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 />
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