Abstract

Abstract The hydriding kinetics of activated uranium powder was studied under low (near equilibrium) hydrogen pressures and between 290 and 370 °C in order to elucidate the hydriding mechanism. Activation of the samples was preformed by repeated cycles of hydriding and decomposition, which led to apparently unchanging kinetics after six cycles at 370 °C and under 470 Torr hydrogen. Scanning electron micrographs show that the activated sample has a complex structure of very thin (between 0.01 and 1 μm thick) thread-like extensions. The hydriding kinetics of the activated uranium samples consist of three stages in general: an initial accelerating stage, growing shorter as the hydrogen pressure increases, associated with hydride phase nucleation and growth. A linear reaction stage follows the initial accelerating step. This stage is associated with the advance of the hydride layer within the powder particles. Finally, a decelerating stage is observed, which may involve the main part of the reaction. It was found that the pressure dependence of the linear kinetic constant, k L , can be described by the relation k L ( P , T )= k L0 ( T )( P / P 0 −1) 2 , where P 0 is the equilibrium pressure for hydrogen absorption. An explanation is suggested for the unusual parabolic pressure dependence based on a nucleation and growth mechanism. The activation energy for the pressure-independent rate constant, k L0 ( T ), is estimated to be 5.4 kcal/g-at. H (0.24 eV), which is in fair agreement with values measured for bulk uranium samples.

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