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Beauheim 1987 - Waste Isolation Pilot Plant - U.S. Department of ...

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The simulation is representative <strong>of</strong> a singleporosity<br />

medium with a transmissivity <strong>of</strong> 0.31 ftzfday<br />

(Table 5-3). Assuming a Culebra porosity <strong>of</strong> 20%, a<br />

total-system compressibility <strong>of</strong> 1 .O x 10-5 psi-1, and a<br />

fluid viscosity <strong>of</strong> 1.0 cp, the skin factor for this<br />

simulation is about -1.8. These values are in<br />

excellent agreement with the FBU results, and<br />

indicate possible slight well development during the<br />

DST's. Again, the decline in the pressure derivative<br />

in Figure 5-33 at late time shows the continuing<br />

influence <strong>of</strong> the overpressure skin on the data.<br />

Figure 5-34 shows a semilog plot <strong>of</strong> the rising-head<br />

slug-test data, along with the best-fit type curve. This<br />

fit provides a transmissivity estimate <strong>of</strong> 0.30 ftz/day<br />

(Table 5-3). which is in excellent agreement with the<br />

FBU and SBU results. This fit was achieved using a<br />

static formation pressure estimate <strong>of</strong> 90.0 psia,<br />

slightly below the pressure measured at the end <strong>of</strong><br />

the SBU. The transducer used for the DST's and<br />

slug test was set at a depth <strong>of</strong> 514.7 ft. The fluid in<br />

the hole during the testing had a specific gravity <strong>of</strong><br />

1.003, and the transducer measured an atmospheric<br />

pressure <strong>of</strong> 12.3 psia before testing began. Hence,<br />

90.0 psia at the transducer depth corresponds to a<br />

static formation pressure <strong>of</strong> about 96.5 psig at the<br />

midpoint <strong>of</strong> the Culebra about 558 ft deep.<br />

Conclusions: The Culebra is 26.5 ft thick at H-14.<br />

The transmissivity <strong>of</strong> the upper 5.8 ft is 0.10 ftZ/day,<br />

while that <strong>of</strong> the entire unit is 0.30 ftz/day. Hence, the<br />

average hydraulic conductivity <strong>of</strong> the upper 5.8 ft <strong>of</strong><br />

the Culebra appears to be about 1.8 times greater<br />

than that <strong>of</strong> the lower 20.7 ft. This difference does<br />

not represent a great degree <strong>of</strong> heterogeneity. Left<br />

unresolved by this testing is the distribution <strong>of</strong><br />

hydraulic conductivity within the Culebra on a finer<br />

scale, such as hydraulic-conductivity differences<br />

between those portions that are less competent and<br />

core quickly, and those that are more competent and<br />

core more slowly.<br />

1 .o<br />

0.9<br />

0.8<br />

0.7<br />

0.6<br />

0<br />

F<br />

I<br />

0.5<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

0.0<br />

I,-, = 295:17:3555<br />

10-3 10-2 lo-' 100<br />

ELAPSED TIME, hours<br />

10' 102<br />

Figure 5-34. H-I4/Culebra Slug-Test Plot<br />

73

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