Mode of Occurrence of Brushite and Whitlockite in a Sialolith-Reference-Cited by-同舟云学术

Mode of Occurrence of Brushite and Whitlockite in a Sialolith

Published:1981-04 Issue:4 Volume:60 Page:842-844
ISSN:0022-0345
Container-title:Journal of Dental Research
language:en
Short-container-title:J Dent Res

Author:

Sakae Toshiro¹,Yamamoto Hirotsugu²,Hirai Goro¹

Affiliation:

1. Department of Oral Histology and Clinical pathology

2. Nihon University School of Dentistry at Matsudo, Matsudo, Chiba 271, Japan

Abstract

A micro-focus X-ray diffractometer was applied to a ground section of sialolith, and localization of brushite and whitlockite was found. The sialolith was composed of a central core of organic material and a layered cortex of mineral components. The major component of the mineral cortex is apatite. Brushite and whitlockite locate independently at the surface layer of the cortex.

Publisher

SAGE Publications

Subject

General Dentistry

Link

http://journals.sagepub.com/doi/pdf/10.1177/00220345810600041401

Reference10 articles.

1. Rowles, S.L.: The Inorganic Composition of Dental Calculus. In: Bone and Tooth Proceedings, First European Symposium, H.J.J. Blackwood, Ed. London: Pergamon Press, 1964, pp. 175-183.

2. Stages of calcium phosphate crystallisation during calculus formation

3. X-Ray Crystallographic Examination of Calculi from Salivary Glands

4. Crystallography of Dental Calculus and the Precipitation of Certain Calcium Phosphates

5. The Source of Mineral Salts in Subgingival Calculus

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