2021
DOI: 10.1007/s00223-021-00825-4
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Measures of Bone Mineral Carbonate Content and Mineral Maturity/Crystallinity for FT-IR and Raman Spectroscopic Imaging Differentially Relate to Physical–Chemical Properties of Carbonate-Substituted Hydroxyapatite

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Cited by 34 publications
(40 citation statements)
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“…These peaks have the lowest width in the spectrum of stoichiometric HAp (sample H S ). It is known [32,33,40,46,53,54] that the increased content of carbonate groups in the hydroxyapatite structure causes the broadening of all bands in its Raman spectrum, resulting in the appearance of a wide band at around 1070 cm −1 with poorly resolved shoulders. This phenomenon is represented in the spectra of the reference samples of nano-cHAp, natural tissues and biocomposites (Figure 4).…”
Section: Raman Spectroscopymentioning
confidence: 99%
See 1 more Smart Citation
“…These peaks have the lowest width in the spectrum of stoichiometric HAp (sample H S ). It is known [32,33,40,46,53,54] that the increased content of carbonate groups in the hydroxyapatite structure causes the broadening of all bands in its Raman spectrum, resulting in the appearance of a wide band at around 1070 cm −1 with poorly resolved shoulders. This phenomenon is represented in the spectra of the reference samples of nano-cHAp, natural tissues and biocomposites (Figure 4).…”
Section: Raman Spectroscopymentioning
confidence: 99%
“…The mode at 1018 cm −1 is also present in the spectrum of natural dentine and is typical for apatite containing divalent ions and vacancies instead of monovalent ions [39]. The broadening of the maximum at about 1070-1075 cm −1 in the spectrum of bioinspired materials is due to the overlap of two vibrational modes: the PO 4 υ 3 stretching mode and the υ 1 mode of the carbonate anion CO 3 2− included in the position of the PO 4 group (B-type substitution), which is typical for biogenic materials [32,33,40,46,53,54]. A low-intensity oscillation in the region of 1103.4 cm −1 is also found in the spectra of samples of natural enamel and dentine of humans.…”
Section: Raman Spectroscopymentioning
confidence: 99%
“…While it would be useful to compare the results of these measurements with other standard techniques, it appears that there are essentially no other acceptable methods to determine the mineral content of a sample of bone. Infra-red analysis (FTIR) of the ratio of PO 4 to amide [2,3] must make assumptions about the composition of the mineral phase. Likewise, the use of back-scattered electron intensity to measure the Ca fraction in a polished section of bone can determine local point-to-point variations in the apparent mineral content but cannot be converted to total mineral content since the composition of the mineral phase is not determined [2,4].…”
Section: Other Methods Of Determinationmentioning
confidence: 99%
“…A região espectral entre 1000 e 1650 cm -1 foi utilizada para investigar os grupos funcionais dos fosfatos de cálcio formados sobre a superfície dos corpos de prova. A escolha dessa região foi realizada com base em estudos anteriores que indicam maior incidência de formação de bandas atribuídas aos fosfatos de cálcio (TAYLOR et al, 2021;SANTOS et al, 2018;REY et al, 2014;KOUTSOPOULOS et al, 2002). Os espectros de FTIR tiveram suas linhas de base corrigidas -com filtro Savitzky-Golay -e depois foram normalizadas e deconvoluídas, utilizando função Gaussiana (R 2 > 0,99), utilizando o software Origin 9.0.0 da OriginLab (ORIGINLAB, NORTHAMPTON, MA).…”
Section: Tratamento Superficial Dos Corpos De Prova Deunclassified
“…As bandas de absorção atribuídas à fase HAp não estequiométrica ou Sr-HAp novamente foram observadas em vibrações do tipo ν3 PO4 3entre ~1157 e 1178 cm -1 (TAYLOR et al, 2021). Bandas entre ~ 1180 e 1210 cm -1 foram observadas e atribuídas às vibrações de estiramento do grupo funcional hidrogenofosfato (ν3 HPO4 2-) (GENG et al, 2016;HORVÁTHOVÁ et al, 2008;KOUTSOPOULOS et al, 2002).…”
Section: β-Tcpunclassified