Kodaka T, Debari K, Sano T, Yamada M
Second Department of Oral Anatomy, School of Dentistry, Tokyo, Japan.
Scanning Microsc. 1994;8(2):241-56; discussion 256-7.
Human calcium phosphate calculi: two sialoliths, a urolith, a rhinolith, and a tonsillolith were investigated by scanning electron microscopy (SEM) and energy-dispersive X-ray analysis (EDX). The sialoliths and urolith had appositional shells with thick cortices, respectively, around several nuclei composed of calcospherulites and a rubber-film fragment. The rhinolith had a thin cortex with appositional laminations around a glomerulus-like mass of calcified cotton-like strings. The tonsillolith had a rough cortex with appositional laminations. Its porous interior was composed of numerous calcified conglomerates with microorganisms and calcified masses with fine appositional laminations around the conglomerates. The major crystals were identified as biological apatites (AP) with a sand-grain rather than a needle-like shape, and plate-shaped octacalcium phosphate (OCP). The AP deposits of the rhinolith probably were associated with magnesium (Mg) phosphates or contained Mg. No OCP was found in the rhinolith. The AP deposits were mainly formed by extracellular calcification. Hexahedral crystals, identified as Mg-containing whitlockite (WH), were precipitated in the internal spaces of the AP and OCP deposits. The rhinolith nucleus consisted of WH crystal deposits only.
通过扫描电子显微镜(SEM)和能量色散X射线分析(EDX)对两颗涎石、一颗尿路结石、一颗鼻石和一颗扁桃体结石进行了研究。涎石和尿路结石分别在由球雏晶和橡胶膜碎片组成的几个核心周围有具有厚皮质的附着壳。鼻石在类似肾小球的钙化棉状条索团块周围有带附着层的薄皮质。扁桃体结石有带附着层的粗糙皮质。其多孔内部由众多带有微生物的钙化团块和围绕团块的带有精细附着层的钙化块组成。主要晶体被鉴定为具有沙粒状而非针状形状的生物磷灰石(AP)和板状磷酸八钙(OCP)。鼻石的AP沉积物可能与磷酸镁(Mg)有关或含有Mg。在鼻石中未发现OCP。AP沉积物主要通过细胞外钙化形成。被鉴定为含镁白磷钙石(WH)的六面体晶体沉淀在AP和OCP沉积物的内部空间中。鼻石核心仅由WH晶体沉积物组成。