An SEM, EDS and vibrational spectroscopic study of the silicate mineral meliphanite (Ca,Na)2Be[(Si,Al)2O6(F,OH)].

Submitted by Marise Leite (marise_mg@yahoo.com.br) on 2015-12-16T13:31:46Z No. of bitstreams: 1 ARTIGO_SEMEDSMeliphanite.pdf: 943599 bytes, checksum: 620e8d2c1864f70533245e519a2e5560 (MD5)Approved for entry into archive by Oliveira Flávia (flavia@sisbin.ufop.br) on 2015-12-17T16:48:20Z (GMT) No. of bitstreams: 1 ARTIGO_SEMEDSMeliphanite.pdf: 943599 bytes, checksum: 620e8d2c1864f70533245e519a2e5560 (MD5)Made available in DSpace on 2016-01-15T16:47:28Z (GMT). No. of bitstreams: 1 ARTIGO_SEMEDSMeliphanite.pdf: 943599 bytes, checksum: 620e8d2c1864f70533245e519a2e5560 (MD5) Previous issue date: 2015The mineral meliphanite (Ca,Na)2Be[(Si,Al)2O6(F,OH)] is a crystalline sodium calcium beryllium silicate which has the potential to be used as piezoelectric material and for other ferroelectric applications. The mineral has been characterized by a combination of scanning electron microscopy (SEM) with energy dispersive spectroscopy (EDS) and vibrational spectroscopy. EDS analysis shows a material with high concentrations of Si and Ca and low amounts of Na, Al and F. Beryllium was not detected. Raman bands at 1016 and 1050 cm 1 are assigned to the SiO and AlOH stretching vibrations of three dimensional siloxane units. The infrared spectrum of meliphanite is very broad in comparison with the Raman spectrum. Raman bands at 472 and 510 cm 1 are assigned to OSiO bending modes. Raman spectroscopy identifies bands in the OH stretching region. Raman spectroscopy with complimentary infrared spectroscopy enables the characterization of the silicate mineral meliphanite