Intrafibrillar mineral may be absent in dentinogenesis imperfecta type II (DI-II)

被引:47
作者
Kinney, JH
Pople, JA
Driessen, CKH
Breunig, TM
Marshall, GW
Marshall, SJ
机构
[1] Univ Calif San Francisco, Dept Prevent & Restorat Dent Sci, San Francisco, CA 94143 USA
[2] Stanford Synchrotron Radiat Lab, Stanford, CA 94309 USA
[3] Univ Pretoria, Dept Restorat Dent, ZA-0002 Pretoria, South Africa
关键词
dentin; dentinogenesis imperfecta; mineralization; small angle scattering; synchroton radiation;
D O I
10.1177/00220345010800061501
中图分类号
R78 [口腔科学];
学科分类号
1003 ;
摘要
High-resolution synchrotron radiation computed tomography (SRCT) and small-angle x-ray scattering (SAXS) were performed on normal and dentinogenesis imperfecta type II (DI-II) teeth. The SRCT showed that the mineral concentration was 33% lower on average in the DI-II dentin with respect to normal dentin. The SAXS spectra from normal dentin exhibited low-angle diffraction peaks at harmonics of 67.6 nm, consistent with nucleation and growth of the apatite phase within gaps in the collagen fibrils (intrafibrillar mineralization). In contrast, the low-angle peaks were almost non-existent in the DI-II dentin. Crystallite thickness was independent of location in both DI-II and normal dentin, although the crystallites were significantly thicker in DI-II dentin (6.8 nm [SD = 0.5] vs. 5.1 run [SD = 0.6]). as determined The shape factor of the crystallites, by SAXS, showed a continuous progression in normal dentin from roughly one-dimensional (needle-like) near the pulp to two-dimensional (plate-like) near the dentin-enamel junction. The crystallites in DI-II dentin, on the other hand, remained needle-like throughout. The above observations are consistent with an absence of intrafibrillar mineral in DI-II dentin.
引用
收藏
页码:1555 / 1559
页数:5
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