Rv. Bogdanov et al., On the valency of uranium in aegirine and on behavior of isotopes U-234 and U-238 at dissolving the mineral, CZEC J PHYS, 49, 1999, pp. 57-63
An attempt has been undertaken to find a correlation beetween the valency f
orms of uranium and the isotopic ratio (AR=U-234/U-238) following the incon
gruent dissolving of the mineral aegirine. The low values of AR (approximat
e to 0.7) observed for hematite are assumed to be connected with the existe
nce of considerable fraction of U(V) form in the original mineral. The disc
ussion is given on the origin of the values of AR approximate to 1 and on i
ts connection with different stabilities of U(IV) and U(VI).