Arnold W H, Konopka S, Kriwalsky M S, Gaengler P
Department of Anatomy, Faculty of Dental Medicine, University of Witten/Herdecke, Alfred-Herrhausen Strasse 50, 58448 Witten, Germany.
Ann Anat. 2003 Oct;185(5):419-24. doi: 10.1016/S0940-9602(03)80099-7.
Dentin is one of the earliest bio-mineralization products to appear in the evolution of vertebrates. Dentin reactions to infection mimic earlier phylogenetic patterns, and carious lesions are divided into different zones which reflect the natural patho-morphological reaction of dentin to the carious attack. It was the aim of this study to investigate deep dentin carious lesions of human molars with combined polarization light microscopy, scanning electron microscopy and energy dispersive X-ray element analysis (EDX) for the determination of different zones of the carious lesions, their extent and the chemical content. Sixteen extracted teeth with deep dentin carious lesions were embedded in Technovit 9100 (Kulzer) and serial sections of 80 microm thickness were made. These sections were then examined with polarized light microscopy to identify the different zones of the lesions. The outlines of the zones were traced consecutively and 3D-reconstructions were made for the determination of the extent and calculation of the volumes of the different zones. From the volumes of the demineralizing dentin and the translucent zone a Dentin Demineralization Index (DDI) was calculated. Three sections of each lesion were then coated with carbon and studied with a scanning electron microscope. 3D-reconstruction of the teeth showed the rather stable translucent zone, interrupted by remnants of dead tracts, and very different volumes of demineralizing dentin. Therefore, with increasing size of the demineralizing dentin, the DDI increased. The chemical content was measured using energy dispersive X-ray analysis (EDX) in areas of intertubular dentin. The content of Ca, P, and C was significantly different in all zones. The Ca/P ratio was significantly different between sound dentin and demineralizing dentin. From the results we conclude that the mineral content of intertubular dentin of the translucent zone and demineralizing dentin is different from that of sound dentin, and the unique mineralization pattern of the translucent zone is a biological reaction to the carious attack. Because active dentin lesions exhibit many non-occluded open dentin tubules, further bacterial invasion or, in case of dentin treatment, the penetration of bonding agents towards the pulp is morphologically not prevented and therefore of clinical importance.
牙本质是脊椎动物进化过程中最早出现的生物矿化产物之一。牙本质对感染的反应模拟了早期的系统发育模式,龋损被分为不同区域,这些区域反映了牙本质对龋病攻击的自然病理形态学反应。本研究的目的是结合偏光显微镜、扫描电子显微镜和能量色散X射线元素分析(EDX)来研究人类磨牙的深层牙本质龋损,以确定龋损的不同区域、范围及其化学组成。将16颗有深层牙本质龋损的离体牙包埋在Technovit 9100(库尔泽公司)中,制作80微米厚的连续切片。然后用偏光显微镜检查这些切片,以识别龋损的不同区域。连续描绘这些区域的轮廓,并进行三维重建,以确定范围并计算不同区域的体积。根据脱矿牙本质和透明层的体积计算出牙本质脱矿指数(DDI)。然后对每个龋损的三个切片进行碳涂层处理,并用扫描电子显微镜进行研究。牙齿的三维重建显示,透明层相当稳定,但被死区残余中断,脱矿牙本质的体积差异很大。因此,随着脱矿牙本质尺寸的增加,DDI也增加。在管间牙本质区域使用能量色散X射线分析(EDX)测量化学组成。所有区域中钙、磷和碳的含量有显著差异。健康牙本质和脱矿牙本质之间的钙磷比有显著差异。从结果中我们得出结论,透明层和脱矿牙本质的管间牙本质矿物质含量与健康牙本质不同,透明层独特的矿化模式是对龋病攻击的生物学反应。由于活跃的牙本质病变表现出许多未封闭的开放牙本质小管,因此在形态学上无法阻止进一步的细菌入侵,或者在进行牙本质治疗时,粘结剂向牙髓的渗透,因此具有临床重要性。