Infrared determination of the degree of substitution of hydroxyl by carbonate ions in human dental enamel

About 11 +/- 1% of the carbonate ions in a human tooth enamel specimen (dense fraction, sp. g. greater than 2.95) were found to be in the A-sites, replacing hydroxyl ions. The determination was made with a difference infrared spectrometry technique utilizing both tooth enamel and a reconstituted bio...

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Bibliographic Details
Published inCalcified tissue international Vol. 37; no. 4; p. 372
Main Authors Elliott, J C, Holcomb, D W, Young, R A
Format Journal Article
LanguageEnglish
Published United States 01.07.1985
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Summary:About 11 +/- 1% of the carbonate ions in a human tooth enamel specimen (dense fraction, sp. g. greater than 2.95) were found to be in the A-sites, replacing hydroxyl ions. The determination was made with a difference infrared spectrometry technique utilizing both tooth enamel and a reconstituted biological apatite with a known amount of replacement of hydroxyl by carbonate ions.
ISSN:0171-967X
DOI:10.1007/bf02553704