Groundwater at Oak Ridge National Laboratory's Field Research Center
(FRC) is contaminated with U(VI) and Tc(VII), has pH values as low as 3.3, and
nitrate concentrations as high as 120 mM. The objective of this research was to
determine if in-situ bio-immobilization is a viable treatment alternative for this water.
A laboratory column packed with crushed limestone and bicarbonate was used
to model in-situ pH adjustment. Denitrification and metal reduction were modeled in
columns packed with FRC sediment with ethanol as the electron donor. Two
intermediate-scale physical models deployed in the field were packed with limestone
and sediment and were stimulated with ethanol to support denitrification, U(VI)
reduction, and Tc(VII) reduction of FRC groundwater.
The limestone/bicarbonate column maintained a pH of above 5 for nearly one
hundred pore volumes without significant loss in hydraulic conductivity. The high-nitrate
(~120 mM) column study provided rates of denitrification (~15.25 mM/day),
ethanol utilization (~13 mM/day), and technetium reduction (~120 pM/day) by
sediment microorganisms, but no uranium reduction was detected. Results of the low
nitrate (3 mM) column study indicate that once the pH of FRC water is adjusted to pH
~7 and nitrate is removed, uranium (~3 μM) and technetium (~500 pM) reduction
occurred with ethanol as the electron donor at rates of 0.5 μM/day and 57 pM/day.
Similar results were obtained in two intermediate-scale (~3 m long) physical
models. Data from the high-nitrate, low-pH model indicate that the pH was increased
and nitrate and technetium reduction were occurring. Decreased U(VI) concentrations
were measured in the presence of high nitrate concentrations. Thus, U(VI) precipitates
may form or sorption of U(VI) may occur near the inlet in the pH adjustment region.
The maximum pseudo-first order rates of reduction measured during the seventh week
of model operation were: nitrate at 0.76 day⁻¹, Tc(VII) at 0.28 day⁻¹, and U(VI) at 0.12
day⁻¹. Ethanol concentrations were reduced from ~180 mM to zero in ~10 days
during the seventh week of model operation. No Fe(II) production was measured.
Concentration data collected from the low nitrate, neutral pH model indicate
that nitrate, uranium, and technetium reduction were occurring, though the model had
been operational for only ~6 weeks. No Fe(II) production was detected but sulfate
reduction was occurring.
The results of the laboratory experiments and the performance of the
intermediate-scale physical models suggest that bio-immobilization is a viable
treatment alternative for the contaminated groundwater at the FRC. / Graduation date: 2004
| Identifer | oai:union.ndltd.org:ORGSU/oai:ir.library.oregonstate.edu:1957/30056 |
| Date | 01 December 2003 |
| Creators | Sapp, Mandy M. |
| Contributors | Istok, Johnathan D. |
| Source Sets | Oregon State University |
| Language | en_US |
| Detected Language | English |
| Type | Thesis/Dissertation |
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