Scientists at Pacific Northwest National
Laboratory believe a research project
using 35 newly drilled wells will help
explain the baffling behavior of uranium
contamination at Hanford.
A decade
ago, Hanford officials believed uranium
contamination at the nuclear reservation
just north of Richland along the
Columbia River was a problem that time
would solve.
After the most contaminated soil was
dug up and hauled to a landfill for
low-level radioactive waste in central
Hanford, they expected the
uranium-contaminated ground water below
it to naturally dissipate.
Instead, levels of contamination
remain at up to three times the drinking
water standard in the ground water.
"The plume here has been far more
persistent than expected," said John
Zachara, PNNL chief scientist who is
leading a team of experts in underground
geochemistry, hydrology and microbiology
on the research project.
They're hoping that with the array of
new wells equipped with sophisticated
monitoring devices they will be able to
get to the bottom of the mystery of how
uranium behaves deep underground.
"We're looking at some very
aggressive technology," said Mike
Thompson, Department of Energy
hydrogeologist.
With the $13 million research
project, scientists believe they will
learn more about how, where and when
uranium binds to the soil, moves with
the ground water, then binds with the
soil again, with some of it eventually
reaching the Columbia River.
Among the key issues are the daily
and seasonal fluctuations in the level
of the Columbia River, creating what
Thompson describes as a washing-machine
action in the uranium contamination.
Scientists want to know more about
how the different chemistry of the river
water and ground water from various
sources affects the uranium
contamination, how the ground water
moves and how thin layers of sediment in
the soil bind and release the uranium.
"Sites like these are complicated
scientifically and the action is below
ground where you can't look at it,"
Zachara said.
During World War II and the Cold War
when plutonium was made at Hanford for
the nation's nuclear weapons program,
the 300 Area just north of Richland was
used to make uranium into fuel for
reactors. As a byproduct of the process,
60 tons of dissolved uranium was
released into the ground in disposal
ponds and trenches in the 300 Area.
The vast majority of uranium
contamination was in the top 15 feet of
soil, which has been dug up, Thompson
said. But the lighter contamination
deeper in the soil appears to be acting
as a persistent and long-term source to
keep recontaminating the ground water
near the Columbia River.
This summer the national lab research
project began with the drilling of 35
wells 60 feet deep that form a triangle
centered on the location of the first
disposal pond used for the release of
uranium-contaminated water. Each side of
the triangular array of wells is about
65 yards long.
They're equipped with sensors that
can detect temperature and measure
electrical resistivity. That allows an
in-depth look at information such as the
consistency of underground soil and the
underground movement of water from
different sources -- rain, ground water
and river water.
The first use of the wells calls for
injecting tracers of salt and varying
temperatures into the ground to follow
their movement.
Later tests are proposed to include
reinjecting contaminated ground water
from the uranium plume to observe the
behavior of the uranium.
DOE's goal is to understand enough
about the properties of the 96 acres of
ground water contaminated with uranium
at the 300 Area to find ways to restore
it to drinking water quality.
Although the uranium enters the river
just upstream from the Richland city
water uptake, the river almost
immediately dilutes the contamination to
easily meet standards for drinking
water.
The research project is planned to be
completed in five years. It's being paid
for with a competitive grant the
national lab won in DOE's Field-Scale
Subsurface Research Challenge.