Page 129 - Geochemistry of Oil Field Waters
P. 129

OTHER METHODS                                                        117


            magnesium. The  excess  of  equivalents per  million of  anions over cations is
            assumed  to  be  sodium  plus  potassium,  and  this  practice  includes all  the
            errors  of  the  analysis  plus  the undetermined  ions in the combined  sodium
            plus  potassium  value.  The  ions  are  converted  to milliequivalents  per  liter
            (me/l)  by  dividing  each  ion  concentration  (mg/l)  by  its  milliequivalent
            weight (mglme) to give the milliequivalents per liter for each ion determined.
            After  adding  the  milliequivalents  per  liter  for  both  the  anions  and  the
            cations, the difference is multiplied by  the milliequivalent weight of sodium
            to give the calculated milligrams per liter of  sodium.
            Procedure. The calculation method is demonstrated as follows:


              Anions:  chloride     (50,000 mg/1)/(35.5 mg/me)  =  1,410 me/l
                        sulfate     (1,290 mg/1)/(48.0 mg/me)  =     27 me/l
                        bicarbonate  (204 mg/1)/(61.0 mg/me)    =     3 me/l
              Total anions                                        1,440 me/l

              Cations:  calcium     (5,900 mg/1)/(20.0 mg/me)  =    295 me/l
                        magnesium  (2,000 mg/1)/(12.1 mg/me)  =     164 me/l
              Total cations                                         459 me/l

            Determination of sodium:
              (1,440 - 459 me/l) x  23.0 mg/me = 22,600 mg/l


            Dissolved solids

              The dissolved solids determination can be used to estimate the accuracy of
            the  resistivity  determination.  The  specific  gravity  determination,  and  the
            evaporation  method  can  be  used  to double  check  the calculated total dis-
            solved  solids.  Theoretically,  if  all  the  dissolved  solids are accurately deter-
            mined, their sum will equal the weight of  the residue left after evaporation
            of  the water.  The  dissolved solids include all the solid material in solution
            which  is  ionized,  or  which  is not  ionized  but  does  not include suspended
            material, colloids, or gases.
              The residue  method  involves evaporating a filtered sample to dryness fol-
            lowed  by  drying the residue  in an  oven  at 180°C for  1 hour. The cooled
            residue is weighed and the total dissolved solids are calculated; e.g.,  if  100 ml
            of  brine is evaporated and the residue weighs 3.0 g, then the dissolved solids
            equal  30,000  mg/l.  The  evaporation  method  is  subject  to  errors  when
            hygroscopic  material  such  as calcium  chloride is in the water,  as is usually
            the case in oilfield waters.
              The calculation method simply involves adding the sum of  all the analyzed
            constituents as follows:
   124   125   126   127   128   129   130   131   132   133   134