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Nanoscale Analysis of Bone Mineral Crystals

机译:纳米级分析骨矿物晶体

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摘要

The mineral component of both bones and teeth comprises of crystals of substituted calcium hydroxyapatite. However, there are very few studies which have characterised and compared individual crystals from these mineralised tissues at the nanoscale. In our previous studies, we have utilised atomic force microscopy (AFM) to characterise crystals isolated from rat developing enamel and have described arrays of repeating charge domains on the crystal surfaces. The present aim was to utilise AFM and Self-Assembled Monolayer (SAM) technologies to investigate the topography and surface properties of crystals isolated from rat femoral cortical bone and compare these with the known characteristics of developing enamel crystals. In contrast to enamel crystals, AFM images clearly showed that individual bone crystals are thin, plate-like structures with sub-nm surface "steps" approximating to the unit cell dimensions for hydroxyapatite. These surface steps may be associated with step or spiral growth. Crystal aggregates were also present, suggesting that crystal fusion may have occurred in vivo. Bone crystals were successfully bound to charged SAM surfaces (both negative and positive) permitting imaging in contact mode AFM. No crystals were observed on uncharged SAMs. Preferential binding was seen on negatively-charged SAM surfaces, indicating a predominantly positive charge on the crystal surfaces similar to that seen in developing enamel crystals. The charge on the crystal surface may play a key role in the mechanism of matrix-mineral interactions.
机译:骨骼和牙齿的矿物成分包括取代羟基磷灰石的晶体。然而,很少有研究表征并将来自这些矿化组织的个体晶体与纳米级的表征相比。在我们之前的研究中,我们利用原子力显微镜(AFM)来表征从大鼠显影搪瓷中分离的晶体,并描述了晶体表面上的重复电荷域的阵列。目前的目的是利用AFM和自组装的单层(SAM)技术来研究从大鼠股骨皮质骨中分离的晶体的形貌和表面性质,并将这些与显影牙釉质晶体的已知特征进行比较。与牙釉质晶体形成对比,AFM图像清楚地表明,个体骨晶体是薄的,具有亚NM表面“步骤”的板状结构,其近似于羟基磷灰石的单元电池尺寸。这些表面步骤可以与步骤或螺旋生长相关联。还存在晶体聚集体,表明晶体融合可能在体内发生。成功结合骨晶体,允许在接触模式AFM中成像的带电的SAM表面(负极和正)。在不带电的Sams上观察到没有晶体。在带负电的SAM表面上看到优先结合,表明在晶体表面上的主要电荷类似于在​​显影牙釉质晶体中看到的晶体表面。晶体表面上的电荷可能在基质矿物相互作用的机制中发挥关键作用。

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