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磨牙切牙矿化不全(MIH)的发病情况。

Onset of molar incisor hypomineralization (MIH).

作者信息

Fagrell Tobias G, Salmon Phil, Melin Lisa, Norén Jörgen G

机构信息

Paediatric Dentistry Special Dental Service, Sahlgrenska University Hospital Mölndal, Mölndal, Sweden.

出版信息

Swed Dent J. 2013;37(2):61-70.

Abstract

The etiological factors and timing of the onset of molar incisor hypomineralization (MIH) are still not clear. The aim of this study was to examine ground radial and sagittal sections from teeth diagnosed with MIH using light microscopy, polarized light microscopy and X-ray micro-computed tomography (XMCT) and to estimate the onset and timing of the MIH and to relate the hypomineralized enamel to the incremental lines. Thirteen extracted permanent first molars diagnosed MIH, were analyzed with light microscopy and XMCT. The hypomineralized areas were mainly located in the mesio-buccal cusps, starting at the enamel-dentin-junction and continuing towards the enamel surface. In a relative gray scale analysis the values decreased from the EDJ towards the enamel surface. The findings indicate that the ameloblasts in the hypomineralized enamel are capable of forming an enamel of normal thickness, but with a substantial reduction of their capacity for maturation of enamel. Chronologically, it is estimated that the timing of the disturbance is at a period during the first 6-7 months of age.

摘要

磨牙切牙矿化不全(MIH)的病因及发病时间仍不明确。本研究的目的是使用光学显微镜、偏振光显微镜和X射线显微计算机断层扫描(XMCT)检查诊断为MIH的牙齿的磨片径向和矢状切片,估计MIH的发病及时间,并将矿化不全的釉质与生长线联系起来。对13颗诊断为MIH的拔除恒牙第一磨牙进行了光学显微镜和XMCT分析。矿化不全区域主要位于近中颊尖,始于釉质-牙本质界并向釉质表面延伸。在相对灰度分析中,数值从釉质-牙本质界向釉质表面降低。研究结果表明,矿化不全釉质中的成釉细胞能够形成正常厚度的釉质,但其釉质成熟能力大幅降低。按时间顺序估计,这种干扰发生在出生后前6至7个月期间。

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