Beauheim 1987 - Waste Isolation Pilot Plant - U.S. Department of ...
Beauheim 1987 - Waste Isolation Pilot Plant - U.S. Department of ...
Beauheim 1987 - Waste Isolation Pilot Plant - U.S. Department of ...
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1.0<br />
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10-3 10-2 lo-’ 1 00<br />
ELAPSED TIME, hours<br />
10’ 102<br />
Figure 5-46. H-1 6/Culebra Slug-Test Plot<br />
at 735.0 ft. Thus, the lower 2.7 ft <strong>of</strong> the Tamarisk and<br />
the upper 3.6 ft <strong>of</strong> the unnamed lower member were<br />
tested along with the Culebra. These overlying and<br />
underlying intervals are composed <strong>of</strong> anhydrite,<br />
gypsum, and/or clay, and were not considered to<br />
have contributed significantly to the transmissivity<br />
measured during the Culebra testing.<br />
The H-17 Culebra testing was performed from<br />
October 9 to 12, <strong>1987</strong>. The testing consisted <strong>of</strong> two<br />
DST flow periods, two buildup periods, and a risinghead<br />
slug test (Figure 5-47). The FFL lasted about<br />
16 minutes, and was followed by a 449- minute FBU.<br />
The SFL lasted about 24 minutes, and was followed<br />
by a 939-minute SBU. To obtain constant flow rates<br />
for buildup analyses, the FFL was divided into two<br />
flow periods having rates <strong>of</strong> 0.368 and 0.259 gpm,<br />
and the SFL was divided into two flow periods having<br />
rates <strong>of</strong> 0.443 and 0.280 gpm (Table 5-1). The slug<br />
test lasted about 48 hr, by which time about 99% <strong>of</strong><br />
the induced pressure differential had dissipated.<br />
The data from these tests are presented in Stensrud<br />
et al. (1988).<br />
A log-log plot <strong>of</strong> the FBU data is presented in<br />
Figure 5-48, along with a simuiation generated by<br />
INTERPRFT. The simulation is representative <strong>of</strong> a<br />
single-porosity medium with a transmissivity <strong>of</strong><br />
0.21 ft*/day (Table 5-3). Assuming a Culebra porosity<br />
<strong>of</strong> 20%, a total-system compressibility <strong>of</strong> 1.0 x<br />
10-5 psi-’, and a fluid viscosity <strong>of</strong> 1.0 cp, the skin<br />
factor for this simulation is -1.5, indicating a<br />
moderately stimulated well. The decline in the<br />
pressure derivative at late time indicates the<br />
presence <strong>of</strong> an overpressure skin created during<br />
coring and reaming <strong>of</strong> the Culebra October 7 and 8,<br />
<strong>1987</strong>. The dimensionless Horner plot <strong>of</strong> the FBU<br />
data (Figure 5-49) also shows the effects <strong>of</strong> the<br />
overpressure skin as the data trend slightly upward<br />
at very late time towards a pressure lower than the<br />
145.5 psia specified as the static formation pressure<br />
for that simulation. In fact, the buildup pressure<br />
reached a maximum <strong>of</strong> 144.8 psia after 275 minutes<br />
<strong>of</strong> the FBU (Figure 5-47), and declined slightly<br />
thereafter. The data collected after the maximum<br />
pressure was reached are not included on the<br />
analysis plots.<br />
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