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

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1.0,<br />

0<br />

I<br />

0.9<br />

0.8<br />

0.7<br />

0.6<br />

0.5<br />

0.4<br />

MATCH PARAMETERS<br />

- p* = 141.30prig<br />

p, = 174.15prig<br />

B - 1.0<br />

t 2.15hr<br />

- rc* = 0.181 fl<br />

I I I I<br />

0.3<br />

0.2<br />

0.1<br />

'B<br />

0.0<br />

to = 170:10:05:00<br />

10-2 10" 100 10'<br />

ELAPSED TIME, hours<br />

102 103<br />

Figure 5-64. WIPP-22/Culebra Slug-Test Plot<br />

Evaluation <strong>of</strong> the Culebra transmissivity at WlPP-30<br />

was accomplished by performing two falling-head<br />

slug tests in December <strong>1987</strong>. The fluid-pressure<br />

data collected during these tests will be presented in<br />

Stensrud et al. (in preparation). The first test was<br />

initiated on December 10, <strong>1987</strong>, and lasted about<br />

28 hr, by which time almost 99% <strong>of</strong> the induced<br />

pressure differential had dissipated. A semilog plot<br />

<strong>of</strong> the data from this test is shown in Figure 5-65,<br />

along with the best-fit typecurve match. This match<br />

provides a transmissivity estimate for the Culebra at<br />

WIPP-30 <strong>of</strong> 0.18 ftz/day (Table 53), 40% lower than<br />

the value reported by Mercer (1983).<br />

The second test was initiated on December 15,<strong>1987</strong>,<br />

and lasted about 52 hr, allowing >99% <strong>of</strong> the induced<br />

pressure differential to dissipate. Figure 5-66 shows<br />

a semilog plot <strong>of</strong> the data from this test, along with<br />

the best-fit type-curve match. This match is very<br />

similar to that obtained for the first test, and provides<br />

a transmissivity estimate <strong>of</strong> 0.17 ft2/day (Table 5-3).<br />

The transmissivity values from both December <strong>1987</strong><br />

tests are in fair agreement with the original value<br />

reported by Mercer (1983) and, most importantly,<br />

confirm the observation <strong>of</strong> low Culebra transmissivity<br />

at WIPP-30. Reconciliation <strong>of</strong> this low transmissivity<br />

with the absence <strong>of</strong> halite in the unnamed lower<br />

member at WIPP-30 is discussed in Section 6.1.<br />

5.2.2.16 P-15. The transmissivity <strong>of</strong> the Culebra<br />

at P-15 was reported by Mercer (1983) to be<br />

0.07 ftzlday based on a bailing test performed by the<br />

USGS in 1977 (Mercer and Orr, 1979). Because this<br />

value is significantly lower than the transmissivity <strong>of</strong><br />

0.9 ftz/day reported by Mercer (1983) for H4b, the<br />

nearest other well, and because <strong>of</strong> limited well<br />

development before the bailing test, well<br />

development and retesting were performed in early<br />

<strong>1987</strong>. Fluid-pressure data collected during the well<br />

development and testing are reported in Stensrud et<br />

al. (1988).<br />

94

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