular scattering is inversely proportional to the
              biquadratic value of wavelength, the bigger of the l, the weaker of
              the scattering effect; and the smaller of the l, the stronger of the
              scattering effect, scattering effect of visible light is stronger than that
              of infrared light, and scattering effect of blue light is stronger than
              that of red light. In a clear sky, other particles are insignificant in
              content; thus Rayleigh scattering has been playing a dominant role.
   141   142   143   144   145   146   147   148   149   150   151