Page 63 - Geochemistry of Oil Field Waters
P. 63

TITR IMETR IC METHODS                                                 51


            Reagents.  The necessary reagents are 0.05N sodium carbonate solution and
            phenolphthalein indicator solution.

            Procedure.  Collect the water sample in the same manner used  in taking the
            sample to be analyzed for dissolved oxygen. Pipet 100 ml of the water into a
            flask  and  add  five  drops  of  phenolphthalein  indicator.  If  the sample turns
            red,  no  free  carbon  dioxide  is  present;  if  it remains  colorless, titrate  the
            sample with the standard sodium carbonate solution to a red endpoint.

            Calcula tion :
              ml Na2 CO,  x N  x  22,000
                    ml sample          = mg/l C02

            Sulfide

              As  mentioned  above,  the  bacterial  reduction  of  sulfate  causes  some
            petroleum-associated  waters to contain appreciable concentrations of hydro-
            gen  sulfide. Knowledge of  the amount of  dissolved sulfide present is neces-
            sary for corrosion and water compatibility studies (Watkins, 1954).
              The following  method  depends upon the reduction of  iodine by the hy-
            drogen sulfide in the brine, as shown by the following equation:

              H2S+I2 +2HI+S

            Because of  the unstable nature of  the hydrogen sulfide in solution in waters
            and brines, the sulfide is not titrated directly.  To prevent the loss of  hydro-
            gen sulfide to the air, an excess of iodine solution is added, and the sample is
            back-titrated  with standard sodium thiosulfate solution, in accordance with
            the following equation:

              2Na2  S2 0, + I2 +. Na2 S4 O6 + 2NaI

              Experiments conducted by the US. Bureau of Mines indicate that residual
            reducing agents that cannot be removed by aeration or boiling are present in
            some oilfield  brines.  Brine from the Arbuckle (siliceous) Limestone forma-
            tion  originally  containing  96  mg/l  hydrogen  sulfide showed  such  residual
            reducing  agents  to  equal  9  mg/l  of  hydrogen  sulfide  after  air  has  been
            bubbled  through  the  brine  for  28  hours.  This  dropped  to  4  mg/l  after
            standing another 24 hours.  Further tests in which the hydrogen sulfide was
            driven  off  by  boiling  indicated  the  presence  of  5 mg/l residual  reducing
            agents. When the brine was neutralized with hydrochloric acid (using methyl
            orange  indicator) before  boiling,  residual  reducing agents  equal to 2  mg/l
            hydrogen sulfide remained.
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