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

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6<br />

4<br />

.-<br />

h<br />

.L<br />

n<br />

*I 2<br />

n<br />

.<br />

:I%<br />

MATCH PARAMETERS<br />

AP = 1.0 psi<br />

t<br />

= 1.0hr<br />

PO = 0.09<br />

- !dC, -730<br />

CDe2s = 3000<br />

P'<br />

= 153.2 psia<br />

0<br />

+ DATA<br />

- SIMULATION<br />

-2<br />

0 1 2 3<br />

DIMENSIONLESS SUPERPOSITION FUNCTION: FLOW PERIOD 7<br />

Figure 5-39. H-1 5/Culebra Second Buildup Dimensionless Horner Plot with INTERPRET Simulation<br />

Figure 5-40 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> 0.10 ftz/day<br />

(Table 5-3), which is in reasonable agreement with<br />

the FBU and SBU results. The best slug-test fit was<br />

obtained by assuming that the pressure was<br />

recovering to a static value <strong>of</strong> 160.0 psia, indicating<br />

the continuing influence <strong>of</strong> the underpressure skin<br />

after the SBU.<br />

5.2.2.7 H-16. Testing <strong>of</strong> the Culebra at H-16 was<br />

planned to provide transmissivity data necessary to<br />

model the response <strong>of</strong> the Culebra to the<br />

construction <strong>of</strong> the Air-Intake Shaft at the WIPP. The<br />

Culebra lies from 702.5 to 724.4 ft deep at H-16<br />

(Figure 3-8). The interval tested extended from<br />

696.5 ft to the then-bottom <strong>of</strong> the hole at 733.9 ft.<br />

Thus, in addition to the Culebra, the lower 6 ft <strong>of</strong> the<br />

Tamarisk and the upper 9.5 ft <strong>of</strong> the unnamed lower<br />

member were tested. With the exception <strong>of</strong> the<br />

lower 2.9 ft <strong>of</strong> the Tamarisk, these overlying and<br />

underlying intervals are composed <strong>of</strong> gypsum and<br />

claystone, respectively, and were not considered to<br />

have contributed significantly to the transmissivity<br />

measured during the Culebra testing. The lower<br />

2.9 ft <strong>of</strong> the Tamarisk is composed <strong>of</strong> claystone,<br />

siltstone, and sandstone, and may have hydraulic<br />

properties similar to those <strong>of</strong> the underlying Culebra.<br />

Hydrologically, the Culebra and the lower Tamarisk<br />

probably behave as a single unit.<br />

All <strong>of</strong> the Culebra testing was performed on August<br />

7, <strong>1987</strong>, the day after the Culebra was cored. The<br />

testing consisted <strong>of</strong> two DST flow periods, two<br />

buildup periods, and a rising-head slug test<br />

(Figure 5-41). The FFL lasted about 17 minutes, and<br />

was followed by a 161-minute FEU. The SFL lasted<br />

about 24 minutes, and was followed by a 208-minute<br />

SBU. For analyses <strong>of</strong> the buildup data, the FFL was<br />

divided into two flow periods with rates <strong>of</strong> 0.731 and<br />

0.500 gpm, and the SFL was divided into two flow<br />

periods with rates <strong>of</strong> 0.818 and 0.512 gpm<br />

(Table 5-1). The slug test lasted 162 minutes, by<br />

which time 93% <strong>of</strong> the induced pressure differential<br />

had dissipated. The data from these tests are<br />

presented in Stensrud et al. (1988).<br />

77

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