Arends J, Jongebloed W, Ogaard B, Rölla G
Scand J Dent Res. 1987 Jun;95(3):193-201. doi: 10.1111/j.1600-0722.1987.tb01830.x.
In this paper a combined microradiography and SEM study is presented on human enamel after a caries attack in vivo for a 4-wk period. The initial enamel caries is induced under a specially designed orthodontic band; plaque accumulation takes place under a niche in the band. The microradiography and SEM were done on the same sections. A special manipulation and breaking technique of the thin sections makes it possible to observe with the SEM, demineralized enamel areas with a mineral content known from microradiography. The results show that with a mineral content of about 50 vol. %, the observable porosity is noticeable at the prism level (interprismatically) but barely noticeable at the cyrstallite level. The surface morphology of the demineralized enamel is at low magnifications not very different from sound enamel. At high magnifications, however, the surface porosity becomes visible. The results indicate that the mineral in vivo losses in enamel after an initial caries attack can be explained mainly by mineral losses from interprismatic areas and from the prism peripheries.
本文介绍了一项针对人体牙釉质在体内遭受4周龋齿侵蚀后的显微放射照相术和扫描电子显微镜(SEM)联合研究。初始牙釉质龋损是在特制的正畸带环下诱发的;菌斑在带环的一个凹陷处积聚。显微放射照相术和扫描电子显微镜观察是在同一切片上进行的。通过对薄片进行特殊的处理和折断技术,利用扫描电子显微镜可以观察到脱矿牙釉质区域,其矿物质含量可通过显微放射照相术得知。结果表明,当矿物质含量约为50%(体积)时,在棱柱水平(棱柱间)可观察到明显的孔隙率,但在微晶水平几乎观察不到。脱矿牙釉质的表面形态在低倍放大时与健康牙釉质没有太大差异。然而,在高倍放大时,表面孔隙率变得可见。结果表明,在初次龋齿发作后,牙釉质中矿物质的体内损失主要可以解释为棱柱间区域和棱柱周边的矿物质损失。