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Thermal and X-ray diffraction analysis studies during the decomposition of ammonium uranyl nitrate
Two types of ammonium uranyl nitrate (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O and NH(4)UO(2)(NO(3))(3), were thermally decomposed and reduced in a TG-DTA unit in nitrogen, air, and hydrogen atmospheres. Various intermediate phases produced by the thermal decomposition and reduction process were investigated...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Netherlands
2012
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4514459/ https://www.ncbi.nlm.nih.gov/pubmed/26224923 http://dx.doi.org/10.1007/s10967-011-1579-8 |
Sumario: | Two types of ammonium uranyl nitrate (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O and NH(4)UO(2)(NO(3))(3), were thermally decomposed and reduced in a TG-DTA unit in nitrogen, air, and hydrogen atmospheres. Various intermediate phases produced by the thermal decomposition and reduction process were investigated by an X-ray diffraction analysis and a TG/DTA analysis. Both (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O and NH(4)UO(2)(NO(3))(3) decomposed to amorphous UO(3) regardless of the atmosphere used. The amorphous UO(3) from (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O was crystallized to γ-UO(3) regardless of the atmosphere used without a change in weight. The amorphous UO(3) obtained from decomposition of NH(4)UO(2)(NO(3))(3) was crystallized to α-UO(3) under a nitrogen and air atmosphere, and to β-UO(3) under a hydrogen atmosphere without a change in weight. Under each atmosphere, the reaction paths of (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O and NH(4)UO(2)(NO(3))(3) were as follows: under a nitrogen atmosphere: (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O → (NH(4))(2)UO(2)(NO(3))(4)·H(2)O → (NH(4))(2)UO(2)(NO(3))(4) → NH(4)UO(2)(NO(3))(3) → A-UO(3) → γ-UO(3) → U(3)O(8), NH(4)UO(2)(NO(3))(3) → A-UO(3) → α-UO(3) → U(3)O(8); under an air atmosphere: (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O → (NH(4))(2)UO(2)(NO(3))(4)·H(2)O → (NH(4))(2)UO(2)(NO(3))(4) → NH(4)UO(2)(NO(3))(3) → A-UO(3) → γ-UO(3) → U(3)O(8), NH(4)UO(2)(NO(3))(3) → A-UO(3) → α-UO(3) → U(3)O(8); and under a hydrogen atmosphere: (NH(4))(2)UO(2)(NO(3))(4)·2H(2)O → (NH(4))(2)UO(2)(NO(3))(4)·H(2)O → (NH(4))(2)UO(2)(NO(3))(4) → NH(4)UO(2)(NO(3))(3) → A-UO(3) → γ-UO(3) → α-U(3)O(8) → UO(2), NH(4) UO(2)(NO(3))(3) → A-UO(3) → β-UO(3) → α-U(3)O(8) → UO(2). |
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