Mineralogy of a calcite sputum lith

H. Kano, Y. Goto, Y. Niitsu, Y. Maruyama
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引用次数: 0

Abstract

A rare case of calcite sputum lith coughed up from the bronchus of a 38-yr-old male subject has been investigated mineralogically. The sputum liths are milky white, sandy grains of 1-3mm in size with “confetto”-like appearance. Under the polarized microscope, they make polycrystalline aggregate. According to the microdiffractometric as well as x-ray microprobe analytic investigation, the mineral has been proved to be almost pure calcite composed of (Ca0.97-0.98Mg0.03-0.02)CO3 with slight compositional zoning. The P-content is only traceable. So any contribution from bone material may be scarecely conceivable. The genetic origin of sputum lith is still remains unknown.
方解石痰岩的矿物学
本文报道一例38岁男性受试者支气管咳出方解石痰石的罕见病例,并进行了矿物学研究。痰石呈乳白色,沙质颗粒,大小1-3mm,呈“五彩纸屑”状。在偏光显微镜下,它们形成多晶聚集体。经显微衍射和x射线显微探针分析,证实该矿物为由(Ca0.97-0.98Mg0.03-0.02)CO3组成的几乎纯方解石,具有轻微的成分分带。磷含量只能溯源。因此,骨骼材料的任何贡献都是难以想象的。痰石的遗传起源仍然是未知的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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