A semiquantitative electron probe X-ray microanalytical (XRMA) technique, in conjunction with transmission electron microscopy, was used to compare the calcium to phosphorus (Ca/P) molar ratios in calcium phosphate standards of known composition, in normal bone and in bone from patients with osteogenesis imperfecta (OI). Using a modified routine processing and resin embedding schedule, the measured Ca/P molar ratio of calcium phosphates standards of known composition were found to correlate well with the Ca/P molar ratio based on their respective chemical formulae. This technique was then used to compare the Ca/P molar ratio in normal human bone and in OI bone. The Ca/P ratio values for normal bone (Ca/P = 1.631) correlated well with those for chemically prepared hydroxyapatite (Ca/P = 1.602), but in bone from OI patients, the Ca/P molar ratio was significantly lower (Ca/P = 1.488). This study has shown that there is a lower Ca/P molar ratio in OI bone compared with normal, matched bone. This suggests that the mineral deviates from the carbanoapatite usually found in bone. Isomorphous substitutions in the carbanoapatite lattice could account for this although this study has neither proved nor disproved this. The altered bone mineral is another factor that could contribute to the increased fracture rate observed in OI.
Fourier transform infrared spectroscopy and 31P solid-state nuclear magnetic resonance spectroscopy were used to determine if any structural or compositional differences in osteogenesis imperfecta (OI) bone mineral could be detected that might help to explain the bone fragility observed in this disease. A previous study by Cassella et al. used an electron probe X-ray microanalytical technique to compare the calcium to phosphorus (Ca/P) molar ratios in normal bone and bone from patients with OI. It was demonstrated that bone from OI patients had a lower Ca/P molar ratio. This study demonstrated that OI bone mineral had a general hydroxyapatite structure and that isomorphous substitutions in the carbanoapatite lattice could account for the low Ca/P molar ratio.
FT-Raman spectroscopic analysis of eight pigmented specimens from an important Hindu statue group, Kali Walking on Siva, acquired in 1895 but of indeterminate age and now in the Horniman Museum, London, has revealed some interesting and unusual combinations of coloured pigments including cinnabar, minium, lapis lazuli and red ochre. Several specimens showed evidence of organic additives, which have been attributed to shellac resins commonly believed to have been used on this type of statuary. The Raman spectroscopic results confirm that the predominant black pigment on the Kali figure is lamp black or soot, in contrast to the SEM-EDX data that suggests the origin of this pigment as from bone black or ivory black from the presence of phosphorus. An eclectic range of white pigments have been identified in this group including lead white, barytes, calcite and anhydrite; rutile and anatase found on one specimen on the jackal in this group have been ascribed to recent unrecorded restoration.
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