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3.0
                                    2.5
                                    2.0
                                    1.5               W
                                    1.0
                                                                − ε
                                    0.5
                                    0.0
                                    -0.5
                                                                     −
                                    -1.0                            ε    ε 0
                                    -1.5
                                    -2.0
                                                               Region of anomalous
                                    -2.5
                                                                   dispersion
                                      0.0     0.5     1.0     1.5     2.0     2.5
                                                             ω/ω 0


                        Figure 4.4: Real and imaginary parts of permittivity for a single resonance model of a
                                                                                           2
                        dielectric with  /ω 0 = 0.2. Permittivity normalized by dividing by   0 (ω p /ω 0 ) .





                          The major characteristic of the dispersion relation (4.104) is the presence of one or
                        more resonances. Figure 4.4 shows a plot of a single resonance component, where we
                        have normalized the permittivity as
                                                                    1 − ¯ω 2
                                                           2                   ,
                                                           p            2
                                            (˜  (ω) −   0 )/(  0 ¯ω ) =
                                                                            2 ¯ 2
                                                                1 − ¯ω 2  + 4 ¯ω
                                                                     2 ¯ω  ¯
                                                           2                   ,
                                                           p            2
                                                                            2 ¯ 2
                                                −˜  (ω)/(  0 ¯ω ) =
                                                                1 − ¯ω 2  + 4 ¯ω
                                                       ¯
                        with ¯ω = ω/ω 0 , ¯ω p = ω p /ω 0 , and   =  /ω 0 . We see a distinct resonance centered at
                        ω = ω 0 . Approaching this resonance through frequencies less than ω 0 , we see that ˜
                                                               √
                        increases slowly until peaking at ωmax = ω 0 1 − 2 /ω 0 where it attains a value of
                                                              1     ¯ ω 2 p

                                                   ˜   max  =   0 +   0  .
                                                                       ¯
                                                                  ¯
                                                              4   (1 −  )
                        After peaking, ˜  undergoes a rapid decrease, passing through ˜  =   0 at ω = ω 0 , and


                        then continuing to decrease until reaching a minimum value of
                                                              1     ¯ ω 2 p
                                                   ˜      =   0 −   0
                                                    min       4   (1 +  )
                                                                       ¯
                                                                  ¯
                                    √

                        at ω min  = ω 0 1 + 2 /ω 0 .As ω continues to increase, ˜  again increases slowly toward


                        a final value of ˜  =   0 . The regions of slow variation of ˜  are called regions of normal

                        dispersion, while the region where ˜  decreases abruptly is called the region of anomalous
                        dispersion. Anomalous dispersion is unusual only in the sense that it occurs over a
                        narrower range of frequencies than normal dispersion.
                        © 2001 by CRC Press LLC
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