In vitro model for frontal sinus obliteration with bioactive glass S53P4

An in vitro model was used to investigate the behavior of a massive frontal sinus obliteration with bioactive glass S53P4 (BG) for clinical purposes. Two sizes of granules (0.63–0.8 mm or 0.8–1.0 mm) in 16 separate BG amounts, weight 25 g, were tested both in simulated body fluid (SBF) and a buffer...

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Veröffentlicht in:Journal of biomedical materials research 2000, Vol.53 (2), p.161-166
Hauptverfasser: Peltola, Matti J., Suonpää, Jouko T. K., Andersson, H., Määttänen, Heli S., Aitasalo, Kalle M. J., Yli-Urpo, Antti, Laippala, Pekka J.
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container_title Journal of biomedical materials research
container_volume 53
creator Peltola, Matti J.
Suonpää, Jouko T. K.
Andersson, H.
Määttänen, Heli S.
Aitasalo, Kalle M. J.
Yli-Urpo, Antti
Laippala, Pekka J.
description An in vitro model was used to investigate the behavior of a massive frontal sinus obliteration with bioactive glass S53P4 (BG) for clinical purposes. Two sizes of granules (0.63–0.8 mm or 0.8–1.0 mm) in 16 separate BG amounts, weight 25 g, were tested both in simulated body fluid (SBF) and a buffer containing trishydroxymethyl aminomethane citric acid (TRIS‐c.a) in standard conditions. The dissolution of silicon (Si) and phosphate (P) was detected with direct current plasma atom emission spectroscopy (DCP‐AES) monthly up to 6 months. The BG masses were scanned by computer tomography (CT) and the scans analyzed by Region of Interest (ROI) technique. Calcium phosphate (CaP)‐ and silica (Si)‐gel‐layers were studied by scanning electron microscopy (SEM) at 1, 3, and 6 months. Cumulative loss of Si and P was stronger in TRIS ‐c.a than in SBF (p < 0.0001), and it was higher with smaller than with larger granules in both solutions (p < 0.0001).This was shown correspondingly by the decrease in Hounsfield units (HU) by ROI analysis (p < 0.0001). In SBF‐soaked BG masses, the CaP‐layer occurred on the uppermost granules, and in TRIS‐c.a at 3–6 months, on the granules in the center and lower parts. The decrease of HU seems to reveal indirectly the resorption of BG. © 2000 John Wiley & Sons, Inc. J Biomed Mater Res (Appl Biomater) 53: 161–166, 2000
doi_str_mv 10.1002/(SICI)1097-4636(2000)53:2<161::AID-JBM5>3.0.CO;2-3
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Calcium phosphate (CaP)‐ and silica (Si)‐gel‐layers were studied by scanning electron microscopy (SEM) at 1, 3, and 6 months. Cumulative loss of Si and P was stronger in TRIS ‐c.a than in SBF (p &lt; 0.0001), and it was higher with smaller than with larger granules in both solutions (p &lt; 0.0001).This was shown correspondingly by the decrease in Hounsfield units (HU) by ROI analysis (p &lt; 0.0001). In SBF‐soaked BG masses, the CaP‐layer occurred on the uppermost granules, and in TRIS‐c.a at 3–6 months, on the granules in the center and lower parts. The decrease of HU seems to reveal indirectly the resorption of BG. © 2000 John Wiley &amp; Sons, Inc. 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The dissolution of silicon (Si) and phosphate (P) was detected with direct current plasma atom emission spectroscopy (DCP‐AES) monthly up to 6 months. The BG masses were scanned by computer tomography (CT) and the scans analyzed by Region of Interest (ROI) technique. Calcium phosphate (CaP)‐ and silica (Si)‐gel‐layers were studied by scanning electron microscopy (SEM) at 1, 3, and 6 months. Cumulative loss of Si and P was stronger in TRIS ‐c.a than in SBF (p &lt; 0.0001), and it was higher with smaller than with larger granules in both solutions (p &lt; 0.0001).This was shown correspondingly by the decrease in Hounsfield units (HU) by ROI analysis (p &lt; 0.0001). In SBF‐soaked BG masses, the CaP‐layer occurred on the uppermost granules, and in TRIS‐c.a at 3–6 months, on the granules in the center and lower parts. The decrease of HU seems to reveal indirectly the resorption of BG. © 2000 John Wiley &amp; Sons, Inc. 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The dissolution of silicon (Si) and phosphate (P) was detected with direct current plasma atom emission spectroscopy (DCP‐AES) monthly up to 6 months. The BG masses were scanned by computer tomography (CT) and the scans analyzed by Region of Interest (ROI) technique. Calcium phosphate (CaP)‐ and silica (Si)‐gel‐layers were studied by scanning electron microscopy (SEM) at 1, 3, and 6 months. Cumulative loss of Si and P was stronger in TRIS ‐c.a than in SBF (p &lt; 0.0001), and it was higher with smaller than with larger granules in both solutions (p &lt; 0.0001).This was shown correspondingly by the decrease in Hounsfield units (HU) by ROI analysis (p &lt; 0.0001). In SBF‐soaked BG masses, the CaP‐layer occurred on the uppermost granules, and in TRIS‐c.a at 3–6 months, on the granules in the center and lower parts. The decrease of HU seems to reveal indirectly the resorption of BG. © 2000 John Wiley &amp; Sons, Inc. J Biomed Mater Res (Appl Biomater) 53: 161–166, 2000</abstract><cop>New York</cop><pub>John Wiley &amp; Sons, Inc</pub><pmid>10713562</pmid><doi>10.1002/(SICI)1097-4636(2000)53:2&lt;161::AID-JBM5&gt;3.0.CO;2-3</doi><tpages>6</tpages></addata></record>
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subjects bioactive glass
Biocompatibility
Biological and medical sciences
Body Fluids
Bone Substitutes
Calcium compounds
Computer aided analysis
Dissolution
Electron Probe Microanalysis
Emission spectroscopy
Frontal Sinus - diagnostic imaging
Frontal Sinus - surgery
Frontal Sinusitis - diagnostic imaging
Frontal Sinusitis - surgery
Glass
Humans
in vitro model
Indicators and Reagents
Medical sciences
Microscopy, Electron, Scanning
Phosphates
Physiological models
region of interest technique
Silicon
sinus obliteration
Surgery (general aspects). Transplantations, organ and tissue grafts. Graft diseases
Technology. Biomaterials. Equipments
Tomography, X-Ray Computed
title In vitro model for frontal sinus obliteration with bioactive glass S53P4
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