Page 169 - Radiochemistry and nuclear chemistry
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Absorption of Nuclear Radiation                 153




























                                               CHEM. SHIFT
                                    FIG. 6.23.  ESCA spectrum of trifluoroacetate.

               emitted  from  the  sample)  is  referred  to  as  the X-ray fluorescence spectrum. It  contains
               lower energy radiation including  K~ radiation emitted by atoms of lower atomic number.
               The  height  of these  other  peaks  is  lower  because  of a  lower  reaction  cross-section  (Fig.
               6.24).  Figure 6.22(B)  illustrates an XFS  analysis of a biological  sample.
                X-ray  fluorescence  analysis using  vacuum tube sources  have become a  well-established
               analytical technique in the last decade.  Nuclear interest stems partly from the possibility of
               using radioactive sources for stimulating X-ray fluorescence in a sample. These sources can
               be classified  depending  on  the mode of production  of the X-rays:
                (i)  ~,-ray sources:  decay between closely located nuclear energy  levels,  e.g.  a  59.5  keV
               -y emitted in the a-decay  of  241  Am:  also  broad  spectrum  -y-sources like   125  I are used.
                (ii)  x-ray sources:  (a) radiation emitted in rearrangement of electron orbitals following or-
               or B-decay (primary X-rays),  e.g.  11.6-21.7  keV uranium L-X-rays from 23gU formed in
               the  c~-decay of 242pu,  or  41.3-47.3  keV  europium  K-X-rays  from  fl-decay  of  153Gd; (b)
               irradiation of a target with a-,  ~-,  or "y-radiation leading to ionization and excitation of the
               target atoms and  its de-excitation by X-ray emission.
                (iii)  Bremsstrahlung  sources,  e.g.  T  in titanium,  or  147pm in aluminum (Fig.  6.10).
                An  important  advantage  of  radioactive  X-ray  fluorescence  sources  is  that  very  small
               instruments  requiring  no  (X-ray)  high  voltage  or  current  can  be  designed  for  field
               applications.  Such  instruments  are used  in  geological  investigations  (bore holes,  mineral
               samples,  etc.),  in-line  mineral analysis (Zn,  Cu,  and other ores  in flotation cycles,  Ca in
               cement raw-material,  etc.),  on-line analysis of surface depositions (Zn on iron sheets,  Ag
               in photographic emulsions, etc.). Figure 6.22 shows fluorescent spectra obtained on bovine
               liver with three different excitation sources: (A) 4 MeV protons (PIXE),  (B) (conventional)
               molybdenum transmission  tube,  and  (C) radioactive 55Fe.
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