The concentration of potassium regularly decreases with moving from a root zone of plants and increases in the order of <$E roman {soil~>>~rhizosphere~>>~rhizoplane}>. The contents of caesium in studied samples was much lower and differed more than one order of magnitude, though no essential differences between the contents of caesium in the total mass of soil, soil, rhizosphere, and rhizoplane are established. The concentration of potassium and caesium in mycelium of fungi almost by one order of magnitude is higher, than that in soil, and fruit bodies of fungi have much more accumulative capacity, than the vegetative body of a fungus - mycelium. Sarcodon imbricatus is characterized by the best accumulative capacity of studied species. The results obtained did not show any correlations between the potassium and caesium uptakes neither in mycelium of fungi, nor in fruit bodies.

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