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Methods for Structural and Chemical Characterization of Nanomaterials  109



                                                        Anatase
                  A/B
                                                        Rutile
                                                        Brookite


          Intensity  R



                          B
                   B                               A       R/B
                                  R  A                     A A
                                         R
                                   A A B   B    B    B         R B
                                             R
          20      25     30     35     40     45      50     55     60
                            2 Theta (degree) (Cu Kα source)
        Figure 4.2  Theoretical X-ray diffraction patterns of the three polymorphs of TiO 2
        particles. A: anatase, B: Brookite, R: Rutile.



        same chemical composition, but different crystal structures). One of the
        best examples for illustrating this point is titanium dioxide (TiO ). Due
                                                                   2
        to the unique physical and chemical properties of TiO , it is widely used
                                                         2
        in industrial applications, particularly as a photocatalyst. Three dif-
        ferent TiO polymorphs exist—rutile, anatase, and brookite—however,
                  2
        only anatase is generally accepted to have significant photocatalytic
        activity. The respective XRD diffraction patterns of the three TiO poly-
                                                                    2
        morphs (Figure 4.2) represent a simple and easy way to distinguish
        between them based on peak location and height.
          Limitations. One of the main limitations of XRD when characterizing
        nanoparticles is that if the amorphization  process occurs without chang-
        ing particle size, it will affect both the intensity and diffraction peak
        width in the same fashion. Moreover, in certain cases the position of the
        peaks for different minerals can overlap, leading to ambiguous identi-
        fication of mineral phases. Because peak width increases with decreas-
        ing particle size, the overlapping of peaks is particularly problematic for
        very small particles.

          Total scattering. XRD is used to probe the periodic structure of miner-
        als (periodicity over distances above 100 Å), but a method has been
        recently “rediscovered” as a result of synchrotron light sources. This
        technique is based on the total scattering of particles and is called the
        pair distribution function (PDF). This method essentially fills the gap
        between XAS (see below) and XRD. The PDF technique has long been
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