A fourier transform infrared spectroscopic and solid-state NMR study of bone mineral in osteogenesis imperfecta.
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.
Cassella
J P
JP
Division of Biology, School of Environmental and Applied Sciences, University of Derby, UK.
Barrie
P J
PJ
Garrington
N
N
Ali
S Y
SY
D000293:Adolescent; D000328:Adult; D015519:Bone Density; D001842:Bone and Bones / Q000473:pathology / Q000503:physiopathology; D005260:Female; D006801:Humans; D009682:Magnetic Resonance Spectroscopy / Q000379:methods; D008297:Male; D010013:Osteogenesis Imperfecta / Q000473:pathology / Q000503:physiopathology*; D010761:Phosphorus Radioisotopes; D017550:Spectroscopy, Fourier Transform Infrared / Q000379:methods
D010761:Phosphorus Radioisotopes