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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MATCH PARAMETERS<br />
-ip<br />
10 PSI<br />
150 t 1 Ohr<br />
PO 0.079<br />
FT<br />
ui<br />
a<br />
3<br />
cn<br />
130ikxk<br />
cn<br />
w<br />
a<br />
i r)n<br />
,<br />
i<br />
i<br />
i<br />
I + - *<br />
+ DATA<br />
- SIMULATION<br />
+PUMP OFF<br />
'lot<br />
to 5/6/83 1O:OO<br />
I I I<br />
100<br />
0 200 400 600 800 100<br />
ELAPSED TIME, hours<br />
Figure 5-79. DOE-l/Culebra Pumping Test Linear-Linear Sequence Plot with INTERPRET Simulation<br />
Drawdown responses probably related to the DOE-1<br />
pumping were noted at wells H-3, H-1, P-17, and<br />
possibly H-4 during routine water-level monitoring.<br />
Because these responses were not anticipated,<br />
however, no pre-test baseline water-level monitoring<br />
had been performed at these wells. Consequently,<br />
the presence or absence <strong>of</strong> pre-existing water-level<br />
trends and water levels precisely at the beginning <strong>of</strong><br />
DOE-1 pumping are not defined. In addition, well H-<br />
4c was being pumped for a tracer test during all<br />
phases <strong>of</strong> the DOE-1 pumping test, which may have<br />
influenced some <strong>of</strong> the water levels observed.<br />
Because <strong>of</strong> these uncertainties concerning the<br />
observed water-level data, the observation-well<br />
"responses" were not interpreted.<br />
5.2.2.22 Engle. The Engle well was pumped for a<br />
period <strong>of</strong> 165.5 hr beginning November 4, 1983, to<br />
collect water-quality samples. The pumping rate was<br />
held at a nearly constant 9.8 gpm for approximately<br />
the first 97 hr <strong>of</strong> pumping. Pressure-drawdown data<br />
collected over this period are amenable to<br />
interpretation. Recovery data were collected for only<br />
one hr after the pump was turned <strong>of</strong>f, producing<br />
nothing useable for interpretation. A more complete<br />
description <strong>of</strong> this test and the test data are<br />
contained in Stensrud et at. (<strong>1987</strong>).<br />
Figure 5-80 shows a log-log plot <strong>of</strong> the Engle<br />
drawdown data, along with simulations <strong>of</strong> the data<br />
generated by INTERPRET. Late-time scatter <strong>of</strong> the<br />
data, particularly <strong>of</strong> the pressure-derivative data, is<br />
probably related to pumping-rate fluctuations. The<br />
model used for the simulations is representative <strong>of</strong> a<br />
single-porosity medium with a transmissivity <strong>of</strong><br />
43 ftz/day (Table 5-3). Assuming a Culebra porosity<br />
<strong>of</strong> 20%, a total-system compressibility <strong>of</strong> 1.0 x<br />
10-5 psi-1, and a fluid viscosity <strong>of</strong> 1.0 cp, the skin<br />
factor for this simulation is about 4.2. A<br />
dimensionless Homer plot <strong>of</strong> the drawdown data,<br />
along with a simulation generated using the same<br />
model, is shown in Figure 5-81. Again, the<br />
simulation matches the test data well until the data<br />
scatter at late time, indicating that an appropriate<br />
model was selected.<br />
106