2019
DOI: 10.1088/1742-6596/1292/1/012013
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Synthesis, characterization and evaluation of bioactivity of glasses in the CaO-SiO2-P2O5-MgO system with different CaO/MgO ratios

Abstract: Bioactive glasses (80Mg, 70Mg, 60Mg and 50Mg) in the system SiO2-CaO-P2O5-MgO were prepared by sol-gel method and then characterized. The structure of the synthesized samples has been studied by X-ray diffraction (XRD), Fourrier Transform Infrared Spectroscopy (FTIR) and Environmental Scanning Electron Microscopy (ESEM). In vitro bioactivity tests were performed in Simulated Body Fluid (SBF). The apparent density and wettability variation with time were measured. The in vitro studies showed the formation of an… Show more

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Cited by 12 publications
(5 citation statements)
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“…The spectra of the as-prepared samples show the absorption bands of the silicate group in the region 1020-1038 cm −1 , and at 446 cm −1 25 . In addition, for SNCP and SNCMP glasses, bands at 570 and within 788-794 cm -1 are observed and ascribed respectively to the bending vibration mode of P-O in amorphous calcium phosphate and to the symmetric stretching of Si-O-Si bond 25,26 ; however, none of these bands is observed for the as-prepared SCMP glass. A broad OH absorption band at 3330 cm −1 and a weak adsorbed water band ~ 1635-1660 cm −1 appeared in the spectra of as-prepared SCMP and SNCP samples.…”
Section: Resultsmentioning
confidence: 88%
“…The spectra of the as-prepared samples show the absorption bands of the silicate group in the region 1020-1038 cm −1 , and at 446 cm −1 25 . In addition, for SNCP and SNCMP glasses, bands at 570 and within 788-794 cm -1 are observed and ascribed respectively to the bending vibration mode of P-O in amorphous calcium phosphate and to the symmetric stretching of Si-O-Si bond 25,26 ; however, none of these bands is observed for the as-prepared SCMP glass. A broad OH absorption band at 3330 cm −1 and a weak adsorbed water band ~ 1635-1660 cm −1 appeared in the spectra of as-prepared SCMP and SNCP samples.…”
Section: Resultsmentioning
confidence: 88%
“…The increase in pH values continues until the tenth day (8.92 ± 0.09, and 8.80 ± 0.02 for BG, and BG/Zn MOF, respectively), then begins to decrease gradually until it reaches 8.26 ± 0.05 and 8.30 ± 0.03 for BG and BG/Zn MOF, respectively, at the end of soaking time. These findings could be explained as follows: at the early stages of incubation, the dissolution of samples takes place leading to Ca 2+ , and Si leaching out from samples, so pH increase occurs rapidly [39]; the Zn +2 release does not contribute to change in pH due to its low content in BG/Zn MOF sample. The decrease in pH may be ascribed to Ca +2 ions precipitation on the surface of the samples due to the attraction of the negative charge of Si-OH groups [46].…”
Section: Ion Release and Ph Change Analysismentioning
confidence: 98%
“…The presence of Zn MOF improved hydroxyapatite formation and caused Ca/P to approach stoichiometric apatite value (Ca/P = 1.67). Ion dissolution from glass samples initiates the formation of hydroxyapatite layer [39].…”
Section: Sem/edx After Sbf Soakingmentioning
confidence: 99%
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“…57 Although replacing calcium with other alkaline earth elements may not negatively affect dissolution rates, it can reduce the rate and amount of HAp formed. 58,59 Magnesium has been well studied and described to delay the formation of an apatite layer. 60,61 On the other hand, strontium has been found to assist in apatite formation through strontium-substituted apatite.…”
Section: Apatite Forming Abilitymentioning
confidence: 99%