Page 36 - Inorganic Mass Spectrometry : Fundamentals and Applications
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26                                                          Smith


      preparation, elimination of contamination, and calibration of the mass spectrome-
      ter all need to be meticulously addressed. All sources of bias must be identified
      and corrected. This often requires making synthetic mixtures of chemically pure
      and isotopically pure (as nearly as possible) enriched isotopes. Very few laborato-
      ries have the interest, the ability, and the support to perform such ~easurements.
      DeBievre and  Peiser have  described the  history  of,  and  some of  the  issues
      involved in, atomic weight ~easurements  [ 1041. Recent determi~ations of atomic
      weights using positive thermal ionization include those for tin [ 1051, europium
       [106], iron [10’7], antimony [108], and titanium [log]. This subject and others
       associated with metrology have been extensively treated in a review by De Laeter
      et al. [110].





       Thermal ionization mass spectrometry is an exceptionally valuable analytical tool.
       Its combinatio~ of  high precision and high sensitivity makes it applicable in a
       wide variety of situations in which isotopic ratios are sought. In conjunction with
       isotope dilution, it provides quantitative analyses that are usually of higher quality
       than those yielded by any other method.
           Isotope ratios provide insight into the physical and chemical processes that
       cause alteration of  their values.  Their application is  expanding as  analytical
       procedures become more sophisticated and sensitive, and as the extent  of scientific
       knowledge increases. As in many fields, much work done today would have been
       impossible a few years ago. With the advent of multicollector inductively coupled
       plasma  (ICP)  mass  spectrometers, it  is  probable that  routine use  of  thermal
       ionization will diminish, but it seems that it will always play a role in applications
       in which utmost sensitivity is required.





         1.  IUPAC  Com~ssion  on  Atomic  Weights  and Isotopic Abundances. Pure  Appl.

         2.  Faure, G. Principles of  Isotope Geology, 2nd Edition, John Wiley  & Sons, New
            York,  1986.
         3.  De Laeter, J. R. Mass. Spectrom. Rev. 1996, 15, 261.
         4.  Nusko, R.; Heurnann, K. G. Fresenius J. Anal. Chem. 1997, 357, 1050.
         5.  Eisenhut, S.; Heumann, K. G. Fresenius J. Anal. Chem. 1996, 354, 903.
         6.  Eagles, J.; Fairweathertait,  S. J.; Portwood, D. E.; Self, R.; Gotz, A,; Heumann, K. G.
            Anal. Chem. 1989, 61, 1023.
         7.  Gotz, A,; Heumann, K. G. Fresenius J. Anal. Chern, 1987, 326, 11 8.
         8.  Heumann, K. 6. Int. J. Mass Spectrorn. Ion Processes 1992, 118, 119, 575.
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