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首页> 外文期刊>Acta biomaterialia >Substrate geometry directs the in vitro mineralization of calcium phosphate ceramics.
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Substrate geometry directs the in vitro mineralization of calcium phosphate ceramics.

机译:基材几何形状引导磷酸钙陶瓷的体外矿化。

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Repetitive concavities on the surface of bone implants have recently been demonstrated to foster bone formation when implanted at ectopic locations in vivo. The current study aimed to evaluate the effect of surface concavities on the surface mineralization of hydroxyapatite (HA) and β-tricalcium phosphate (β-TCP) ceramics in vitro. Hemispherical concavities with different diameters were prepared at the surface of HA and β-TCP sintered disks: 1.8mm (large concavity), 0.8mm (medium concavity) and 0.4mm (small concavity). HA and β-TCP disks were sintered at 1100 or 1200°C and soaked in simulated body fluid for 28 days at 37°C; the mineralization process was followed by scanning electron microscopy, energy-dispersive spectroscopy, X-ray diffraction and calcium quantification analyses. The results showed that massive mineralization occurred exclusively at the surface of HA disks treated at 1200°C and that nucleation of large aggregates of calcium phosphate started specifically inside small concavities instead of on the planar surface of the disks. Regarding the effect of concavity diameter size on surface mineralization, it was observed that small concavities induce 124- and 10-fold increased mineralization compared to concavities of large or medium size, respectively. The results of this study demonstrated that (i) in vitro surface mineralization of calcium phosphate ceramics with surface concavities starts preferentially within the concavities and not on the planar surface, and (ii) concavity size is an effective parameter to control the spatial position and extent of mineralization in vitro.
机译:最近已经证明了骨植入物表面上的重复凹陷,以促进体内异位位置时培养骨形成。目前的研究旨在评估表面凹陷对羟基磷灰石(HA)和β-三钙(β-TCP)陶瓷体外陶瓷表面矿化的影响。在HA和β-TCP烧结盘的表面上制备具有不同直径的半球形凹凸:1.8mm(凹陷大),0.8mm(中等凹陷)和0.4mm(小凹陷)。 HA和β-TCP盘在1100或1200℃下烧结并在37°C下浸泡在模拟体液中28天;矿化过程之后是扫描电子显微镜,能量分散光谱,X射线衍射和钙定量分析。结果表明,在1200℃处理的HA盘表面上仅发生大量矿化,并且磷酸钙的大聚集体的成核在小盘的平面上开始。关于凹凸直径大小对表面矿化的影响,观察到与大或中等尺寸的凹凸相比,小凹陷诱导124-和10倍的矿化。本研究的结果证明(i)磷酸钙陶瓷的体外表面矿化,表面凹陷优先于凹陷内,而不是在平面上,并且(ii)凹凸尺寸是控制空间位置和范围的有效参数矿化体外矿化。

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