Page 238 - Inorganic Mass Spectrometry - Fundamentals and Applications
P. 238

224                                                         Smith


                                                                 et
            Institute of Science and  Technology  has  been  described  by  Bowers a1 [3]. A re-
            cent report describes  using  isotope  dilution  to calibrate analysis of  solid  samples
            using electrothermal vaporization  with  inductively  coupled  plasma  mass  spec-
            trometry  (ICP-MS) [4].
                 It is obvious  that, no matter  what  kind of mass  spectrometer or ionization
            method is used,  correction for isotopic bias is mandatory for successful  applica-
            tion of isotope dilution, The basis of the whole  technique rests on ~stwo~y
                                                                        meas-
            urement of the isotope dilution ratio [R,  in Eq. (5.7)], which  necessitates  applica-
            tion of a  bias  correction.  Accuracy of the final  result is critically  dependent  upon
            accurate  calibration of the inst~mentation, and,  as  always, it is important to have
            analysis of reference  materials  mimic  as  closely  as  possible  that of samples.





            An  absolutely essential step in isotope dilution is to achieve  equilibration of spike
                                                                       is
            and  sample.  The  spike is usually  added  as  a  solution  whose  concentration accu-
            rately  known; since many  samples  are  not  solutions,  chemical  processing is usu-
            ally  required  to  equilibrate  the  two.  This  invariably  involves  dissolving  the  sam-
            ple, not always  a  simple  task. The spike  solution is added to the  sarnple,  and  the
            two  are  thoroughly  mixed. ~quilibration for some  elements  requires  nothing  more
                                                                 like
            than  to  have  spike  and  sample  in  solution  together.  Some  elements, plutonium,
            have  a  multiplicity of oxidation  states  and  require  more effort; this  very  often in-
            cludes  drying the sample  and  redissolving it, and  adding  an  oxidizing or reducing
            agent to ensure that the target  element in both spike and sample assumes the same
            oxidation  state.  Once  equilibration is attained, it is unnecessary to achieve full re-
            covery of the  analyte  element  in  subsequent  chemical  processing,  one of the  big
            advantages of  isotope dilution.  Full  recovery  is not  required  because  chemical
            processes do not cause isotopic  fractionation, at least  to the degree  necessary to af-
            fect  results  significantly. This characteristic of isotope dilution is p~icularls ad-
            vantageous  when the sample is a  complex  matrix  such as vegetation, soil, or ani-
            mal  tissue. To exploit  this  attribute, the spike  should  be  added the sample  as  early
                                                            to
            in  the  chemical prep~ation process as possible.  For  example,  in  the  author's  lab-
            oratory the 233U spike is added to the platinum  dish cont~ning a  vegetation  sam-
            ple  whose  uranium  content is desired  before it is inserted into the muffle  furnace;
            the  spike is thus  introduced  before  any  chemical  processing has occurred.
                 Because  extensive  chemical  processing involved  in  using isotope dilution,
                                                is
            it is important to determine  the  level of the  process  blank  before  analyzing  sa-
            ples.  Although there are a  few  instances in which  doing so is unnecessary, the vast
            majority of problems  require it; it obviously  becomes  more  important  with  de-
            creasing  concentration of the analyte  element.  Many  elements  are  ubiquitous in
            nature  and  occur at some  level  in  virtually all reagents,  including  purified  water.
            In  numerous  applications the blank  level  rather  than  the ins~mentation determines
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