作者: E.D. Eanes , I. Zipkin , R.A. Harper , A.S. Posner
DOI: 10.1016/0003-9969(65)90068-3
关键词: Analytical chemistry 、 Crystallography 、 X-ray crystallography 、 Fluoride 、 Bone mineral 、 Materials science 、 Crystallinity 、 Crystallite 、 Apatite 、 Diffraction 、 Bone tissue 、 Cell biology 、 Otorhinolaryngology 、 General Dentistry 、 General Medicine
摘要: Abstract Small-angle X-ray diffraction studies were performed on a series of human rib samples containing varying amounts fluoride. The results show that rise in fluoride content was accompanied by decrease the area interface between mineral apatite phase and remaining bone tissue. Detailed analysis suggest this can only be accomplished an increase mean volume concomitant number crystallites. Further considerations improvement “crystallinity” as measured wide-angle diffraction, reported previous publications, accounted for entirely crystallite size. Apparently these progressive changes tolerated individual without producing significant physiological consequences.