Page 134 - Inorganic Mass Spectrometry - Fundamentals and Applications
P. 134

124                                                         Olesik

                                                do
            concentrations  are  assigned  last  because  they not  have  a  unique  isotopic  pattern
            to aid  in  their  identification.  This  approach  was  used to reduce the computation
            time  that  would be necessary  to  solve  a  complete set of  simultaneous  equations
            and  to  deal  with  species  in  the  spectrum  that  might  not  be  anticipated  in  the  model.
                 Recently, a full multicompo~ent analysis  approach  for automated  semi-
            quantitative  survey  analysis  by  ICP-MS  has  been  described  [153,208,209].  The
            computing  power  of  personal  computers  (PCs)  has  increased  sufficiently  that
            modeling  a  matrix of 250  masses by 105  species  can be done  quickly  (about  10 sec
            on  a  100-MHz  Pentium  PC). A database of the  isotopic  patterns of all elemental
                                is
                                                                    the
            ions  and  interferent  ions used. The database  can  be  expanded  beyond current
            400  interferent  ions.  Elemental  and  polyatomic  ions  with  signals  below  the
            estimated  standard  deviations  in  the  total  measured intensities are  excluded  from
            the  model. To assess  which  elemental  and  polyatomic  ions  are  in  the  experimental
            spectrum  a relative standard  deviation  (RSD)  function  that  has  been  modeled  in
                                     is
            terms of source  and  shot  noise used  [208].  Diagnostics for goodness of  fit  of  the
            model  include  graphical  comparison of  mass  spectra  with  elemental  ion  or  inter-
            ferent  ion  spectra  and  precision for each  element or interferent  ion. The measured
            intensity at each isotope for a  given  elemental or polyatomic  ion is divided by the
            corresponding  natural  abundance  to  calculate  a  set
                                                    of element i~te~~ities. "he RSD
            of the  element  intensities is a  measure of the  quality of the model  fit. The precision
            information  can also be used  to  determine  true  detection  limits in  the  sample.
                 There are three potential  limitations of the MCA  approach.  If  the  signals at
            some  masses  (such  as mlz = 56) are  over range because of large  signals (ArO+,
            Fe+, andlor CaO+), it is more  difficult to assign  their  element  intensities  at other
            masses.  Monoisotopic  elements  have  more  uncertainty  because  there is no iso-
            topic  pattern  to  assess  the  model  fit. there  are  more  species  than  masses  over  a
                                          If
            region of  the  spectrum,  there  is not  a unique  solution.  For example, Cr+ may
            require  correction for Ti+, V+, Fe+, and ArO+.
                 Semiquantitative  analysis  procedures  have  also  been  used  with  laser  abla-
             tion  ICP-MS  [7 1,2 10-2 131. The effect of experimental  parameters  and  potential
            improvements in  accuracy of  semiquantitiative analysis using  ICP-
             also  been  discussed  recently  [208,214-2161,  along  with the use of se~qu~tita-
             tive analysis  with  a  double-focusing  ICP-MS  in  both  low-  and  high-resolution
             modes [2  171.







                  S is  used  for  elemental  analysis  of  every  type  of  sample  imaginable,
             including  gases, liquids, and  solids.  Element  concentrations  in  natural,  process,
             and  waste  waters;  biological  tissues,  hair,  and  fluids;  metalloproteins;  and  drugs
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