摘要

The minerals of the mixite group - zalesiite CaCu6[(AsO4)(2)(AsO3OH)(OH)(6)]center dot 3H(2)O from abandoned uranium deposit Zalesi,Czech Republic and calciopetersite CaCu6[(PO4)(2)(PO3OH)(OH)(6)]center dot 3H(2)O from a quarry near Domasov na Bystrici, northern Moravia, Czech Republic - were studied by Raman and infrared spectroscopy. The observed bands were assigned to the stretching and bending vibrations of (AsO4)(3-) and (AsO3OH)(2-) ions in zalesiite, and (PO4)(3-) and (PO3OH)(2-) in calciopetersite, and to molecular water, hydroxyl ions, and Cu-(O,OH) units in both minerals. O-H center dot center dot center dot O hydrogen-bond lengths in zalesite and calciopetersite structures were calculated with Libowitzky's empirical relation.

  • 出版日期2011-5