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氟化物与氟斑牙

Fluorides and dental fluorosis.

作者信息

Møller I J

出版信息

Int Dent J. 1982 Jun;32(2):135-47.

PMID:6749693
Abstract

This paper attempts to review present knowledge on the ingestion and metabolism of fluoride in relation to the occurrence of endemic dental fluorosis, a condition caused by an excessive intake of fluoride during tooth formation. The clinical appearance of dental fluorosis is characterized by lustreless opaque white patches in the enamel which may become striated, mottled and/or pitted. The opaque areas may become stained yellow to dark brown. The affected teeth may show a pronounced accentuation of the perikymata and, in more severe cases, multiple pits and larger areas of hypoplasia of the enamel appear so that the normal morphology of the tooth is lost. Due to the universal presence of fluoride in water, soil and the atmosphere it is not surprising that humans are exposed to various levels of fluoride intake , not only through food and water, but in industrial and pharmaceutical products and other sources. Water-borne fluoride, however, has been said to represent the largest single component of this element's daily intake, except where unusual dietary patterns exist. The daily amount of fluoride intake through water varies with climate (maximum daily temperature) and age. It has been postulated that significant changes in patterns of food and beverage ingestion, because of changes in available products and the ways in which they are marketed as well as many foods and beverages being processed in fluoridated communities, may have caused a change in the prevalence and severity of dental fluorosis over the past 30 years. Since fluoride remains pre-eminent among the measures available for increasing the resistance of teeth to caries attack, continued and renewed research on the ingestion and metabolism still has high priority.

摘要

本文旨在综述与地方性氟斑牙发生相关的氟摄入与代谢的现有知识,地方性氟斑牙是一种在牙齿形成过程中因过量摄入氟而引起的病症。氟斑牙的临床表现特征为牙釉质出现无光泽的不透明白色斑块,这些斑块可能会变成条纹状、斑驳状和/或凹陷状。不透明区域可能会被染成黄色至深褐色。受影响的牙齿可能会出现明显的釉面横纹加深,在更严重的情况下,会出现多个凹坑和更大面积的牙釉质发育不全,从而使牙齿失去正常形态。由于氟普遍存在于水、土壤和大气中,人类不仅通过食物和水,还通过工业和医药产品及其他来源接触到不同水平的氟摄入,这并不奇怪。然而,据说除了存在特殊饮食模式的情况外,水中的氟是该元素每日摄入量的最大单一组成部分。通过水摄入的氟的每日量随气候(最高每日温度)和年龄而变化。据推测,由于可获得产品及其销售方式的变化,以及许多食品和饮料在含氟社区进行加工,食品和饮料摄入模式的显著变化可能在过去30年中导致了氟斑牙患病率和严重程度的变化。由于在可用于增强牙齿抗龋能力的措施中,氟仍然最为突出,因此对氟摄入与代谢的持续研究和重新研究仍具有高度优先性。

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