M. Koskenlinna et al., LOW-TEMPERATURE CRYSTAL-STRUCTURES AND THERMAL-DECOMPOSITION OF URANYL HYDROGEN SELENITE MONOHYDRATE, UO2(HSEO3)(2) H2O AND DIAMMONIUM URANYL SELENITE HEMIHYDRATE, (NH4)(2)UO2(SEO3)(2)CENTER-DOT-0.5H(2)O, Acta chemica Scandinavica, 51(3), 1997, pp. 264-269
The structures of the uranyl hydrogen selenite monohydrate, UO2(HSeO3)
(2) . H2O and diammonium uranyl selenite hemihydrate, (NH4)(2)UO2(SeO3
)(2) . 0.5H(2)O have been determined by S-ray diffraction at 193 K and
their thermal decomposition studied. The structure of (NH4)(2)UO2(SeO
3)(2) . 0.5H(2)O is layered. The layers are formed by the two unequal
selenite ions acting as bridging ligands between three and two U-VI io
ns, respectively. The ammonium ions and the water molecule form an arr
ay, which through a complex hydrogen bond network holds the layers tog
ether. In UO2(HSeO3)(2) . H2O the hydrogen selenite ion acts as a brid
ging ligand between two consecutive U-VI ions, leading to a structure
of one-dimensional zigzag chains. (NH4)(2)UO2(SeO3)(2) . 0.5H(2)O deco
mposes in air between 570 and 640 K in a single thermogravimetric step
to a phase containing uranyl selenite with additional selenium dioxid
e. The final product, U3O8, is formed between 870 and 930 K. After deh
ydration UO2(HSeO3)(2) . H2O decomposes to stoichiometric UO2SeO3 . Se
O2. This compound decomposes further to the same non-stoichiometric ur
anyl selenite-selenium dioxide phase as the ammonium compound.