THE EFFECT OF IONIZING RADIATION ON URANOPHANE

dc.contributor.authorUtsunomiya S.
dc.contributor.authorWang L.-M.
dc.contributor.authorEwing R.C.
dc.contributor.authorDouglas M.
dc.contributor.authorClark S.B.
dc.date.accessioned2021-12-02T03:58:05Z
dc.date.available2021-12-02T03:58:05Z
dc.date.issued2003
dc.description.abstractThe susceptibility of uranophane, a uranyl sheet silicate, ideally Ca(UO2)2(SiO3OH)2(H2 (H2O)5, to ionizing irradiation has been evaluated by systematic irradations with 200 ke V electrons over the temperature range 94 to 573 K. High-resolution transmission electron microscopy revealed that amorphous domains formed locally, concurrently with a gradual disordering of the entire structure. Amorphization doses at room temperature were 1.1 × 1010 Gy for uranophane, 1.3 × 1010 Gy for Sr-substituted uranophane, and 1.9 × 1010 Gy for Eu-substituted uranophane; thus, there was an increase in amorphization dose with increasing average atomic mass. At 573 K, the amorphization dose of uranophane was 2.0 × 1011 Gy. The temperature dependence of the amorphization dose of uranophane has two stages; ≤413 K and >413 K. Based on a defect accumulation model, the effective activation energies for amorphization at each stage are 0.0440 eV and 0.869 eV, respectively. This suggests that the presence of H2O (and OH-) reduce the energy deposition required to cause amorphization. Above 413 K, the amorphization dose increased due to the absence of H2O and OH- and the absence of radiolytic decomposition of H2O and OH-.
dc.identifierhttps://www.elibrary.ru/item.asp?id=14384366
dc.identifier.citationAmerican Mineralogist, 2003, 88, 1, 159
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/32613
dc.subjectUranophane
dc.titleTHE EFFECT OF IONIZING RADIATION ON URANOPHANE
dc.typeСтатья

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