1991
DOI: 10.1016/s0006-3495(91)82113-0
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Novel infrared spectroscopic method for the determination of crystallinity of hydroxyapatite minerals

Abstract: Biologically important apatite analogues have been examined by Fourier Transform Infrared Spectroscopy (FT-IR), and a method developed to quantitatively assess their crystalinity. Changes in the phosphate v1 and v3 regions, 900-1,200 cm-1, for a series of synthetic (containing hydroxide, fluoride, or carbonate ion) and biological apatites with crystal sizes of 100-200 A were analyzed with curve-fitting and second derivative spectroscopy. The v1,v3 contour was composed of three main subbands. Correlations were … Show more

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Cited by 351 publications
(291 citation statements)
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“…The mineral content decrease observed in the present study is much steeper than could be explained by the difference in the relative density of peritubular dentin alone, supporting the distinct nature of mantle dentin. The width of the mantle dentin zone (based here on its distinct mineral properties relative to the rest of dentin) has been a subject of controversy in addition to debate about its relative mineral and matrix content [7,[25][26]. In our results, mantle dentin in bovine incisors was represented by an 80-100μm wide strip, in agreement with earlier data [5].…”
Section: Discussionsupporting
confidence: 90%
“…The mineral content decrease observed in the present study is much steeper than could be explained by the difference in the relative density of peritubular dentin alone, supporting the distinct nature of mantle dentin. The width of the mantle dentin zone (based here on its distinct mineral properties relative to the rest of dentin) has been a subject of controversy in addition to debate about its relative mineral and matrix content [7,[25][26]. In our results, mantle dentin in bovine incisors was represented by an 80-100μm wide strip, in agreement with earlier data [5].…”
Section: Discussionsupporting
confidence: 90%
“…These peculiarities of MgHA/Coll can be similarly observed in the FTIR spectrum of young bone; while they tend to disappear in mature bone and in highly crystalline synthetic apatite [28][29][30]. Correlation was noted between the fractional intensity of ~1050 cm -1 band related to PO 4 3-group and the crystal size of the apatite: a reduction of the apatitic crystal size induced an increase of the percentage area of this component [31,32]. All these features indicate that the mineral phase containing Mg ions and nucleated on the natural template (collagen) is non-stoichiometric and remarkably amorphous resembling very well the features of newly deposited bone mineral.…”
Section: Development and Characterization Of The Lower (Bony) And Intmentioning
confidence: 56%
“…[18], carbonate-phosphate ratio (890 -850 cm -1 / 1200 -900 cm -1 ) [19], crystallinity (1030/1020 cm -1 ) [20,21], collagen maturity (1660/1690 cm -1 ) [22] and acid phosphate (1127/1096 cm -1 ) [23]. Furthermore, the spatial heterogeneity of each parameter was determined from the full width of half maximum (FWHM) of the Gaussian curve fitted to the pixel histogram of the measured area [24].…”
Section: Ftirmentioning
confidence: 99%