Monitoring of hydroxyapatite conversion by luminescence intensity and color during mineralization of Sm3+-doped β-dicalcium silicate
Autor: | Dongping Luo, Li Xie, Xu Chuanyan, Yadong Li, Ren-Jie Xu, Zhu Yangguang, Xiao-Qiang Zhou, Guang-Xiang Chen |
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Rok vydání: | 2020 |
Předmět: |
Materials science
Scanning electron microscope Simulated body fluid Biophysics Analytical chemistry 02 engineering and technology General Chemistry 010402 general chemistry 021001 nanoscience & nanotechnology Condensed Matter Physics 01 natural sciences Biochemistry Atomic and Molecular Physics and Optics Silicate 0104 chemical sciences chemistry.chemical_compound chemistry Fourier transform infrared spectroscopy Chromaticity 0210 nano-technology Luminescence Spectroscopy Diffractometer |
Zdroj: | Journal of Luminescence. 226:117468 |
ISSN: | 0022-2313 |
DOI: | 10.1016/j.jlumin.2020.117468 |
Popis: | Sm3+-doped β-dicalcium silicate (β-Ca2SiO4: Sm3+) was resoundingly prepared by the traditional high-temperature solid-state reaction method. The crystal structure, morphology and composition of β-Ca2SiO4: Sm3+ before and after mineralization was characterized by X-ray diffractometer (XRD), fourier transform infrared spectroscopy (FTIR), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDS), respectively. The luminescence properties of β-Ca2SiO4: Sm3+ before and after mineralization were investigated by luminescence spectroscopy. The results show that Sm3+ ion has the effect of stabilizing β-Ca2SiO4 and β-Ca2SiO4: Sm3+ has good biological activity and can be converted to hydroxyapatite (HA) in simulated body fluid. Meanwhile, with the prolongation of mineralization time, the luminescence intensity of Sm3+ ion decreased gradually, and the CIE chromaticity coordinates moved from orange region to yellow green region. This suggests that the evolution of luminescence properties can be used as an obvious qualitative feature to monitor the mineralization process of β-Ca2SiO4: Sm3+. |
Databáze: | OpenAIRE |
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