Page 19 - Geochemistry of Oil Field Waters
P. 19

8                               SAMPLING SUBSURFACE OILFIELD WATERS


            TABLE 2.1
            Changes in the composition of  petroleum-associated waters (mg/l)

            Constituent   Well  1             Well  2            Well 3
                          1947      1957      1947     1957      1956      1959

            Sodium and
            potassium     29,062    25,000     46,038   45,924  1,491       856
            Magnesium      1,100     1,200      2,011    2,200      30        2
            Calcium        5,900     5,500     14,200   14,400      60       10
            Bicarbonate       34        12        24        12     600     1,800
            Sulfate           14        50         3        52     200        0
            Chloride      58,500    51,800    102,100  102,800  2,000       300

            Total dissolved
            solids        94,610    83,562    164,376  165,388  4,381      2,968
                           ~-            _. -

              There is a tendency for some petroleum-associated waters to become more
            dilute  as the oil  reservoir  is  produced.  Such  dilution  may  result  from the
            movement  of  dilute  water  from  adjacent  compacting  clay  beds  into the
            petroleum  reservoir  as  pressure  declines  with  the continued removal of  oil
            and brine (Wallace, 1969).
              The composition  of  petroleum-associated water  varies  with the position
            within the geologic structure from which it is obtained. For example, if  the
            water table is tilted, the more dilute water probably will be on the structural-
            ly  high  side.  In  some  cases  the  salinity  will  increase  upstructure  to  a
            maximum  at the point  of  oil-water  contact.  Usually  this is caused  by  in-
            filtrating meteoric waters.
              Few  of  the samples  collected  by  drill-stem test  are truly  representative
           formation-water  samples.  During  drilling,  the pressure  in  the well  bore  is
           intentionally  maintained  higher  than  that  in  the formations.  Filtrate  from
           the drilling mud seeps into the permeable strata, and this filtrate is the first
            liquid to enter the test tool.
              The most truly representative formation-water sample usually is obtained
           after the oil well has produced  for a period of time and all extraneous fluids
           adjacent to the wellbore have been  flushed out.  Samples taken immediately
           after  the  well  is  completed  may  be contaminated with drilling muds,  with
            drilling  fluids,  and/or  with  well  completion  fluids,  such  as  filtrate  from
            cement, tracing fluids, and acids, which contain many different chemicals.

            Drill-stem test

              The  drill-stem  test,  if  properly  made,  can  provide  a  reliable  formation
           water sample. Mud  filtrate will be the first fluid to enter the drill-stem test
           tool, and it will be found at the top of the fluid column immediately below
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