从患有复发性石灰石病的患者中提取的石灰石的基本特征
Buyanbileg Sodnom-Ish1, Mi Young Eo1, Kezia Rachellea Mustakim1
1Department of Oral and Maxillofacial Surgery, Dental Research Institute, School of Dentistry, Seoul National University, Seoul, Korea.
复发性石,或唾液结石,涉及细菌和炎症外体形成分层结构. 这一案例凸显了剩余的石块碎片如何可能导致岩石的快速重新形成.
科学领域:
- 口腔医学是指口腔医学.
- 病理学 病理学 病理学
- 生物材料科学 生物材料科学
背景情况:
- 石灰石形成机制尚不清楚,罕见的复发率 (1% - 10%).
- 这项研究研究了一例独特的快速,反复复发的下腺质病例.
研究的目的:
- 为了阐明反复复发的小石形成的病原遗传过程.
- 确定参与唾液结石发展的关键组成部分.
主要方法:
- 组织学,扫描电子显微镜 (SEM),能量分散光谱 (EDS) 和传输电子显微镜 (TEM) 都被采用.
- 分析来自单个患者下下腺的复发性小炎.
主要成果:
- 这些石头呈现出三层结构:一个中心的,一个高度矿化的中间层,以及一个外围的多层区域.
- 在元素分析中,发现了Ca,C,O,Cu,F,N,P,Si,Zn和Zr.
- 在石头结构内,TEM确定了细菌细胞膜和炎症外体,特别是在外围和中心区域.
结论:
- 酸盐的形成涉及细菌,炎症外体和脱皮的唾液上皮细胞的复杂相互作用.
- 快速复发可能归因于剩余的石碎片,作为细菌感染和随后的石头生长的巢穴.
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