Page 137 - Geochemistry of Oil Field Waters
P. 137

Chapter 4.  INTERPRETATION  OF  CHEMICAL  ANALYSES  OF  OIL-
                        FIELD WATERS





              Water  analyses  may  be  used  to identify the source of  a  water.  In  the
           oilfield one of  the prime uses of these analyses is to determine the source of
           extraneous water  in  an  oil well, so  that casing can be set and cemented to
           prevent such  water  from flooding  the  oil  or  gas horizons. In some wells a
           leak  may  develop in  the  casing or cement, and water analyses are used to
           identify  the water-bearing horizon so that  the leaking area can be repaired.
           With  the present  emphasis on water pollution  prevention, it is very impor-
           tant to locate the source of  a polluting brine, so that remedial action can be
           taken.
              Comparisons of  water-analysis data are tedious and time-consuming; there-
           fore, graphical methods are commonly used for positive, rapid identification.
           A number of systems have been developed, all of which have some merit.

           Calculating probable compounds

              The hypothetical combinations of  dissolved constituents found in waters
           are commonly calculated by  combining the positive and negative radicals in
           the following order:
              calcium               bicarbonate
              magnesium             sulfate
              sodium                chloride
              potassium             nitrate

              Calcium  is  combined  with  bicarbonate,  and  if  more calcium is available
           than  that  consumed  by  bicarbonate,  it  is  combined with sulfate, chloride,
           and nitrate until exhausted. Conversely, any excess bicarbonate is combined
           with magnesium, sodium, and potassium until consumed. Other radicals can
           and  should  be  added  for  most  petroleum  reservoir waters.  These include
           lithium,  strontium,  barium,  iron, borate,  phosphate,  bromide,  and  iodide.
           They can be grouped in the appropriate column and then in the calculations
           each  positive and negative radical  is totally  combined,  the next  following
           radical  is combined until both the cations and anions are exhausted. If  the
           analysis is correct,  the cations and anions will be present in approximately
           equivalent amounts.
              To  calculate  the  hypothetical  combinations,  the reacting values  of  the
           positive  and  negative  radicals  or  ions  are calculated  as  follows:  reacting
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