Page 313 - Book Hosokawa Nanoparticle Technology Handbook
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FUNDAMENTALS                            CH. 5 CHARACTERIZATION METHODS FOR NANOSTRUCTURE OF MATERIALS
                  a Michelson interferometer and the obtained interfer-  The K–M function is proportional to the sample
                  ence signals are subjected to Fourier transformation.   concentration if the absorptive power of the sample is
                                                                 low and the scattering coefficient is constant for all
                    5.3.3.2 Observation of the powder surface    particles constituting the sample. Because the K–M
                  If light is applied to a powder sample, complex opti-  function can also be affected by the particle size,
                  cal paths will be generated by transmission, scatter-  shape, filling structure, and so on, these parameters
                  ing, reflection, and so on.  With this in mind, the  need to be kept constant when this function is used for
                  method of measurement needs to be changed depend-  quantitative analysis. However, concerning the nano-
                  ing on which of these optical paths is to be utilized  sized particles, it is difficult to keep these parameters
                  and addressed, and transmission and diffuse reflection  constant in a highly reproducible manner, and particu-
                  methods are often used for this purpose.       lar care is needed when the peaks are compared. Other
                    With the transmission method, the light transmitted  methods available include reflection absorption spec-
                  through a disk-shaped sample is measured with the  troscopy, photoacoustic spectroscopy, and so on [3].
                  latter usually prepared by pressure forming. If disk  Fig. 5.3.16 shows the DRIFT spectra for nanosized
                  forming is difficult, alternative methods available are  silica particles prepared by different methods. One type
                  compressive forming with KBr and spraying of the  of silica was prepared in the liquid phase (precipitation
                                                                            2 –1
                  sample onto the IR ray-transmitting material board.  method, 160 m g , Nipsil, Tosoh Corporation), while
                    With the diffuse reflection method, i.e., diffuse  the other was synthesized in the gaseous phase (flame
                                                                            2 –1
                  reflectance IR Fourier transform spectroscopy  method, 300 m g , Aerosil, Nippon Aerosil Co., Ltd.).
                  (DRIFT), spectra are obtained by measuring the dif-  The sharp peak in the highest wave number region
                  fuse reflective light, which returns after diffusion  near 3,750 cm  1  can be attributed to an isolated SiOH
                  within the sample. If light is applied to the powder  group, while the slightly broad peak at about 3,660 cm  1
                  layer, it diffuses in various directions, while repeating  is attributable to the hydrogen-bonded SiOH group. The
                  reflection on the particle surface, as shown in   extensive absorption around 3,400–3,450 cm  1  is attrib-
                  Fig. 5.3.15, and is eventually released out of the sam-  utable to –OH vibration associated with physically
                  ple from the uppermost layer.                  adsorbed water. Qualitatively speaking, a larger amount
                    During this process, light is repeatedly transmitted  of the isolated SiOH group is formed by the flame
                  through the superficial layer of the particles. For this  method, which is explained by hydrolysis occurring at
                  reason, the diffuse reflective light contains information  high temperatures (1,000 C or higher).
                  about the IR absorptive property of the material in the  In the case of silica prepared by the precipitation
                  vicinity of the particle surface. In research related to  method, the amounts of the hydrogen-bonded SiOH
                  fine particles, this method is often used for identifica-  group and physically adsorbed water are large. In
                  tion of the surface and observation of adsorbed species.  practice, the water content was about 3 mass% for sil-
                  The Lambert–Beer’s rule is inapplicable to the data col-  ica prepared by the flame method and 6–9 mass% for
                  lected by DRIFT, and instead of it, the Kubelka–Munk  that prepared by the precipitation method respec-
                  equation (K–M equation) is used for such data [1, 2].  tively. As far as nanosized particles of metal oxides


                                         I
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                       D
                   D
                         R        D                                                     Precipitation method
                                          R  R      D
                                                                  Absorbance (Arb. Unit)  Flame method
                                                     O








                                                                  4000    3600   3200    2800   2400    2000
                                                                                           -1
                                                                                Wavenumber (cm )
                  Figure 5.3.15                                  Figure 5.3.16
                  Diffusion of light through powder layer.       Drift spectra of silica nanoparticles.

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