Dahm S, Furseth R
Calcif Tissue Res. 1976 Oct 12;21(2):115-20. doi: 10.1007/BF02547387.
Analysis of human dentine by infrared spectrophotometry suggests that ball-grinding may result in damage of the apatite crystallites. The present study includes further assessments of this effect by X-ray diffraction, infrared spectroscopy, and electron microscopy. Each of three coarse-ground dentine samples (Group I) was divided into three portions of 30 mg. One of these portions was ball-ground for approximately 1 min (Group II), the second portion for 6 min (Group III), and the third portion for 23 min (Group IV). The 002 reflection showed line broadening, most marked from Group II to III. Electron microscopy showed a gradual change in crystallite appearance with increased grinding, most pronounced from Group II to III. These observations indicate that by prolonged grinding a limit is approached where no further changes in the crystallites occur. Electron microscopy also indicated that fracture of the crystallites might have occurred. This was probably accompanied by strains in the lattice. The infrared spectra indicated that no breakdown of the apatite structure had occurred during the entire grinding.
通过红外分光光度法对人牙本质进行分析表明,球磨可能会导致磷灰石微晶受损。本研究通过X射线衍射、红外光谱和电子显微镜对这种效应进行了进一步评估。三个粗磨牙本质样本(第一组)中的每一个都被分成三份,每份30毫克。其中一份进行约1分钟的球磨(第二组),第二份进行6分钟的球磨(第三组),第三份进行23分钟的球磨(第四组)。002反射显示出线宽化,从第二组到第三组最为明显。电子显微镜显示,随着研磨时间的增加,微晶外观逐渐变化,从第二组到第三组最为显著。这些观察结果表明,通过长时间研磨,会接近一个极限,此时微晶不会再发生进一步变化。电子显微镜还表明,微晶可能发生了断裂。这可能伴随着晶格中的应变。红外光谱表明,在整个研磨过程中,磷灰石结构没有发生分解。