INEB
INEB
TitleDissolution studies of hydroxyapatite and glass-reinforced hydroxyapatite ceramics
Publication TypeJournal Article
2003
AuthorsQueiroz, AC, Santos, JD, Monteiro, FJ, Prado da Silva, MH
Secondary AuthorsG., S, F.L., FJ, G.A., S, P.L., S
JournalMaterials CharacterizationMater Charact
Volume50
Issue2-3
Pagination197 - 202
Date Published2003///
10445803 (ISSN)
Ceramic materials, Dissolution, glass, Glass-reinforced hydroxyapatite, hydroxyapatite, Immersion times, Scanning electron microscopy
In the continuous agitation assays, glass-reinforced hydroxyapatite (GR-HA) was shown to form a calcium phosphate (CaP) layer, but hydroxyapatite (HA) only formed dispersed precipitates. The formation of this layer was first detected on the GR-HA with a 7.5% glass addition (7.5 GR-HA) after only 3 days of immersion in simulated body fluid (SBF). The time required for layer formation decreased as the amount of glass added to the HA increased. The dissolution rate of the materials followed a similar pattern, i.e. the dissolution rate for GR-HA was higher than for HA, and increased with the addition of glass. The immersion of 7.5 GR-HA in water showed almost linear dissolution kinetics over the immersion periods (3, 7, 15, 30 and 60 days). The concentration of calcium ions in solution and the scanning electron microscopy (SEM) analysis of the 7.5 GR-HA specimens immersed in water and in SBF revealed a clear competition between the material dissolution and the precipitation of a CaP phase. Fourier transformed infrared spectroscopy with alternated total reflectance (FTIR-ATR) analysis indicated that the CaP phase that formed during longer immersion times (30 and 60 days) could be a carbonate-substituted CaP precipitate. As expected from previous work, the GR-HA behavior in terms of its in vitro bioactivity is higher than HA because a homogeneous CaP layer is formed and the precipitation occurs faster. From the dissolution test and in accordance with the chemical composition of the samples, GR-HA was more soluble than HA. © 2003 Elsevier Inc. All rights reserved.
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