The kinetics of dissolution of UO2 under reducing conditions and the influence of an oxidized surface layer (UO2+x): Application of a continuous flow-through reactor

Author:

Bruno Jordi,Casas Ignasi,Puigdomènech Ignasi

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference47 articles.

1. Oxidation of Uranium Dioxide at 298 K studied by using X-ray Photoelectron Spectroscopy;Allen;J. Phys. Chem.,1986

2. Oxidizing lixiviation of pitchblendes and precipitation of the uranium with hydrogen;Balaceanu,1958

3. Role of surface speciation in the low temperature dissolution of minerals;Blum;Nature,1988

4. Validation of the SKBU1 uranium thermodynamic data base for its use in geochemical calculations with EQ3/6;Bruno,1989

5. Studies of the radionuclide coprecipitation-solid solution formation. The UO2(s)-La(OH)3(s) coprecipitation as an analogue for the UO2(s)-Pu(OH)3(s) system;Bruno,1985

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