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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Two factors raised questions about these<br />
datafinterpretations. First, reported Culebra<br />
transmissivities are higher at holes northwest (P-l4),<br />
southwest (H-7), northeast (H-3, DOE-l), and east (H-<br />
11) <strong>of</strong> H-4 than at H-4. Second, early tests <strong>of</strong> the<br />
Culebra at well DOE-2 appeared to indicate the<br />
presence <strong>of</strong> a recharge boundary, which was later<br />
shown to be simply poor hydraulic communication<br />
between the well and the formation. Good hydraulic<br />
communication was established by acidizing DOE-2,<br />
and subsequent tests revealed a transmissivity<br />
higher than previously estimated (<strong>Beauheim</strong>, 1986).<br />
Hence, concern arose as to whether the reported<br />
Culebra properties for H-4 were real, or were affected<br />
by poor communication between the H-4 wells and<br />
the formation.<br />
To resolve this question, H-4c was acidized and a<br />
falling-head slug test was performed to evaluate<br />
whether or not the acidization had resulted in an<br />
increase in the apparent transmissivity <strong>of</strong> the<br />
Culebra. Well H-4c was selected as the test well<br />
1 .o<br />
because it is a cased hole with perforations providing<br />
access to the Culebra, similar to DOE-2. The well<br />
was acidized on July 16, 1986, by injecting nearly<br />
200 gallons <strong>of</strong> a 20% hydrochloric acid solution at the<br />
Culebra level over a period <strong>of</strong> about 2 hr. After a<br />
waiting period <strong>of</strong> over an hour, the spent acid was<br />
swabbed from the well. The well was then<br />
developed over a 7-day period by repeatedly<br />
pumping most <strong>of</strong> the water from the well and<br />
allowing the water level to recover (Stensrud et al.,<br />
<strong>1987</strong>).<br />
On July 31, 1986, a falling-head slug test was<br />
initiated in HAC. The test continued tor about 45 hr<br />
until August 2, 1986. The data from this test are<br />
reported in Stensrud et al. (<strong>1987</strong>). A plot <strong>of</strong> the test<br />
data and the best fit to a slug-test type curve are<br />
shown in Figure 5-20. The good fit between the data<br />
and the type curve indicates that on the scale <strong>of</strong> the<br />
test, the Culebra at H-4c behaves hydraulically as a<br />
single-porosity medium. No evidence <strong>of</strong> a recharge<br />
boundary is observed in the data.<br />
0.9<br />
0.8 p* = 59.47 psig<br />
pi 103.90 psig<br />
0.7<br />
0.6<br />
0<br />
T 0.5<br />
I<br />
0.4<br />
t<br />
= 1.2hr<br />
0.3<br />
0.2<br />
0.1<br />
0.0<br />
10'3 10-2 lo-' 100 10' 102<br />
ELAPSED TIME, hours<br />
Figure 5-20. H+c/Culebra Post-Acidiration Slug-Test Plot<br />
62