SYNTHESIS, STRUCTURE AND CHARACTERIZATION OF URANIUM(IV) PHENYL PHOSPHONATE, U(O3PC6H5)(2), AND URANIUM(IV) PYRO PHOSPHATE, UP2O7

Citation
A. Cabeza et al., SYNTHESIS, STRUCTURE AND CHARACTERIZATION OF URANIUM(IV) PHENYL PHOSPHONATE, U(O3PC6H5)(2), AND URANIUM(IV) PYRO PHOSPHATE, UP2O7, Journal of solid state chemistry, 121(1), 1996, pp. 181-189
Citations number
50
Categorie Soggetti
Chemistry Inorganic & Nuclear","Chemistry Physical
ISSN journal
00224596
Volume
121
Issue
1
Year of publication
1996
Pages
181 - 189
Database
ISI
SICI code
0022-4596(1996)121:1<181:SSACOU>2.0.ZU;2-V
Abstract
Two tetravalent uranium compounds have been characterized. The structu re of a new uranium(IV) phosphonate, U(O3PC6H5)(2), has been solved fr om laboratory X-ray powder diffraction data by using ab initio methodo logy. U(O3PC6H5)(2) crystallizes in the space group C2/m with a = 9.45 59(7) A, b = 5.6769(5) Angstrom, c = 14.9687(12) Angstrom, beta = 96.5 39(5) Angstrom, V = 798.3(1) Angstrom(3), Z = 2. The reliability facto rs were R(WP) = 8.0%, R(p) = 6.04%, and R(F) = 3.0%. The structure is lamellar, and the framework of the U(O3P)(2) layers is similar to that of the alpha-Zr(HPO4)(2) . H2O-type structure, although the symmetry of the phosphonate group is higher than that of the phosphate groups i n alpha-Zr(HPO4)(2) . H2O and the phosphonate group in Zr(O3PC6H5)(2). The phenyl groups are located in the interlamellar space, being incli ned 10 degrees to the c-axis. The phenyl rings are tilted out 53 degre es from the ac plane, and they are disordered. We have also characteri zed this compound by UV-VIS-IR spectroscopies and thermal analysis. Th e thermal decomposition product is uranium(IV) pyre phosphate. This co mpound was identified through its X-ray powder diffraction pattern. UP 2O7 crystallizes in the Pa(3) over bar space group (a = 8.6311(2) Angs trom, V = 642.99(4) Angstrom(3), Z = 4). The structure belongs to the cubic ZrP2O7-type structure. The reliability factors were R(WP) = 11.7 %, R(P) = 8.6%, and R(F) = 10.4%. Disorder has been found in the oxyge n that bridges the pyrophosphate groups, leading to an angular P-O-P a rrangement. The VIS-near-IR adsorption spectra revealed the uranium(IV ) presence and the oxygen environment. (C) 1996 Academic Press, Inc.