2002
DOI: 10.1023/a:1013182917829
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Cited by 8 publications
(1 citation statement)
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“…The spectroscopic envelope for most of the oxyhydroxide minerals are observed from 855 to 830 cm −1 , with a handful of weak modes appearing at lower wavenumbers [86,87]. Curite (Pb 3+x (H 2 O)[(UO 2 ) 4 O 4+x (OH) 3x ] 2 ) and vandenbrandeite (Cu[UO 2 (OH) 4 ]) are notable exceptions because the uranyl bands are significantly red shifted to ~800–770 cm −1 [86,88,89]. This difference in vibrational frequency arises from structural variations within the mineral sheet topologies.…”
Section: Chemical and Structural Elucidation Of Uranium Solid-state Cmentioning
confidence: 99%
“…The spectroscopic envelope for most of the oxyhydroxide minerals are observed from 855 to 830 cm −1 , with a handful of weak modes appearing at lower wavenumbers [86,87]. Curite (Pb 3+x (H 2 O)[(UO 2 ) 4 O 4+x (OH) 3x ] 2 ) and vandenbrandeite (Cu[UO 2 (OH) 4 ]) are notable exceptions because the uranyl bands are significantly red shifted to ~800–770 cm −1 [86,88,89]. This difference in vibrational frequency arises from structural variations within the mineral sheet topologies.…”
Section: Chemical and Structural Elucidation Of Uranium Solid-state Cmentioning
confidence: 99%