Volume 40, Issue 2 pp. 359-369

QUANTIFICATION OF ACTINIDE MIGRATION PATHWAYS AT ROCKY FLATS, COLORADO1

Ian B. PatonChristine S. DaytonDavid M. JubenvilleEugene R. WeinerMartha W. Hyder

Martha W. Hyder

Respectively, Senior Project Engineer, Wright Water Engineers, Inc., 2490 West 26th Avenue, Suite 100-A, Denver, Colorado 80211; Project Manager, Kaiser-Hill Company, L.L.C., RFETS, 10808 Hwy. 93, Unit B, T130C, Golden, Colorado 80403–8200; Project Manager and Senior Chemist, Wright Water Engineers, Inc., 2490 West 26th Avenue, Suite 100-A, Denver, Colorado 80211; and Senior Scientist, Wind River Environmental Group, L.L.C. 3785 South Poplar Street, Denver, Colorado 80237 (E-Mail/Paton: [email protected]).

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First published: 08 June 2007
Citations: 1
1

Paper No. 02027 of the Journal of the American Water Resources Association (JAWRA) (Copyright © 2004). Discussions are open until October 1, 2004.

Abstract

ABSTRACT: Migration of plutonium, americium, and uranium (actinides) in the environment at the Rocky Flats Environmental Technology Site (RFETS) is the subject of ongoing studies to develop effective strategies for cleanup and regulatory closure of the Department of Energy facility. The Actinide Migration Evaluation pathway analysis quantified actinide transport processes to validate a qualitative conceptual model of environmental actinide transport. Major actinide transport mechanisms evaluated include surface water, ground water, airborne, and biological pathways. Relative quantities of actinide movement via different pathways were compared in terms of actinide loads delivered off the RFETS, using a combination of monitoring data, predictive transport models and results from historic RFETS studies. Results indicate air and surface water constitute the dominant transport mechanisms for plutonium and americium. In ground water, shallow alluvial flow is a limited pathway for plutonium and americium because of the low aqueous solubility of these actinides and their tendency to sorb to soil. However, localized flow in shallow alluvium is a more significant pathway for uranium movement, because of the relatively higher solubility of uranium (VI) species, though isotopic ratios indicate much of the uranium is from natural sources. Biological transport of actinides by mammals, birds, fish, and arthropods is small compared to the other pathways.

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