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Radiation Effects on Matter                   167

               elementary  constituents  and  also  combined  into  more  complex  polymeric  products.
               Radiation decomposition (radiolysis) of water caused evolution of hydrogen and oxygen gas
               and  formation  of  hydrogen  peroxide.  Conversely,  it  was  shown  that  water  could  be
               synthesized through irradiation of a mixture of H 2 and 0 2.  In  1911  S.  Lind  found that  1
               g  of  radium  exposed  to  air  resulted  in  the  production  of 0.7  g  of  ozone  per  hour.  By
               relating  this  radiation yieM to  the number of ions produced  by  the  amount of radiation,
               Lind initiated the quantitative treatment of radiation-induced changes.



                                           7.1. Energy transfer

                The chemical effects of radiation depends on the composition of matter and  the amount
               of energy deposited by the radiation.  In this section we consider only the energy transfer.
               For this purpose it is practical to divide high energy radiation into (1) charged particles (e-,
               e+,  a,  etc)  and  (2)  uncharged particles  (n)  and  electromagnetic  radiation  ('y).  The  latter
               produce  recoil  atomic  ions,  products  of  nuclear  reactions  and  electrons  as  charged
               secondary ionizing particles. The terms direct and indirect ionizing radiation are often used
               for (1)  and  (2)  respectively.
                The amount of energy imparted to matter in a given volume is

                                         Eim p  =  Ein  +  ]~Q-  Eou t               (7.1)

               where Ein is the energy (excluding mass energy) of the radiation entering the volume, Eou t
               is the energy of the radiation leaving the volume, ]~Q is the sum of all Q-values for nuclear
               transformation  that  have  occurred  in  the volume.  For a  beam of charged particles Ein  =
               Elan;  for "y-rays it is ET.  If no nuclear transformations occur,  ]~Q =  0.  For neutrons which
               are  captured  and  for  radionuclides  which decay  in  the absorber,  EQ  >  0;  in  the  case of
               radionuclides already present  in the absorber,  Ein  =  0.


               7.1.1.  Charged particles

                We learned in the previous chapter that the energy of charged particles is absorbed mainly
               through ionization and atomic excitation.  For positrons the annihilation process (at Eld n  ~.
               0) must be considered.  For electrons of high kinetic energy bremsstrahlung must be taken
               into account.  However,  in the following we simplify by neglecting annihilation and brems-
               strahlung processes.  The bremsstrahlung correction can be made with the aid of Figure 6.9
               which  gives  the  average  specific  energy  loss  of  electrons  through  ionization  and
               bremsstrahlung.
                It has been  found that the average energy w  for the formation of an ion pair in  gaseous
               material by charged particles is between 25 and 40 eV.  For the same absorbing material it
               is fairly independent of the type of radiation and the energy. Table 7.1  lists values of w in
               some gases. The ionization potentialsj of the gases are lower than the w-values and the rest
               of the energy, w-j,  must be used for excitation.  Since the excitation energies per atom are
               _<  5  eV,  several  excited  atoms  are  formed  for each  ion pair  formed.  While  it  is easy  to
               measure w in a gas, it is more difficult to obtain reliable values for liquids and solids. They
               also  differ  more  widely;  e.g.  w  is  1300  eV  per  ion  pair  in  hexane  (for  high  energy
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