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

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Figure 5-61 WIPP-l8/Culebra Slug-Test Plot<br />

Figure 5-62 shows a semilog plot <strong>of</strong> the falling-head<br />

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

fit provides a transmissivity estimate <strong>of</strong> 0.60 ftz/day<br />

(Table 5-3).<br />

5.2.2.13 WIPP-21. To evaluate the transmissivity<br />

<strong>of</strong> the Culebra at WIPP-21, a falling-head slug test<br />

lasting approximately 120 hr was initiated on July 11,<br />

1986. The fluid-pressure data from this test are<br />

reported in Saulnier et al. (<strong>1987</strong>). About 99% <strong>of</strong> the<br />

induced pressure differential was dissipated during<br />

the test. Figure 5-63 shows a semilog plot <strong>of</strong> the<br />

falling-head slug-test data, along with the best-fit type<br />

curve. This fit provides a transmissivity estimate <strong>of</strong><br />

0.25 ftzlday Vable 5-3).<br />

5.2.2.14 WIPP-22. The transmissivity <strong>of</strong> the<br />

Culebra at WIPP-22 was also evaluated by<br />

performing a falling-head slug test. The test was<br />

initiated on June 19, 1986, and lasted approximately<br />

75 hr. The fluid-pressure data from this test are<br />

reported in Saulnier et at. (<strong>1987</strong>). About 98% <strong>of</strong> the<br />

induced pressure differential was dissipated during<br />

the test. Figure 5-64 shows a semilog plot <strong>of</strong> the<br />

falling-head slug-test data, along with the best-fit type<br />

curve. This fit provides a transmissivity estimate <strong>of</strong><br />

0.37 ftz/day (Table 5-3).<br />

5.2.2.15 WIPP-30. Mercer (1983) reported the<br />

transmissivity <strong>of</strong> the Culebra at WIPP-30 to be<br />

0.3 ft2/day, based on a slug test performed by the<br />

USGS in 1980 (Richey, <strong>1987</strong>). Verification <strong>of</strong> this<br />

value was considered warranted by two<br />

observations. First, WIPP-30 lies in an area where no<br />

halite is present beneath the Culebra in the unnamed<br />

lower member. At every other location where the<br />

Culebra has been tested and no halite is present in<br />

the unnamed member, the Culebra is fractured and<br />

has a transmissivity <strong>of</strong> at least 8 ft*/day (Mercer,<br />

1983, and this report). Second, water-level<br />

responses observed in WIPP-30 to pumping at WIPP-<br />

13, 3.5 miles away, have led to an interpreted<br />

apparent transmissivity <strong>of</strong> 28 ft2/day for the Culebra<br />

between WIPPSO and WIPP-13 (<strong>Beauheim</strong>, <strong>1987</strong>b).<br />

92

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