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通过X射线显微断层扫描对人类前磨牙和釉珠中牙釉质和牙本质的矿物质含量进行比较。

A comparison of the mineral content of enamel and dentine in human premolars and enamel pearls measured by X-ray microtomography.

作者信息

Anderson P, Elliott J C, Bose U, Jones S J

机构信息

Department of Child Dental Health, London Hospital Medical College, U.K.

出版信息

Arch Oral Biol. 1996 Mar;41(3):281-90. doi: 10.1016/0003-9969(95)00122-0.

Abstract

Mineral content gradients in two composite enamel pearls from permanent human upper molars were measured by X-ray microtomography (XMT) at a resolution of 15-30 microns. This non-destructive microscopic technique was used to make 15-microns thick XMT slices with 100-microns separation through one pearl and 250-microns separation through the other. Average mineral contents were calculated from the linear absorption coefficients determined from regions of the XMT slices assuming the inorganic component to be calcium hydroxyapatite. These values were compared with similar XMT studies of coronal enamel and dentine of upper permanent premolars. A mineral content gradient in the pearls, reducing from the enamel surface to the amelodentinal junction, was found; this was similar to that observed in the coronal enamel of the upper premolar. The mineral contents in the surface and deeper enamel regions of the pearl were similar to those observed in premolar enamel. In contrast, the mineral content for the dentine of the pearl was greatest at the amelodentinal junction, i.e. the gradient was in the opposite direction to that observed in premolar dentine. These results suggest that the process of mineralization of the pearl dentine differs from that in permanent control dentine. In addition, gradients in enamel and dentine mineral contents reducing from the tip of the pearl to the base of the pearl were found.

摘要

通过分辨率为15 - 30微米的X射线显微断层扫描(XMT)测量了两颗来自人类恒牙上颌磨牙的复合釉珠中的矿物质含量梯度。这种非破坏性的显微技术用于制作15微米厚的XMT切片,其中一颗釉珠的切片间距为100微米,另一颗为250微米。假设无机成分是羟基磷灰石,根据XMT切片区域确定的线性吸收系数计算平均矿物质含量。将这些值与对上颌恒前磨牙牙冠釉质和牙本质的类似XMT研究结果进行比较。发现釉珠中存在矿物质含量梯度,从釉质表面到釉牙本质界逐渐降低;这与在上颌前磨牙牙冠釉质中观察到的情况相似。釉珠表面和较深釉质区域的矿物质含量与前磨牙釉质中观察到的相似。相比之下,釉珠牙本质的矿物质含量在釉牙本质界处最高,即梯度方向与前磨牙牙本质中观察到的相反。这些结果表明,釉珠牙本质的矿化过程与恒牙对照牙本质不同。此外,还发现了从釉珠尖端到基部釉质和牙本质矿物质含量逐渐降低的梯度。

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