Page 119 - Geochemistry of Oil Field Waters
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COLORIMETRIC METHODS                                                  107





            where A = mg NaPO,  (heated sample), and B = mg NaPO,  (unheated sample).


            Precision. The precision is about k3% of the amount present.


            Silica

              Silicon is the second  most  abundant  element  in  the earth’s crust and is
            found  in  most  rocks  as the oxide  Si02 or  as a  silicate such as Mg,Si2O5
            (OH), . The solubilities of  silicate minerals in saline waters are a function of
            temperature,  pressure, pH, Eh, dissolved gases, and other ions in solution. A
            limited  amount  of  research  has  been  done concerning silicate solubilities
            (Collins, 1969) in saline solutions. Some investigators believe that most silica
            exists in solution as H4Si04 (White et al., 1956); others that it exists both in
            colloidal form  and as H4Si04 (Krauskopf, 1956). Hydration of  silica gives
            the following reaction:

              Si02 + 2H2 0 + Si(OH), or H4 Si04

              A  method  developed  by  Schrink  (1965) was used to study silicate solu-
            bilities in saline waters (Collins, 1969) and it gave satisfactory results. It also
            has  been  used  to analyze some petroleum-associated waters.  The method
            involves adding 1 ml of  a 4% ammonium molybdate solution in 0.75 molar
            sulfuric acid solution to an appropriate aliquot of  the water sample; add 15
            ml of  4.5N sulfuric acid; extract for 1 minute with ethyl acetate; and deter-
            mine  the  absorbance  of  the  ester  extract  with  a  spectrophotometer  at  a
            wavelength of  335 mp.


            Nitrate nitrogen
              Nitrate is the most highly oxidized form of  nitrogen and is the most stable
           form  in  an  oxidizing  environment.  Many  fertilizers  contain  nitrate,  and
           waters will  leach the nitrate  from  soil or rock. Most rocks do not contain
            much nitrate; therefore, it is unlikely that petroleum-associated waters con-
           tain appreciable quantities of  nitrate. The nitrate in deep waters also may be
           depleted through anion exchange (George and Hastings, 1951).
              Chloride is a serious interference in many of  the methods used to deter-
           mine nitrate nitrogen. Oxidizing or reducing agents such as ferric or ferrous
           iron also interfere. The Brucine method (Fisher et al.,  1958) can be applied
           to  a  petroleum-associated water.  To determine the nitrate  concentration,
           transfer  an  aliquot  of  the sample containing up  to 15 pg of  nitrate into a
            50-ml Erlenmeyer flask, add  15 ml of  water, 1 ml of  Brucine reagent (2%
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