Thin films of UO 2, which were either fine-crystalline or mono-crystalline were treated in an electron diffraction set with oxygen (10 −3 torr) between 300 and 750°C for about 20 hr. Diffraction photographs were taken in transmission from time to time. The fine-crystalline specimens showed transformation to UO 2+ x and U 3O 8− x . Other phases, as U 3O 7 or U 2O 5 e.g. could not be observed. The hexagonal U 3O 8− x -phase exhibits a super structure cell with a = 6.72 A ̊ , c = 6 × 4.105 A ̊ , whose c-axis is 6 times as large as the U 3O 8 cell observed by Siegel. (3) The lattice constant of UO 2+ x decreases with increasing time of oxidation, but increases at the moment, when the U 3O 8− x -superstructure phase is formed. This shows, that part of the oxygen for the formation of U 3O 8− x must be taken from UO 2+ x . At a pressure of 10 −4 torr the mono-crystalline specimens from a superstructure with a = 3 a UO 2+ x ; at 10 −3 torr a tetragonal superstructure with a = 4 a UO 2+ x is formed. The latter phase has the composition UO 2,19, it probably forms the oxygen-rich phase border of UO 2+ x and its atomic positions were given in a former paper (1). The atomic arrangements during the oxidation of UO 2 to U 3O 8 can be described in a similar way as with the systems NbO and TaO: in the beginning additional oxygen atoms are built into the lattice in a disordered manner. At distinct concentrations they arrange in long periods, forming superstructure cells. This also is in accordance with the formation of superstructures during reduction of U 3O 8, as observed by Sato. (8,9)
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