Page 132 - Geochemistry of Oil Field Waters
P. 132

120                                       ANALYSIS OF OILFIELD WATERS


            the blank titration  (formation water) as 0% spent acid.  Draw a straight line
            from  this  point  through  the intersection  of  the 100% spent  acid  and the
            10.0-ml CDTA  lines as illustrated  in Fig.  3.12.  This procedure corrects for
            any Ca+’  or Mg+2 present in the dilution water.
              In cases where it is impossible to obtain formation water for the 0% spent
            acid,  a  reasonable  approximation  can  be  made  by  titrating  100 ml  of  the
            water used  for washing and dilution.  To this volume of  CDTA, add 1.3 ml.
            This value can then be used for the 0% spent acid point on the plot.


           Free HCl
              When  free  HC1 is indicated  (pH below  4), and it is to be determined, an
           additional sample is required.  Withdraw  1.0 ml of  clear sample. Start with
           step  3 and follow the procedure.  The free HC1 is determined by  the differ-
           ence of the two titrations:
              % free HC1= (A -B)  x  1.5
           where A  = ml standard CDTA to titrate  CaCO,  treated  sample, and B = ml
           standard CDTA to titrate sample.

           Acetic acid solutions

              Generally,  acetic  acid  solutions  are  mixtures  of  acetic  acid  and  HC1.




                       Example:  10% HCI  t  5%  acetic  acid
                             I ml =  7.0 ml  CDTA
                             I ml  formation  waler =  1.3  ml  CDTA
                             I ml  return  water = 4.2 ml  CDTA
                             I ml  CDTA = 9.0 mg  Ca
                             Return  canlains  51%  rpent  acid


















                                 ml,  CDTA
           Fig.  3.13. Graph for use in calculating the amount of spent mineral and organic acid in a
           water sample.
   127   128   129   130   131   132   133   134   135   136   137