Hiraide F, Nomura Y
Laryngoscope. 1980 Jan;90(1):152-8. doi: 10.1288/00005537-198001000-00016.
Salivary calculi were formed by a laminated mixture of inorganic and organic substancs. However, there was no regular pattern for the growth of stones, as laminal thickness and the arrangement of the laminal component were not uniform. Finger-like radial projections, longitudinal pavements or amorphous structures were seen on the fractured surface of the calculi. No inert foreign body or microorganism was found in the calculi. There were two modes of formation in calculous nucleus, one developed by maturation of a primitive core, the other formed in homogenous mineral mass. X-ray microanalysis proved that most salivary calculi contained chemical elements such as calcium, phosphorous, potassium, sodium, magnesium, chlorine, sulfur, manganese, chromium and aluminum. As far as we have examined, these elements were distributed with almost equal density throughout the calculus.
唾液结石由无机和有机物质的层状混合物形成。然而,结石的生长没有规律模式,因为层的厚度和层状成分的排列并不均匀。在结石的断裂面上可见指状放射状突起、纵向铺砌结构或无定形结构。在结石中未发现惰性异物或微生物。结石核心有两种形成方式,一种由原始核心成熟发育而来,另一种在均匀矿物质团块中形成。X射线微分析证明,大多数唾液结石含有钙、磷、钾、钠、镁、氯、硫、锰、铬和铝等化学元素。就我们所检查的情况而言,这些元素在整个结石中分布密度几乎相等。