Kr. Campbell et al., MERCURY DISTRIBUTION IN POPLAR CREEK, OAK-RIDGE, TENNESSEE, USA, Environmental toxicology and chemistry, 17(7), 1998, pp. 1191-1198
As a result of the lithium-isotope separation process used in the prod
uction of thermonuclear fusion weapons during the mid-1950s and early
1960s, 150 t of mercury were released into Poplar Creek (via East Fork
Poplar Creek) in Oak Ridge, Tennessee, USA. This project was performe
d as part of a Comprehensive Environmental Response, Compensation, and
Liability Act (CERCLA) remedial investigation to define the nature an
d extent of mercury contamination in Poplar Creek. Ultraclean sampling
techniques and ultrasensitive analytical methods were used to determi
ne methylmercury and inorganic mercury concentrations in surface water
, sediment, and pore water from Poplar Creek. Total methylmercury and
inorganic mercury concentrations (0.08-0.7 ng/L and 0.4-560 ng/L, resp
ectively) in surface water from reaches downstream from the East Fork
Poplar Creek confluence were significantly higher (p < 0.05) than the
upstream reference reach (0.05-0.3 ng/L and 0.1-27 ng/L, respectively)
. Concentrations in surface water increased with distance downstream f
rom the source (East Fork Poplar Creek), which was opposite of expecte
d results. Sediment methylmercury and inorganic mercury concentrations
also increased with the distance downstream from the source and were
highest near the mouth of Poplar Creek (1.0-12 ng/g and 630-140,000 ng
/g, respectively). High concentrations in surface water and sediment n
ear the mouth of Poplar Creek appear to be a result of sediment deposi
tion and resuspension, apparently caused by the stronger Clinch River
current acting as a barrier and its backflow into Poplar Creek as a re
sult of hydropower operations.