Tc-99, U-236, and Np-237 in the Snake River Plain aquifer at the Idaho National Engineering and Environmental Laboratory, Idaho Falls, Idaho

Citation
Tm. Beasley et al., Tc-99, U-236, and Np-237 in the Snake River Plain aquifer at the Idaho National Engineering and Environmental Laboratory, Idaho Falls, Idaho, ENV SCI TEC, 32(24), 1998, pp. 3875-3881
Citations number
24
Categorie Soggetti
Environment/Ecology,"Environmental Engineering & Energy
Journal title
ENVIRONMENTAL SCIENCE & TECHNOLOGY
ISSN journal
0013936X → ACNP
Volume
32
Issue
24
Year of publication
1998
Pages
3875 - 3881
Database
ISI
SICI code
0013-936X(199812)32:24<3875:TUANIT>2.0.ZU;2-E
Abstract
The Idaho National Engineering and Environmental Laboratory (INEEL) is loca ted on the eastern Snake River Plain in southeastern Idaho; it is a multipu rpose complex operated by the U.S. Department of Energy. Among its installa tions is the Idaho Chemical Processing Plant (ICPP), a facility designed pr incipally to recover highly enriched uranium (greater than or equal to 93% U-235) from different nuclear fuel types used in naval propulsion, research , and test reactors. Starting in 1952 and continuing until 1984, low-level radioactive waste was discharged from the ICPP directly to the Snake River Plain aquifer by means of an injection well and seepage ponds. Over time, a suite of radionuclides have been measured in the aquifer including H-3, Cl -36, Sr-90, Cs-137, I-129, and Pu isotopes. Reported here are the first mea surements of the long-lived radionuclides Tc-99, U-236, and Np-237 in the a quifer and their downgradient concentration changes during water transport through fractured basalt. Like Cl-36, 99Tc behaves conservatively during tr ansport while I-129, U-236, and Np-237 indicate retardation.