Kodaka T, Hirayama A, Miake K, Higashi S
Second Department of Oral Anatomy, School of Dentistry, Showa University, Tokyo, Japan.
Scanning Microsc. 1989 Sep;3(3):843-53; discussion 853-4.
In human supra- and subgingival calculus, bacillus-shaped deposits showing various rocky-pile forms composed of hexahedrally based crystals were observed by scanning electron microscopy. The crystal size measured approximately 0.1-1.5 microns. The electron probe microanalysis always detected calcium, phosphorous, and magnesium. Their molar ratios resembled those of magnesium-containing whitlockite and moreover the crystals also gave the electron diffraction pattern of whitlockite. The bacillus-shaped deposits happened to coexist with the intracellular calcifying microorganisms, furthermore, oral microorganisms partially replaced by the hexahedrally based crystals were found. The crystal deposits were never seen in the surface layers of calculus exposed to the oral cavity, but occurred in the innermost layers and intra-spaces of supragingival and ledge-type subgingival calculus and in the outer layers of deep subgingival calculus.
在人类龈上和龈下牙石中,通过扫描电子显微镜观察到呈杆菌状的沉积物,其呈现出由六面体晶体构成的各种石堆状形态。晶体大小约为0.1 - 1.5微米。电子探针微分析始终检测到钙、磷和镁。它们的摩尔比类似于含镁的白磷钙矿,而且这些晶体还给出了白磷钙矿的电子衍射图谱。杆菌状沉积物恰好与细胞内钙化微生物共存,此外,还发现部分被六面体晶体取代的口腔微生物。晶体沉积物从未在暴露于口腔的牙石表层中见到,而是出现在龈上和壁架型龈下牙石的最内层和内部间隙以及深部龈下牙石的外层。