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Optical Fibers and Optical Fiber Amplifiers

                                     Optical Fibers and Optical FIber Amplifiers  195

            To appreciate the role of water, we can start by examining a spec-
          trum of the air we breathe (Fig. 9.2). The transmittance spectrum of
          glass is similar to that of air. The fundamental absorption occurs at
          2730 nm. This wavelength has a frequency that corresponds exactly
          to the molecular vibration frequency of H 2 O. The first overtone, one
          octave higher, occurs at 1370 nm. Both of these absorption bands can
          be seen in Fig. 9.2. It is easy to detect the band at 1370 nm by taking
          a spectrum of a tungsten lightbulb on a moderately humid day. If you
          need to make measurements in this region on a humid day, you can
          get rid of the absorption by purging the spectrometer with dry nitro-
          gen gas. The high-transparency region around 1550 nm is a kind of is-
          land in between regions where the water absorption is high. In glass,
          this high-transparency region occurs at the same wavelength: 1550
          nm.
            The wavelength where minimum attenuation occurs is also influ-
          enced by scattering due to random fluctuations in the glass itself.
          Glass is amorphous. This means that the atoms of silicon and oxygen
          are not arranged in a regular periodic pattern. On the local molecular
          level each silicon atom is attached to two oxygen atoms, but the over-
          all network of SiO 2 molecules is irregular, as shown in Fig. 9.4. The
          fluctuations are frozen into the glass fiber during the fiber drawing
          process at high temperature. The SiO 2 molecules are about a thou-
          sand times smaller than the wavelength of visible light. Scattering or
          diffusion of light by objects much smaller than the wavelength is
          called Rayleigh scattering. This same phenomenon is responsible for
          the blue color of the sky. Rayleigh scattering strength depends in-



















                                    {      Optical Wavelength ( m)
                            Low-loss region
                         1.530  m <   < 1.700  m
          Figure 9.2. Transmittance of air as a function of wavelength. Note that most of the ab-
          sorption bands can be related to the presence of water and carbon dioxide. Note that
          the transmission is close to 100% at wavelengths around 1550 nm.

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