Mishima H, Yamamoto H, Sakae T
Department of Anatomy, Nihon University School of Dentistry, Chiba, Japan.
Scanning Microsc. 1992 Jun;6(2):487-93; discussion 493-4.
Ten salivary stones in the human submandibular gland were investigated by scanning electron microscopy-energy dispersive spectroscopy (SEM-EDS) and X-ray diffraction analyses. The stones usually showed a lamellar pattern. SEM observations revealed cubical, plate-like, granular, small and large granules, polyhedral or globular structures in these stones. By X-ray powder diffraction analysis, the main constituents of salivary stones were found to be apatite and whitlockite. SEM-EDS analyses showed that Ca and P were the major elements, frequently accompanied by Mg and S, and less frequently by Na, Al, Si, Cl, K, Fe, Cu and Zn. Ca/P molar ratios ranged from 1.00 to 2.00 with the average of 1.53, showing two maxima of about 1.50 and 1.60. The Ca/P molar ratio of about 1.50 corresponded to the value of whitlockite. The Ca/P molar ratio of 1.60 corresponded approximately to the value of apatite.
通过扫描电子显微镜-能量色散光谱(SEM-EDS)和X射线衍射分析,对人类下颌下腺中的10颗涎石进行了研究。这些结石通常呈现出层状结构。扫描电子显微镜观察显示,这些结石中存在立方体、板状、颗粒状、大小颗粒、多面体或球状结构。通过X射线粉末衍射分析,发现涎石的主要成分是磷灰石和白磷钙矿。SEM-EDS分析表明,钙(Ca)和磷(P)是主要元素,常伴有镁(Mg)和硫(S),较少伴有钠(Na)、铝(Al)、硅(Si)、氯(Cl)、钾(K)、铁(Fe)、铜(Cu)和锌(Zn)。钙/磷摩尔比范围为1.00至2.00,平均为1.53,呈现出约1.50和1.60的两个最大值。钙/磷摩尔比约为1.50对应于白磷钙矿的值。钙/磷摩尔比为1.60大约对应于磷灰石的值。