Biomimetic mineralization of partially bioresorbable glass fiber reinforced composite |
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Authors: | M.?V?kiparta author-information" > author-information__contact u-icon-before" > mailto:marju.vakiparta@utu.fi" title=" marju.vakiparta@utu.fi" itemprop=" email" data-track=" click" data-track-action=" Email author" data-track-label=" " >Email author,A.-P.?Forsback,L.?V.?Lassila,M.?Jokinen,A.?U.?O.?Yli-Urpo,P.?K.?Vallittu |
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Affiliation: | (1) Department of Prosthetic Dentistry, Turku Biomaterials Centre, University of Turku, Institute of Dentistry, Itäinen Pitkäkatu 4 B, FIN-20520 Turku, Finland;(2) University of Turku, Institute of Dentistry, Turku Biomaterials Centre, Turku, Finland;(3) Department of Prosthetic Dentistry and Biomaterials Research, University of Turku, Institute of Dentistry, Turku, Finland;(4) Department of Prosthetic Dentistry, Turku Biomaterials Centre, University of Turku, Institute of Dentistry, Turku, Finland |
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Abstract: | The aim of this study was to investigate the biomimetic mineralization on the surface of a glass fiber reinforced composite with partially resorbable biopolymer matrix. The E-glass fibers were preimpregnated with a novel biopolymer of poly(hydroxyproline) amide, and further impregnated in the monomer system of bis-phenyl glycidyl dimethacrylate (Bis-GMA)—triethylene glycol dimethacrylate (TEGDMA), which formed interpenetrating polymer networks (IPN) with the preimpregnation polymer. After light-initiated polymerization of the monomer system, the rhombic test specimens (n = 6) were immersed in the simulated body fluid (SBF) with the bioactive glass for 24 h, and then the apatite nuclei were allowed to grow for 1, 3, 5 and 7 days in the SBF. The control test specimens (n = 3) were immersed in SBF without the bioactive glass. According to the scanning electron microscope (SEM), a mineral layer was formed on the surface of all the specimens, which were immersed with bioactive glass. The layer was thickened by the prolonged immersion time to a uniform layer. The Ca/P atomic ratio of the mineral varied between 1.30 and 1.54 as analyzed by the energy dispersive X-ray analysis (EDXA). The Fourier transform infrared spectroscopy (FT-IR) spectra gave signals for the mineral, which are characteristic of both bone-like apatite and orthocalciumphosphate. In conclusion, the mineral layer was formed on the surfaces of the specimens by biomimetic mineralization, the mineral being a mixture of bone-like apatite, orthocalciumphosphate and other calcium phosphates. |
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