Low-frequency Raman spectroscopy
was used to characterize
variably
substituted hydroxyapatites with Sr2+, F–, and CO3
2– as the substituting species
in the crystalline and amorphous forms. These samples were characterized
for substitution and crystallinity using methods previously explored
in the literature (XRPD, IR, and Raman spectroscopy) to demonstrate
a range of substitutions, and the levels of crystallinity were achieved.
The sample series was characterized with low-frequency Raman spectroscopy
where clear differences between amorphous and crystalline forms along
with systematic changes in the crystalline spectra with the level
of substitution were observed. Solid-state density functional theory
was used to identify and characterize the observed low-frequency Raman
modes, and principal component analysis further explored the trends
in the data set. A new crystallinity index (CI) was proposed using
the ratio of intensities at 140 and 110 cm–1 (CILFRintensityStokes) or −140 and −110 cm–1 (CILFRintensityanti‑Stokes). When correlated to
the XRPD-based CI, better correlation was observed with CILFRintensityStokes (NRMSE = 0.11, R
2 = 0.85) and CILFRintensityanti‑Stokes (NRMSE = 0.11, R
2 = 0.88) compared to the previously used CIIR (NRMSE = 0.24, R
2 = 0.03) or CIRaman (NRMSE = 0.15, R
2 = 0.66)
methods, which were particularly sensitive to the degree of substitution
interfering with the level of crystallinity, thus making this a promising
method for estimating crystallinity when dealing with variably substituted
apatites.