Page 97 - Geochemical Remote Sensing of The Sub-Surface
P. 97

74                                                    O.F.  Putikov and B.  Wen

            I~                       1    ~ ,, ,3/;
                 ImIx
                 t'\               "-'  /    :


               j:~      ///-"
                9  "-[   \,   ...'/





            0%        %-1         %  -2  %,o
                            o.V
           Fig.  2-49.  Typical  shape  of natural  water  cathodic  polarograms:  TDS-  total  dissolved  solids  or
           salinity in gram/litre (g/l);  1- TDS>5" 2-  I<TDS<5; 3-  TDS<I  (reproduced with permission from
           Putikov,  1993).

              The DCPL mode polarogram  is stepped,  the  steps being termed polarographic  waves.
           The value of the step potential depends  upon the type of electrochemical reaction  and the
           composition  of  the  water.  The  corresponding  increase  in  current  depends  upon  the
           concentration  of  the  dissolved  component.  For  the  same  potentials  of  electrochemical
           reactions  in  PPL  polarograms  a  maximum  of  current,  Imax, is  determined.  This  has  a
           proportional  dependence  on  the  concentration  of  the  dissolved  component  that  reacts
           with  the  mercury-dropping  electrode  (WE).  A  negative  WE  potential  produces  a
           cathodic  polarogram,  whilst a positive  WE potential produces  an anodic polarogram.
              Several  polarographic  waves  that  correspond  to  current  increasing  at  the  potentials
           q~,, q92, %  and q~!~2o can be revealed on the cathodic polarogram (Fig.  2-49).  The  nature  of
           these waves corresponds  to the following  electrochemical reactions,


           (Pi"   02 +  2H + +  2e--+  H202
           (P2"   H202 +  2H + +  2e--+  2H20
           (03:   Me  2+ +  2e-  --+ Me ~
                   2H + +  2e--+  H21"
           (~H 20  "

              At the potentials  tot  and q)2 a two  stage reduction  of dissolved  gaseous  02  takes place.
           At the potential  %  the reduction  of heavy metal ions  Me 2+, such  as Fe 2+ or Mn 2§  occurs.
           The  potential  q~.:o  is the  threshold  for the  electrochemical  decomposition  of water  with
           the  release  of gaseous  hydrogen.  With  a  decrease  of salinity  there  is  an  increase  in  the
           shift  of  the  apparent  potentials  q~.~, ...,  q).2o of  the  electrochemical  reactions.  If  the
           salinity  is <5  g/1,  the  first polarographic  wave  of oxygen  at potential  q),  is  complicated
           by a polarographic  maximum of the first kind,  Im,x.
              On  anodic  polarograms  of chloride  water  (Fig.  2-50,  curve  1),  the  CI  polarographic
           wave  at the potential  q),  corresponds  to the  reaction  2C1- --+ C12'I" +  2e-, whilst on  anodic
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