On the valency of uranium in aegirine and on behavior of isotopes U-234 and U-238 at dissolving the mineral

Citation
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
Citations number
3
Categorie Soggetti
Physics
Journal title
CZECHOSLOVAK JOURNAL OF PHYSICS
ISSN journal
00114626 → ACNP
Volume
49
Year of publication
1999
Part
1
Supplement
1
Pages
57 - 63
Database
ISI
SICI code
0011-4626(1999)49:<57:OTVOUI>2.0.ZU;2-V
Abstract
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).