Larsen M J, Fejerskov O
Department of Oral Anatomy, Royal Dental College, Aarhus, Denmark.
Scand J Dent Res. 1989 Aug;97(4):285-96. doi: 10.1111/j.1600-0722.1989.tb01615.x.
The aim of the present paper was to identify some chemical and structural factors which may prevent a full remineralization of caries lesions and to study whether it is possible to overcome such obstacles. Samples of powdered enamel apatite were equilibrated with solutions metastably supersaturated with respect to enamel hydroxyapatite and fluorapatite. After 10 min and 60 min of equilibration at 20 degrees C the suspensions were centrifuged and the calcium and phosphate concentrations and the pH were determined in the supernatant. In parallel studies, 50 75-microns-thick sections of 27 fluorotic teeth of a severity of 5-7 according to Thylstrup and Fejerskov's classification were examined by microradiography and in polarized light using distilled water, and Thoulett's media or seen dry in air. Five obstacles inhibiting remineralization were identified: 1) Although remineralizing solutions or saliva are supersaturated with respect to enamel apatite the total amount of calcium and phosphate dissolved in it is small, so that after precipitation of the dissolved mineral only 1/20,000-1/30,000 of the volume of the mineralizing solution is occupied by mineral. 2) The concentration gradients from the mineralizing solution into the enamel is small, which indicates a slow diffusion into and out of the lesion. 3) The uptake of calcium and phosphate by the enamel apatite crystals is so rapid that the aqueous phase within the pores can be presumed to be only marginally supersaturated in the deeper parts of the lesion. 4) The surface layer of the enamel lesions was found to be a serious obstacle to remineralization so that a subsurface area remains hypomineralized after exposure to salivary remineralization even for a lifetime. 5) Nucleation of new apatite crystals to substitute lost crystals is an unsolved problem.
本文的目的是确定一些可能阻碍龋损完全再矿化的化学和结构因素,并研究是否有可能克服这些障碍。将粉末状牙釉质磷灰石样品与相对于牙釉质羟基磷灰石和氟磷灰石亚稳过饱和的溶液平衡。在20℃平衡10分钟和60分钟后,将悬浮液离心,并测定上清液中的钙、磷浓度和pH值。在平行研究中,根据Thylstrup和Fejerskov分类法,对27颗氟斑牙的50个75微米厚的切片进行了微放射照相检查,并在偏振光下使用蒸馏水、Thoulett介质进行观察,或在空气中干燥观察。确定了阻碍再矿化的五个障碍:1)尽管再矿化溶液或唾液相对于牙釉质磷灰石是过饱和的,但其中溶解的钙和磷总量很小,因此在溶解的矿物质沉淀后,矿化溶液中只有1/20000 - 1/30000的体积被矿物质占据。2)从矿化溶液到牙釉质的浓度梯度很小,这表明进入和离开病变的扩散缓慢。3)牙釉质磷灰石晶体对钙和磷的吸收非常迅速,以至于可以推测病变较深部位孔隙内的水相仅略微过饱和。4)发现牙釉质病变的表层是再矿化的严重障碍,因此即使暴露于唾液再矿化一生,病变的次表层区域仍保持矿化不足。5)新的磷灰石晶体成核以替代丢失的晶体是一个未解决的问题。