Page 59 - Geochemistry of Oil Field Waters
P. 59

TITRlMETRIC METHODS                                                   47


            add three drops of  ammonium molybdate solution, 0.5 g sodium fluoride (if
            iron is present), and 0.5 g potassium  iodide, mix until dissolved, and acidify
            with 15 ml  of  6N hydrochloric  acid.  Titrate with  0.OW sodium thiosulfate
            using starch indicator.  Disregard any return of  blue color after the endpoint.
            Record this titration for the bromide calculation.

            Calculations. Iodide: ml of Na, S2 O3 for sample - ml of Na, S2 O3 for blank =
            corrected ml of Na, S2 O3 :

              (ml x  N) Na2S203 x  21,150-
                                         - mg/l I-
                      ml sample
            Bromide: ml of Na2  S2 O3 for sample - ml of Na2 S2 O3 for blank = corrected
            ml of  Na2S203  :
              (ml x  N) Na,  S203 x  13.320
                      ml sample          - mg/l I-  x  0.63 = mg/l Br-
              The precision and accuracy of  the method  are about 3% and 676, respec-
            tively, of the amounts of bromide and iodide present.

            Oxygen

              The  solubility  of  a  gas varies  directly  with  pressure  and  inversely  with
            temperature  and  usually  is  reduced  by  the  presence  of  dissolved minerals.
            Most  petroleum-associated waters  contain  little  or  no  dissolved  oxygen  in
            situ at depth.  Knowledge of  the dissolved oxygen content of  waters that are
            to be reinjected  for waterflooding or disposal is needed to determine treat-
            ment required  to prevent corrosion. Instrumental and wet chemical methods
            (American Petroleum Institute, 1968) are available for the determination of
            dissolved  oxygen.  Instrumental  methods  usually  are  modifications  of  the
            rotating platinum electrode method (Marsh, 1951), but with them the residual
            current  (when no oxygen  is present) is difficult to determine. The modified
            Winkler method probably is the most accurate wet chemical method available
            (Watkins, 1954).
              In the Winkler method  for quantitatively determining dissolved oxygen in
            water,  a  glass-stoppered  bottle  is  completely  filled  with  the  water  to  be
            tested.  Manganous  sulfate  (MnS04  )  and  potassium  hydroxide  (KOH)  are
            added,  forming a precipitate  of  manganous hydroxide (Mn(OH), ) in accor-
            dance with the following reaction:

              MnS04 + 2KOH  + Mn  (OH),  + K2S04
              The  manganous  hydroxide  combines  with  the  oxygen  dissolved in  the
            water to form a higher oxide of  uncertain composition, assumed to be man-
            ganese hydroxide (MnO(OH), ), as follows:

              2Mn (OH),  + 0, + MnO (OH),
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