Cathodoluminescence response of natural and synthetic lanthanide-rich phosphates (Ln3+: Ce, Nd)

• Published in: Radiation physics and chemistry (Oxford, England : 1993) Vol. 141; pp. 271 - 275
• Main Authors: Barrera-Villatoro, A., Boronat, C., Rivera-Montalvo, T., Correcher, V., Garcia-Guinea, J., Zarate-Medina, J.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01-12-2017; Elsevier BV
• Subjects: Cathodoluminescence; Cerium; Chemical precipitation; Crystal defects; Heat treatment; Lanthanides; Monazite; Neodymium; Phase transitions; Phosphates; Scanning electron microscopy; X-ray diffraction; Phosphates; Cathodoluminescence; Lanthanides; Monazite
• ISSN: 0969-806X; 1879-0895
• DOI: 10.1016/j.radphyschem.2017.07.027

This paper reports on the cathodoluminescence (CL) emission of both natural and synthetic lanthanide-rich phosphates (Ln3+: Ce, Nd) previously characterized by X-ray Diffraction (XRD), Environmental Scanning Electronic Microscopy (ESEM) and Energy Dispersive Spectroscopy. The thermal treatment at 700°C performed on the synthetic sample obtained by chemical precipitation, promotes increasing of the crystallinity degree giving rise to a phase transition from the hexagonal (comprising monazite and rabdophane) into the monoclinic (cerianite and monazite) structures detected by XRD. Despite the size and the morphology of the grains are similar under ESEM, it could be appreciated significant differences among CL signals attending to the shape (with well-defined peaks for the annealed sample) and intensity (with lower emission for the non-thermally pretreated synthetic phosphate). The main wavebands centered at (i) 360, 380 and 490nm are associated respectively with 5D3/2 → 2F5/2 and 5D3/2 → 2F7/2 transitions as well as a redox reaction assigned to the presence of Ce3+, (ii) 276, 424, 516 and 531nm are linked respectively to 2G9/2→4I9/2, 2P1/2→4I9/2, 4G9/2→4I9/2 and 4G7/2→4I9/2 Nd3+ transitions and (iii) 400–490nm is due to non-bridging oxygen hole centers related to the tetrahedral PO43- groups or structural defects for the heated synthetic samples. The natural sample from Madagascar, with a very complex CL spectrum, displays a characteristic band emission in the green-yellow and red regions corresponding to [UO2]2+ groups and Sm3+ respectively.
•Synthetic Monazite were synthesized by Chemical precipitation method.•Cathodoluminescence emission displays spectra with well-defined maxima.•Thermal treatment (700°C) induces an increase of the crystallinity degree.