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  1. 松本歯学(Print edition:ISSN 0385-1613 Online edition:ISSN 2188-7233)
  2. 8巻(1982)
  3. 1号

硬化象牙質に関する電子顕微鏡的研究 第2報 歯冠硬化象牙質の細管内沈着物と歯石および唾石との比較

https://mdu.repo.nii.ac.jp/records/319
https://mdu.repo.nii.ac.jp/records/319
0ec92c03-4bf3-4f2a-8c05-816e879dcb28
名前 / ファイル ライセンス アクション
matsumoto_shigaku_08-01-04.pdf matsumoto_shigaku_08-01-04.pdf (8.6 MB)
Item type Journal Article(1)
公開日 2012-05-23
タイトル
タイトル 硬化象牙質に関する電子顕微鏡的研究 第2報 歯冠硬化象牙質の細管内沈着物と歯石および唾石との比較
言語
言語 jpn
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
その他(別言語等)のタイトル
その他のタイトル Electron-microscopical Studies on the Sclerosed Dentin Second Report : Comparative observations on the intertubular deposits in the coronal dentin, dental calculus and salivary stone
著者 赤羽, 章司

× 赤羽, 章司

赤羽, 章司
枝, 重夫
川上, 敏行
中村, 千仁
河住, 信

抄録
内容記述タイプ Abstract
内容記述 For the purpose of serchirg the origin of the intratubular deposits in the coronal sclerosed dentin, the deposits were compared with dental calculus and salivary stone by a scanning electron microscope and electron probe microanalysers with energy and wavelength dispersive x-ray spectroscopies including the contour map method. Results were as follows: 1. The layer of minute crystals covered on the attrition surface contained the elements of Na, Mg, Al, P, S, Cl, Ca, Mn, Fe, Zn, Br. 2. The rhombohedral crystals in the dentinal tubules contained the elements of F, Na, Mg, P, S, Cl, Ca. 3. The hypo-and hyper-calcified areas and leptothrichia, whether calcified or not, were observed on the dental calculus. An analysis on the surface layer showed that it contained the elements of F, Na, Mg, Al, Si, P, S, K, Ca, Zn. Mg had a tendency to increase in hypocalcified area. 4. On the fractured surface of dental calculus, the stratified stractures, calcified leptothrichia, plate-like crystals and hexagonal cuboidal crystals were observed. These consisted of the elements of Na, Mg, Si, P, S, Cl, Ca, Zn. The crystals were much abundant in Mg. 5. A lamella stracture, indeterminate and hexagonal crystals, and rod-shaped stractures were observed on the surface of salivary stones. The elements of these surface stractures were Na, Zn, As, Br, In, Sn, Pb. 6. The stratified stractures being composed of hypo-and hyper-calcification, minute granular, rod-shaped, plate-like and globular crystals were seen on the fractured surface of salivary stones and contained the elements of F, Na, Mg, Al, P, S, Cl, Ca, Cr, Cu, As, Se, Pd, In, I, Au, Hg, Pb. The hypocalcified area was much abundant in S. 7. According to the contour map of dental calculus with the teeth, dental calculi were more abundant in P and Ca than cementum and dentin. The contour map showed that the Ca contents and the stratified stractures closely correlated. 8. The contour maps showed more clearly than x-ray images that the contents of P, S, and Ca and the stratified stractures correlared. 9. The elements of intratubular deposits in the coronal sclerosed dentin were considered to come from saliva because the stracture and elements of crystals reratively resembled to those of dental calculi.
書誌情報 松本歯学

巻 8, 号 1, p. 23-50, 発行日 1982-06-30
出版者
出版者 松本歯科大学学会
ISSN
収録物識別子タイプ ISSN
収録物識別子 0385-1613
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00232590
フォーマット
内容記述タイプ Other
内容記述 application/pdf
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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