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Geoelectrochemistry and stream dispersion                              61









                                       irlil

                             N





           Fig. 2-39. The basic mode of the contact polarisation curve (CPC) field installation: 1- ore body;
           2-  borehole; 3-  compensation  resistor; 4-  electric current source; 5-  resistance  of  shunt; 6-
           potentiometer;  7-  recorder; A-  current electrode; B-  auxiliary  current  electrode; M-  measuring
           electrode; N- non-polarisable measuring (reference) electrode (reproduced with permission  from
           Ryss, 1983).


           other  pole,  electrode  B,  is  placed  in  the  host  rocks  beyond  the  ore  body.  Recording
           comprises  the  simultaneous  measurement  of current,  which  flows  across  the  ore  body
           surface,  and the  electrode  potential  of the  ore  body.  The  current  is  supplied  as  a  linear
           function of time.  In order to measure  electrode potential  of the  ore body,  one  measuring
           electrode,  M  is  positioned  inside  the  ore  body  and  another  measuring  electrode,  N,  is
           placed  in the host rocks directly  in contact  with the  ore body.  In practice  we  cannot put
           electrode  N  at  the  desired  point,  so  it  is  impossible  to  measure  directly  the  electrode
           potential of the ore body in the  field.  However Ryss (1969,  1973)  found that by putting
           another  measuring  electrode  on  the  ground  surface  in  the  host  rocks  beyond  the  ore
           body,  it  is  possible  to  eliminate  the  difference  between  the  measured  voltage  and  the
           electrode potential of the ore body by means  of the compensation method (Fig.  2-39).  In
           this case the difference of potentials AUMN between the two measuring electrodes is,

           AUMN =(a+~AU;


           where,  q~ is  the  electrode  potential  of the  ore  body (the  useful  signal),  and  )-".AUi is  the
           sum  of the  potential  differences  in  different  parts  of the  measuring  circuit  (in  the  ore
           body,  in  the  host  rocks  and  so  on)  which  comprises  the  disturbance.  Usually
            l yAu, I>>   and  this  does  not  allow  us  to  observe  the  polarisation  effects  without
           using a special technique  of potential  separation,  which is based on the  different natures
           of the potentials q~ and ~AUi.  Since q~ is produced by electrochemical  reactions,  whereas
           ~AUi  satisfies  Ohm's  law,  q~ is  a  non-linear  function  of current,  but  Y.AUi is  a  linear
           function.  This  difference  between  q~ and  ~AUi  is  used  in  CPC  for  elimination  of  the
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