Assessment of the Safe Isolation of Solid Radwaste in Subsurface Repositories


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Abstract

A calculation of the removal of radionuclides by groundwaters from a subsurface repository of solid low-level waste was performed. A two-dimensional model of the groundwater flow and advective-dispersive transport of radionuclides in a vertical section of a subsurface aquifer, along which radionuclide-contaminated groundwater moves from the repository to an open body of water, was studied. Data from many years of experimentation on the leaching of cemented low-level waste were used in the calculations. It was shown that the rocks of the aquifer effectively retain medium half-life radionuclides (60Co, 137Cs, 90Sr). An engineered barrier – a 0.7 m thick layer of consolidated bentonite clay – can secure the safety of a repository for long-lived transuranium radionuclides (235U, 239Pu) for 20000 years.

About the authors

V. I. Mal’kovskii

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences (IGEM RAN)

Author for correspondence.
Email: malk@igem.ru
Russian Federation, Moscow

S. V. Yudintsev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences (IGEM RAN)

Email: malk@igem.ru
Russian Federation, Moscow

V. S. Gupalo

National University of Science and Technology MISiS

Email: malk@igem.ru
Russian Federation, Moscow

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