Structure, biomineralization and biodegradation of Ca-Mg oxyfluorosilicates synthesized by inorganic salt coprecipitation
E. Salahinejad, M. Jafari Baghjeghaz

TL;DR
This study synthesized Ca-Mg oxyfluorosilicates with varying fluoride levels, analyzing their structure, biomineralization potential, and biodegradability, revealing optimal fluoride doping for biomedical applications.
Contribution
It introduces a novel synthesis method for fluoride-doped Ca-Mg oxyfluorosilicates and identifies optimal fluoride levels for enhanced biomineralization.
Findings
Samples with up to 2 mol% F are single-phase diopside.
Optimal fluoride content for biomineralization is 1 mol%.
Fluoride incorporation enhances apatite formation without forming fluorite.
Abstract
In this research, a novel group of Ca-Mg oxyfluorosilicates containing different levels of fluoride substituting for oxide was synthesized by an inorganic salt coprecipitation process followed by calcination/sintering. The effects of the incorporation of fluoride on the resultant structural characteristics, apatite-forming ability and biodegradability were evaluated by X-ray diffraction, transmission electron microscopy, scanning electron microscopy/energy-dispersive X-ray spectroscopy, Fourier transform infrared spectroscopy, inductively coupled plasma spectroscopy and pH measurements. According to the results, the samples containing up to 2 mol% F present a single-phase structure of diopside (MgCaSi2O6) doped with F. It was also found that to meet the most biomineralization characteristic, the optimal value of fluoride in the homogeneous samples is 1 mol%. In this regard, on the one…
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Taxonomy
TopicsFluoride Effects and Removal · Clay minerals and soil interactions · Bone Tissue Engineering Materials
