目的:牙槽骨质量对颌面部的完整性和功能至关重要,取决于牙槽骨矿化。本研究旨在探讨体内牙槽骨矿化的变化,从生后大鼠矿物质沉积和晶体转变的角度。
方法:Wistar大鼠出生后九个时间点,从第1天到第56天,设置为获取上颌牙槽骨样本。每个时间点由90只大鼠组成,45名女性和45名男性。牙槽骨的宏观形态通过微计算机断层扫描重新进行,矿物质含量通过热重分析进行定量。扫描电子显微镜,高分辨率透射电子显微镜和振动光谱学。此外,通过振动光谱表征结晶度和组成,X射线衍射,X射线光电子能谱和选定区域电子衍射。
结果:在出生后的大鼠中,矿物质沉积的逐渐增加伴随着牙槽骨质量和体积的大量增长。而矿物百分比最初下降,然后上升,在出生后第14天(P14)首次观察到牙齿萌出时达到最低点。此外,局部矿化是由无定形前体的形成引发的,然后转化为矿物晶体,而生长过程中骨骼的平均结晶度没有统计学上的显着变化。
结论:在出生后大鼠的早期生长过程中,牙槽骨的矿化是持续的。矿物沉积随年龄增加,而结晶度在一定范围内保持稳定。此外,矿物质百分比在P14达到最低点,这可能归因于牙齿萌出。
OBJECTIVE: Alveolar bone quality is essential for the maxillofacial integrity and function, and depends on alveolar bone mineralization. This study aims to investigate the in vivo changes in alveolar bone mineralization, from the perspective of mineral deposition and crystal transition in postnatal rats.
METHODS: Nine postnatal time points of Wistar rats, ranging from day 1 to 56, were set to obtain the maxillary alveolar bone samples. Each time point consisted of ninety rats, with 45 females and 45 males. Macromorphology of alveolar bone was reconducted by Micro-Computed Tomography and the mineral content was quantified via Thermogravimetric analysis, Scanning Electron Microscope, High-Resolution Transmission Electron Microscopy and vibrational spectroscopy. Furthermore, the crystallinity and composition were characterized by vibrational spectroscopy, X-ray Diffraction, X-ray Photoelectron Spectroscopy and Selected Area Electron Diffraction.
RESULTS: The progressive increase of mineral deposition was accompanied by substantial growth in alveolar bone mass and volume in postnatal rats. Whereas the mineral percentage initially decreased and then increased, reaching a nadir on postnatal day 14 (P14) when tooth eruption was first observed. Besides, localized mineralization was initiated by the formation of amorphous precursors and then converted into mineral crystals, while there was no statistically significant change in the average crystallinity of the bone during growth.
CONCLUSIONS: Mineralization of alveolar bone is ongoing throughout the early growth in postnatal rats. Mineral deposition increases with age, whereas the crystallinity remains stable within a certain range. Besides, the mineral percentage reaches its lowest point on P14, which may be attributed to tooth eruption.