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人类氟斑牙的本质与机制。

The nature and mechanisms of dental fluorosis in man.

作者信息

Fejerskov O, Manji F, Baelum V

机构信息

Department of Oral Anatomy, Dental Pathology and Operative Dentistry, Royal Dental College, Aarhus, Denmark.

出版信息

J Dent Res. 1990 Feb;69 Spec No:692-700; discussion 721. doi: 10.1177/00220345900690S135.

Abstract

Any use of fluorides, whether systemic or topical, in caries prevention and treatment in children results in ingestion and absorption of fluoride into the blood circulation. The mineralization of teeth under formation may be affected so that dental fluorosis may occur. Dental fluorosis reflects an increasing porosity of the surface and subsurface enamel, causing the enamel to appear opaque. The clinical features represent a continuum of changes ranging from fine white opaque lines running across the tooth on all parts of the enamel to entirely chalky white teeth. In the latter cases, the enamel may be so porous (or hypomineralized) that the outer enamel breaks apart posteruptively and the exposed porous subsurface enamel becomes discolored. These changes can be classified clinically by the TF index to reflect, in an ordinal scale, the histopathological changes associated with dental fluorosis. Compared with Dean's and the TSIF index, we consider the TF index to be more precise. Recent studies on human enamel representing the entire spectrum of dental fluorosis have demonstrated a clear association between increasing TF score and increasing fluoride content of the enamel. So far, no useful data on dose (expressed in mg fluoride/kg b.w.)-response (dental fluorosis) relationships are available. In this paper, we have, therefore, re-evaluated the original data by Dean et al. (1941, 1942), Richards et al. (1967), and Butler et al. (1985) from the USA, by applying the equation of Galagan and Vermillion (1957) which permits the calculation of water intake as a function of temperature.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

在儿童龋齿预防和治疗中,无论是全身使用还是局部使用氟化物,都会导致氟化物摄入并吸收进入血液循环。正在形成的牙齿矿化可能会受到影响,从而可能发生氟斑牙。氟斑牙反映出表层和次表层牙釉质的孔隙率增加,导致牙釉质看起来不透明。临床特征呈现出一系列变化,从牙釉质各部位出现的细微白色不透明线条到完全呈白垩色的牙齿。在后一种情况下,牙釉质可能孔隙过多(或矿化不足),以至于萌出后外层牙釉质会破裂,暴露的多孔次表层牙釉质会变色。这些变化可通过TF指数进行临床分类,以按顺序量表反映与氟斑牙相关的组织病理学变化。与迪恩指数和TSIF指数相比,我们认为TF指数更精确。最近对代表氟斑牙全谱的人类牙釉质进行的研究表明,TF评分增加与牙釉质氟含量增加之间存在明显关联。到目前为止,尚无关于剂量(以毫克氟/千克体重表示)-反应(氟斑牙)关系的有用数据。因此,在本文中,我们重新评估了来自美国的迪恩等人(1941年、1942年)、理查兹等人(1967年)以及巴特勒等人(1985年)的原始数据,应用了加拉根和弗米利恩(1957年)的公式,该公式允许根据温度计算水摄入量。(摘要截选至250字)

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