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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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