Abstract
In order to investigate the possibility of the disposal of solid waste directly in the soil, the movement of HTO-labelled water was studied in the soil of Püspökszilágy, Hungary (Plant for the Processing and Storage of Radioactive Waste) at depths from 2.0 to 2.9 m under the surface level. To characterize the water movement a time-independent quantity—migration distance divided by the amount of irrigated water—was chosen. Its value diminished from the initial 0.3 to 0.2 cm/L with the increase of the clay content of the soil. The developed mathematical model fits the experimental results adequately.
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