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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

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