2005 Salt Lake City Annual Meeting (October 16–19, 2005)

Paper No. 7
Presentation Time: 9:30 AM


CHRISTENSEN, John N., Center for Isotope Geochemistry, Lawrence Berkeley National Laboratory, MS 70A4418, 1 Cyclotron Road, Berkeley, CA 94720, DRESEL, P. Evan, Pacific Northwest National Lab, Richland, WA 99352, CONRAD, Mark E., Center for Isotope Geochemistry, Earth Science Division, Lawrence Berkeley National Lab, 1 Cyclotron RD, MS 70A-4418, Berkeley, CA 94720 and DEPAOLO, Donald J., Center for Isotope Geochemistry, Lawrence Berkeley National Lab, MS 70A4418, 1 Cyclotron Rd, Berkeley, CA 94720, jnchristensen@lbl.gov

Uranium from nuclear industrial activities covers a wide range of 235U/238U and 236U/238U due to variable combinations of isotopic enrichment and use in nuclear reactors. In addition, the irradiation of 232Th produces 233U and thus a signature separate from variable burn-up of different U fuel types. Natural background uranium in groundwater and porewater has essentially constant 235U/238U, virtually zero 236U/238U and 233U/238U, but variable 234U/238U due to alpha recoil effects. The contrasts in isotopic composition between natural and processed uranium, as well as the wide compositional range of processed uranium, provides the means to trace contaminant uranium in the environment and delineate the sources and history of contamination.

We have developed techniques of high precision measurement of uranium isotopes using an ICP source multiple collector magnetic sector mass spectrometer (MC-ICPMS) (IsoProbe, GV Instruments Ltd.). U isotopic compositions are measured simultaneously using a combination of Faraday cups (for 235U and 238U) and a Daly photomultiplier ion counting system (for 234U, 236U and 233U in separate measurements). U is separated from samples prior to introduction to the MC-ICPMS via a desolvation system. A single analysis of a 20ppb U solution uses ~10ng of sample U. We use bracketing analyses of a natural secular equilibrium U standard to correct instrumental mass fractionation, establish Daly/Faraday gain, and account for peak-tailing on 236U. This allows us to avoid the use of a 233U -236U double spike for mass fractionation correction that would compromise our ability to measure 236U and 233U. The lower limit for 236U/238U measurement is about 2x10-8. For 1ppb U in a water sample, this represents 5x107 atoms 236U per liter.

As demonstrations of our techniques we will present data from several ongoing studies at the Hanford Site, where decades of nuclear related activities have left significant local U contamination, including: (1) investigation of the connection between groundwater and vadose zone contamination in the B-BX-BY Waste Management Area (WMA) (Christensen et al. (2004) Env. Sci. Tech., 38:3330) (2) behavior of vadose zone U contamination in a core from the T WMA (3) sourcing, apportioning and tracing the contribution of the Hanford Site to the U flux of the Columbia River.