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Published online 20 November 2007
Published in Vadose Zone J 6:1018-1030 (2007)
DOI: 10.2136/vzj2006.0158
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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SPECIAL SECTION: HANFORD SITE

Isotopic Studies of Contaminant Transport at the Hanford Site, Washington

John N. Christensena,*, Mark E. Conrada, Donald J. DePaoloa,b and P. Evan Dreselc

a Center for Isotope Geochemistry, Earth Sciences Division, E.O. Lawrence Berkeley National Lab., 1 Cyclotron Rd., Berkeley, CA 94720
b Dep. of Earth and Planetary Science, Univ. of California, Berkeley, CA 94720
c Pacific Northwest National Lab., Richland, WA 99353

* Corresponding author (jnchristensen{at}lbl.gov).

Received 1 November 2006.

Processes of fluid flow and chemical transport through the vadose zone can be characterized through the isotopic systematics of natural soils, minerals, pore fluids, and groundwater. In this contribution, we first review our research using measured isotopic variations, due both to natural and site-related processes, of the elements H, O, N, Sr, and U, to study the interconnection between vadose zone and groundwater contamination at the Hanford Site in south-central Washington State. We follow this brief review with a presentation of new data pertaining to vadose zone and groundwater contamination in the Waste Management Area (WMA) T-TX-TY vicinity. Uranium isotopic data for the C3832 core (WMA TX) indicate the involvement of processed natural U fuel and link the observed U contamination to releases near single-shelled tank TX-104. The data also preclude contamination from an early 1970s TX-107 leak. In the case of the C4104 core (WMA T), the U isotopic data indicate a mixture of processed natural and enriched U fuels consistent with the major leak from T-106 in 1973. Uranium and strontium isotopic data for the cores also provide direct evidence for chemical interaction between high-pH waste fluid and sediment. Isotopic data ({delta}15N and {delta}18O) for groundwater nitrate contamination in multidepth samples just to the northeast of WMA T are distinct from that seen in surrounding wells and suggest tank waste (possibly from the 1973 T-106 event) as a source of very high 99Tc concentrations recently observed at the northeast corner of WMA T.

Abbreviations: MC–ICPMS, multiple-collector inductively coupled plasma–mass spectrometer • WMA, Waste Management Area




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G. W. Gee, M. Oostrom, M. D. Freshley, M. L. Rockhold, and J. M. Zachara
Hanford Site Vadose Zone Studies: An Overview
Vadose Zone J., November 20, 2007; 6(4): 899 - 905.
[Abstract] [Full Text] [PDF]




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