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

被引:25
作者
Beasley, TM
Dixon, PR
Mann, LJ
机构
[1] US DOE, Environm Measurements Lab, New York, NY 10014 USA
[2] Univ Calif Los Alamos Natl Lab, Los Alamos, NM 87545 USA
关键词
D O I
10.1021/es980390d
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Idaho National Engineering and Environmental Laboratory (INEEL) is located on the eastern Snake River Plain in southeastern Idaho; it is a multipurpose complex operated by the U.S. Department of Energy. Among its installations is the Idaho Chemical Processing Plant (ICPP), a facility designed principally 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 measurements of the long-lived radionuclides Tc-99, U-236, and Np-237 in the aquifer and their downgradient concentration changes during water transport through fractured basalt. Like Cl-36, 99Tc behaves conservatively during transport while I-129, U-236, and Np-237 indicate retardation.
引用
收藏
页码:3875 / 3881
页数:7
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