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体外或口腔内脱矿后牙釉质物理变化与碘渗透能力变化之间的相关性。

Correlation between physical changes in tooth enamel and changes in iodide penetrability following in vitro or intraoral demineralization.

作者信息

Kashket S, Ahern J M

机构信息

Forsyth Dental Center, Boston, Mass.

出版信息

Caries Res. 1989;23(4):232-7. doi: 10.1159/000261183.

DOI:10.1159/000261183
PMID:2790855
Abstract

Demineralization of bovine tooth enamel was assessed by various physical means, and results were compared to measured changes in penetrability to iodide ions (delta Ip). Blocks of bovine enamel were exposed in vitro to lactate buffer (pH 4.3) containing 25 mM CaCl2 and 10 mM KH2PO4 for up to 4 days. Delta Ip increased over a wide range with time. A plot with respect to microhardness exhibited a pronounced inflection, with delta Ip rising rapidly at indentation depths greater than 2.5 microns. Microradiography and polarized light microscopy demonstrated subsurface lesions coincident only with the higher delta Ip values. The limited demineralization during the early time periods, therefore, was associated with only minimal changes at or near the enamel surface, yet could be detected readily with the delta Ip system. Demineralization produced intraorally in subjects rinsing with 5% sucrose was accompanied by increases in delta Ip, but no changes in surface microhardness or microscopic appearance of the enamel. It appeared that, under these conditions, demineralization was limited to the surface and corresponded to the very early phases of lesion formation.

摘要

通过多种物理方法评估牛牙釉质的脱矿情况,并将结果与碘离子渗透性的测量变化(δIp)进行比较。将牛牙釉质块在体外暴露于含有25 mM氯化钙和10 mM磷酸二氢钾的乳酸缓冲液(pH 4.3)中长达4天。δIp随时间在很宽的范围内增加。关于显微硬度的曲线呈现出明显的拐点,在压痕深度大于2.5微米时,δIp迅速上升。显微放射照相术和偏光显微镜显示,亚表面病变仅与较高的δIp值一致。因此,在早期阶段有限的脱矿与牙釉质表面或其附近仅微小的变化相关,但使用δIp系统可以很容易地检测到。在用5%蔗糖漱口的受试者口腔内产生的脱矿伴随着δIp的增加,但牙釉质的表面显微硬度或微观外观没有变化。在这些条件下,脱矿似乎仅限于表面,并且与病变形成的非常早期阶段相对应。

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