Kodaka T, Ohohara Y, Debari K
Second Department of Oral Anatomy, School of Dentistry, Showa University, Tokyo, Japan.
Scanning Microsc. 1992 Jun;6(2):475-85; discussion 485-6.
Dental calculus formed after 10 days on resin plates, applied to the lingual sides of the mandibular gingival regions in eight human subjects, was investigated by means of scanning electron microscopy (SEM) and energy-dispersive X-ray microanalysis (EDX). The mineral deposits were mainly divided into three types: A, B, and C. The type A deposits showing an average Ca/P molar ratio of 1.42 were densely packed with fine needle-shaped crystals formed by the intra- and extra-cellular calcification. The type A deposits, probably composed of Ca-deficient apatites and the transitional forms between apatite and octacalcium phosphate (OCP), were observed in all subjects. The type B deposits showing an average Ca/P molar ratio of 0.96 were aggregated with polygonal column, triangular plate-shaped, and rhombohedral crystals. These crystals identified as brushite (CaHPO4-2H2O:dicalcium phosphate dihydrate: DCPD) were found in four subjects. Platelet-shaped crystals of the type C deposits were observed in three subjects. Their Ca/P molar ratio of 1.26 and the crystal shape were similar to those of OCP. Whitlockite crystals were not found although Mg-containing hexagonal disk-like crystals were observed in two subjects.
对八名人类受试者下颌牙龈区域舌侧树脂板上10天后形成的牙结石,通过扫描电子显微镜(SEM)和能量色散X射线微分析(EDX)进行了研究。矿物质沉积物主要分为三种类型:A、B和C。A型沉积物的平均钙/磷摩尔比为1.42,由细胞内和细胞外钙化形成的细针状晶体紧密堆积。在所有受试者中均观察到A型沉积物,其可能由缺钙磷灰石以及磷灰石和磷酸八钙(OCP)之间的过渡形式组成。B型沉积物的平均钙/磷摩尔比为0.96,由多边形柱状、三角形板状和菱面体晶体聚集而成。在四名受试者中发现了这些被鉴定为透钙磷石(CaHPO4·2H2O:磷酸二钙二水合物:DCPD)的晶体。在三名受试者中观察到了C型沉积物的血小板状晶体。其钙/磷摩尔比为1.26,晶体形状与OCP相似。尽管在两名受试者中观察到了含镁的六边形盘状晶体,但未发现白磷钙矿晶体。