Page 40 - Radiochemistry and nuclear chemistry
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Nuclei,  Isotopes  and Isotope  Separation         29


               Because of the law of conservation  of energy

                                               EIp  --  Eki n
               and

                                                hv  =  kT                          (2.41)

               This development assumes that the vibrational energy is completely converted to fragment
               translational  energy.  This  assumption  is  not  always  valid  for  polyatomic  fragments,  in
               which internal excitation may occur. Introducing (2.41) into (2.38) and equaling (2.37) and
               (2.38)  yields

                                        k[A][BC]  =  kTh-I[ABC#]                   (2.42)

               It is assumed  that ABC # is in dynamic equilibrium with the reactants A and BC.  Thus

                                          [ABC#]/([A][BC])  =  k #                 (2.43)

               According  to  (2.17)

                                          k"  =  FABC"/( 'A FBc  )                 (2.44)

               which with  (2.42)  yields

                                        k  =  kT FABC./(h F A Fac  )                (2.45)


               This expression must be multiplied by a factor r,  which is the probability that the complex
               will  dissociate  into products  instead of back into  the reactants  as assumed in  (2.43).  The
               factor g  is called the transmission  coefficient.  The  final  rate expression  thus becomes:

                                       k  =  g k  TFABc#/(h F A FBC )               (2.46)

                As is  shown in  w   the grand partition  functions F i can be calculated from theory and
               spectroscopic  data;  because  these  functions  are  mass  dependent  k  is  mass  dependent.  In
               calculating  the Fi's,  all modes of energy must be included as well as the population of the
               different  energy states.
                For  isotopes  of  the  lighter  elements,  the  activation  energy  term  makes  the  main
               contribution to the reaction rate isotope effect, while for the heavier elements the vibrational
               frequency  causing  the decomposition  into  the products  plays  the larger role.  Because  the
               energy  states  usually  are  more  separated  for  the  isotopic  molecules  of the  products  and
               reactants than for the transition state,  isotope effects are usually larger in reaction kinetics
               than in equilibria.
                Studies  of kinetic  isotope  effects  are of considerable  theoretical  interest,  particularly  in
               organic chemistry.  The practical applications are still meager, but this will not necessarily
               be so in the future.  An example is the decrease in metabolic rate for 13C compounds, which
               has led to the suggestion of its use for treatment of certain diseases,  as e.g.  porphyria.
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