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氟斑牙人牙釉质中窝点的扫描电子显微镜和显微放射照相研究。

A scanning electron microscopic and microradiographic study of pits in fluorosed human enamel.

作者信息

Thylstrup A, Fejerskov O

出版信息

Scand J Dent Res. 1979 Apr;87(2):105-14. doi: 10.1111/j.1600-0722.1979.tb00661.x.

Abstract

The aim of the present study has been to correlate the surface appearance of pitted, fluorosed enamel in the scanning electron microscope (SEM) with the microradiographic features of the underlying tissue. Intact enamel surfaces of severely fluorosed teeth appeared similar to that of normal enamel. In the unabraded surfaces discrete pits were sharply demarcated from the surrounding intact enamel surface leaving steep walls of parallel running rods. The microradiographic appearance of sections made through pits indicated that focal loss of surface enamel occurred corresponding to the inner highly hypomineralized part of the fluorotic subsurface lesion. The abrupt wall formation and the finding that the striae of Retzius never changed direction along the margins of the lesions indicated that pits in fluorosed enamel may be secondarily produced defects rather than true hypoplasias. Further evidence of the posteruptive origin of the defects was derived from the observation that enamel lamellae occasionally formed part of the lateral border. The relatively higher degree of radiopacity observed in the tissue surrounding the pit indicates a posteruptively acquired deposition of minerals in the exposed porous enamel.

摘要

本研究的目的是将扫描电子显微镜(SEM)下斑釉症的凹陷、氟斑牙釉质的表面外观与下层组织的显微放射照相特征联系起来。重度氟斑牙完整的釉质表面与正常釉质表面相似。在未磨损的表面,离散的凹坑与周围完整的釉质表面界限分明,留下平行排列的釉柱陡峭壁。通过凹坑制作的切片的显微放射照相外观表明,表面釉质的局灶性缺失与氟斑牙表层下病变内部高度矿化不足的部分相对应。凹坑边缘的突然形成以及芮氏线沿病变边缘从未改变方向的发现表明,氟斑牙釉质中的凹坑可能是继发产生的缺陷,而非真正的发育不全。缺陷萌出后起源的进一步证据来自于观察到釉板偶尔构成了凹坑侧缘的一部分。在凹坑周围组织中观察到的相对较高的不透射线性表明,在暴露的多孔釉质中存在萌出后获得性矿物质沉积。

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