Kodaka T, Debari K, Yamada M
Second Department of Oral Anatomy, School of Dentistry, Showa University, Tokyo, Japan.
Scanning Microsc. 1991 Sep;5(3):713-21.
Twenty one extracted human teeth with dental calculi on the enamel and cementum surfaces, fixed in 10% neutral formaldehyde, were selected for this study. After ethanol dehydration and air drying, these calculi were removed by tweezers to observe the teeth surfaces under them. The inspection of these surfaces using SEM and EDX revealed hexahedrally based crystals including pseudocuboidal, rhombohedral and variable rugged rocky shapes. These crystals were identified as Mg-containing whitlockite. The pseudocuboidal crystals, measuring about 4.5 microns in maximum length, were widely distributed on the cervical enamel surface previously covered by calculus. On the root surface, however, these areas decreased remarkably; the shapes changed from pseudocubes into rhombohedrons and rugged rocky structures, while their sizes were smaller and the Mg content decreased. The difference in frequency and morphological variation of the hexahedrally based crystals might be caused by the different characteristics of enamel and cementum surfaces and the Mg present on these surfaces.
本研究选取了21颗牙釉质和牙骨质表面有牙结石的拔除人类牙齿,将其固定于10%中性甲醛中。经乙醇脱水并风干后,用镊子去除这些牙结石,以观察其下方的牙齿表面。使用扫描电子显微镜(SEM)和能谱仪(EDX)对这些表面进行检查,发现了基于六面体的晶体,包括伪立方体、菱面体和形状各异的粗糙岩石状。这些晶体被鉴定为含镁白磷钙石。最大长度约为4.5微米的伪立方体晶体广泛分布在先前被牙结石覆盖的颈部牙釉质表面。然而,在牙根表面,这些区域显著减少;形状从伪立方体变为菱面体和粗糙的岩石结构,同时尺寸变小且镁含量降低。基于六面体的晶体在频率和形态变化上的差异可能是由牙釉质和牙骨质表面的不同特性以及这些表面上存在的镁所导致的。