Page 64 - Geochemistry of Oil Field Waters
P. 64

52                                        ANALYSIS OF OILFIELD WATERS


           Reagents.  The  necessary  reagents  are  potassium  iodide,  standard  sodium
            thiosulfate, 0.1N and 0.01N; standard iodine solutions, 0.1N and 0.01N; and
            starch indicator solution.

           Procedure.  Collect  the  sample  in  a  glass-stoppered  bottle  (approximately
            200-mi  capacity) in  the  manner previously described  for dissolved oxygen.
            Analysis should be made as soon as possible after sampling.
              Pipet  5 ml of 0.1N or 0.01N standard iodine solution, depending upon the
           hydrogen  sulfide  concentration  expected,  into  each  of  two  Erlenmeyer
           flasks. It may  be necessary to use a larger quantity of  0.01N solution if  the
           hydrogen-sulfide content of the sample is high.
              Add  approximately  1 g  of  potassium  iodide crystals to each flask.  (This
           step usually may be omitted in determinations on brine samples because of
           the high  mineral content of  the water.)  Add  50 ml of  distilled  water to the
           flask  to be  used  for  a  blank  determination,  and  pipet  50 ml of  the water
           sample  into the  other  flask.  Titrate  both the distilled  water  blank and the
           water sample with  standard sodium thiosulfate solution of  the same normal-
           ity as the iodine solution used, adding 1 ml of starch indicator near the end
           of  the  titration.  Record  the milliliters of  thiosulfate used in each  titration.

           Calculation.  Subtract  the  milliliters  of  thiosulfate  solution  used  for  the
           sample from the milliliters used  for the blank  and use the difference in the
           following formula:
              (ml x  N) I2 - (ml x N) Na2S203 x  17,000
                             ml sample                = mg/l H2 S




           Sulfur compounds
              The  redox  potential  of  petroleum-associated waters indicates that sulfur
           compounds  other  than  sulfate and sulfide may exist in solution. When the
           water is brought to the land surface, the change in pressure and temperature
           will  affect  the redox  potential  and,  if  the sample  is allowed to come into
           contact with the atmosphere, the equilibria of the sample will start to change
           immediately.  Better  methods are needed  to determine the composition of a
           water  in  situ.  The following method  can  be used to gain a semiqualitative
           estimation of the amomts of thiosulfate, sulfite, and sulfide in a water.

           Reagents.  Zinc  carbonate  suspension:  add  zinc  acetate  to  a  solution  of
           sodium  carbonate,  filter  and  wash  the  precipitate  with  several volumes of
           cold  water.  Prepare the zinc carbonate suspension by vigorously shaking the
           precipitate with water.
              The other reagents are glycerol iodine, 0.01N; sodium thiosulfate,  0.01N;
           starch indicator solution; glacial acetic acid; and formaldehyde.
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