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268   Chapter Twelve

          As an aside, note that this (300 K) is a reasonable value for the
        ambient temperature and that our result indicates that the earth and
        most things on it are strongly emitting at a wavelength of 10  m. This
        is the basis of the “see in the dark” FLIR systems which are sensitive
        to this spectral region; most such systems use germanium optics,
        which transmit well in the 8- to 14- m region (which also happens to
        be a good transmission window of the atmosphere). Thus there is no
        such thing as darkness if you can detect 10- m radiation.
          Suppose we wish to know the characteristics of this blackbody in the
        wavelength region between 4 and 5  m. We express these wavelengths
        in terms of 	 max as 4/9.66   0.414 and 5/9.66   0.518. From Fig. 12.6,
        the corresponding values of W 	 /W 	, max are 0.07 and 0.25; these values,
        multiplied by W 	, max   3.13   10  3  W cm  2   m  1  give us the spectral
        radiant emittances for these wavelengths
        At 4  m:
                          W   0.22   10   3  W cm  2   m  1

        At 5  m:
                          W   0.78   10   3  W cm  2   m  1

          Using the fraction scale across the top of the chart, we find that
        about 0.011 of the radiation is emitted below 5  m (rel. 	  0.518) and
        about 0.0015 below 4  m. Thus, approximately 1 percent of the total
        radiation (W TOT ), amounting to about 4   10  4  W/cm , is emitted in this
                                                        2
        spectral band. The radiance of the surface will be 4   10 /  W ster  1
                                                              4
        cm  2  in this spectral band. If the blackbody is a foot square, with an
                            2
        area of about 1000 cm , it will radiate about 0.4 W between 4 and 5  m
        into a hemisphere of 2  ster.
          Most thermal radiators are not perfect blackbodies. Many are what are
        called gray-bodies. A gray-body is one which emits radiation in exactly
        the same spectral distribution as a blackbody at the same temperature,
        but with reduced intensity. The total emissivity ( ) of a body is the ratio
        of its total radiant emittance to that of a perfect blackbody at the same
        temperature. Emissivity is thus a measure of the radiation and
        absorption efficiency of a body. For a perfect blackbody    1.0, and
        most laboratory standard blackbodies are within a percent or two of
        this value. The table of Fig. 12.7 lists the total emissivity for a number
        of common materials. Note that emissivity varies with both wave-
        length and with temperature.
          Radiation incident on a substance can be transmitted, reflected (or
        scattered), or absorbed. The transmitted, reflected, and absorbed frac-
        tions obviously must add up to 1.0. The absorbed fraction is the emis-
        sivity. Thus a material with either a high transmission or a high
        reflection must have a low emissivity.
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