ARCHAEOLOGICAL GLASSES – A MODEL FOR THE STABILITY EVALUATION OF THE VITRIFIED RADIOACTIVE WASTE

Authors

  • Yu. Lytvynenko State Institution "The Institute of Environmental Geochemistry of National Academy of Sciences of Ukraine", 34а Acad. Palladin Ave., Kyiv, 03142, Ukraine
  • Т. Melnychenko State Institution "The Institute of Environmental Geochemistry of National Academy of Sciences of Ukraine", 34а Acad. Palladin Ave., Kyiv, 03142, Ukraine
  • V. Kadoshnikov State Institution "The Institute of Environmental Geochemistry of National Academy of Sciences of Ukraine", 34а Acad. Palladin Ave., Kyiv, 03142, Ukraine
  • V. Shkapenko State Institution "The Institute of Environmental Geochemistry of National Academy of Sciences of Ukraine", 34а Acad. Palladin Ave., Kyiv, 03142, Ukraine

DOI:

https://doi.org/10.17721/1728-2713.97.12

Keywords:

liquid radioactive waste, volume reduction, archaeological and borosilicate glasses, aluminosilicates, protective gel layer, leaching rate

Abstract

This article presents the possibility of usage of the archaeological glasses to predict the behavior of radionuclides incorporated into the glass matrix, under the conditions of the underground storage during prolonged contact with the groundwater. Archaeological glasses, whose age is more than two thousand years old, selected from the cultural horizon of the archaeological reserve "Olvia" were examined. A gel layer was formed on the surface of the glass prolonged contact with the soil, on the outer surface of which layered aluminosilicates are formed. The formation of a protective layer of the glass occurs by the mechanism of the incongruent dissolution. It has been experimentally established that alkaline and alkaline earth cations (Na, Ca), partially silicon and iron, are intensively removed into the soil during leaching from the glass, with the practical immobility of aluminum. Simulation of glass fracture was performed in Soxhlet extractors under conditions of continuous exposure to hot water (t = 75–80 °C) saturated with carbon dioxide for 6 months. The change in the rate of components removal from the glass is connected with an increase in the thickness of the "locking" gel layer, the thickness of which increases over time. Cyclic changes in the dissolution rate of the glass are connected with the partial destruction of the gel layer due to the increase in thickness of the gel layer and, accordingly, a decrease in the adhesion of the gel to the glass. The results of the aluminosilicate (archaeological) glasses fracture study and their comparison with the results of the borosilicate glasses fracture study indicate that archaeological glasses can be a model for the predicting of the behavior in natural conditions of the glass matrices intended for radioactive waste volume reduction for centuries. 

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Published

2025-01-16

How to Cite

Lytvynenko, Y., Melnychenko Т., Kadoshnikov, V., & Shkapenko, V. (2025). ARCHAEOLOGICAL GLASSES – A MODEL FOR THE STABILITY EVALUATION OF THE VITRIFIED RADIOACTIVE WASTE. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 2(97), 92-96. https://doi.org/10.17721/1728-2713.97.12