Page 196 - Radiochemistry and nuclear chemistry
P. 196

180                  Radiochemistry and Nuclear Chemistry


                                            H.  +  0 2 ~  .HO 2
                                       9 HO 2  +  Fe 2+~FO 3+  +  HO 2-


                                          HO 2-  +  H +-~H20 2
                                   H202  +  Fe 2+  ~  Fe 3+  +  OH-  +  .OH

                                        9 OH  +  Fe 2 +  --~ Fe 3 +  +  OH-


               The yield of Fe 3+  is given by the equation

                      G(Fe 3+)  =  2G(H202)  +  3[G(eaq- )  +  G(.H)  +  G(.HO2)]  +  G(.OH)   (7.12)

               Figure 7.7 shows radiation yields for oxidation of Fe 2 + in acidic solution as a function of
               the LET value (see also  w
                When the concentration of the aqueous solution is greater than  ~. 0.1  M, the solutes may
               undergo direct radiolysis.  The products of the radiolysis of the solute can react with water
               itself or with  the radiolytic  products of water.  Irradiation of solutions  containing  sulfate,
               sulfite,  or  sulfide  ions  with fast  neutrons  yields  radioactive  phosphorus,  through  the
               32S(n,p)32p  reaction,  almost  exclusively  as  orthophosphate.  However,  depending  on  the
               redox  conditions  of  the  solution,  reduced  species  of  phosphorus  also  appear  in  minor
               amounts.  Somewhat in  contrast  to this,  slow neutron  irradiation  of solutions  of NaHPO 4
               yields phosphorus in many different oxidation states;  thus P( + 1), P( + 3) and P( + 5) appear
               in species such as hypophosphite,  phosphite,  and o-phosphate.  These species are all rather
               stable in aqueous solutions, and have been identified through paper r   analysis.
               In  general,  it  may  be  assumed  that  slow  neutron  irradiation  of  solutions  of  oxyanions
               changes  the  central  atom  to  another  (usually  a  more  reduced)  valence  state  through
               n,y-reactions.  For example,  while manganese is in the Mn(+ 7) state in MnO4-,  neutron
               capture leads to the formation of 56Mn2 +  species.  However, if the product valence state is
               unstable  at ambient  solution  conditions,  it may be immediately  oxidized to a more  stable
               higher valence state.
                The  self radiolysis  of  a  solution  may  change  the  chemical  equilibria  of  the  solution
               components.  For  example,  the  c~-decay of  plutonium  decomposes  water;  in  a  solution
               containing  1 mole of 239pu, ca.  0.01  mole of H202  is produced  per day.  This  hydrogen
               peroxide can react with the plutonium to form a precipitate of plutonium peroxide. To avoid
               this precipitation,  nitrite ions are added to the solution  to react with the hydroxyl radicals
               formed by the radiolysis and to eliminate the H202.


                                         7.8.  Organic compounds

                As discussed above, the chemical consequences of radiolysis depends on the physical state
               and  the  molecular  composition  of the  irradiated  material.  Two  properties,  the  dielectric
               constant and the electron mobility, are of great importance for the fate of the ion pairs (the
               radical  cations  and  the electrons)  formed on ionization.
   191   192   193   194   195   196   197   198   199   200   201