Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The crystal structure of a new compound, (H3O)[(UO2)(SeO4)(SeO2OH)] (monoclinic, P21/n, a = 8.6682(19), b = 10.6545(16), c = 9.846(2) Å, β = 97.881(17)°, V = 900.7(3) Å3), was solved by direct methods and refined to R1 = 0.050. The structure contains two symmetrically different Se atoms. The Se1 site is coordinated by three O atoms as is characteristic of Se4+ cations. The Se2 site is coordinated by four O atoms and forms selenate anion SeO4 2-. The structure is based on selenite-selenate sheets [(UO2)(SeO4)(SeO2OH)]- linked by the interlayer H3O- ions. The sheets are parallel to (101). The structure is compared to that of schmiederite, Pb2Cu2(SeO3)(SeO4)(OH)4.
| Язык оригинала | английский |
|---|---|
| Страницы (с-по) | 663-667 |
| Число страниц | 5 |
| Журнал | Geology of Ore Deposits |
| Том | 51 |
| Номер выпуска | 7 |
| DOI | |
| Состояние | Опубликовано - 1 янв 2009 |
ID: 49250358