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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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