Darendeliler M A, Kharbanda O P, Chan E K M, Srivicharnkul P, Rex T, Swain M V, Jones A S, Petocz P
Department of Orthodontics, Faculty of Dentistry, University of Sydney, Sydney, Australia.
Orthod Craniofac Res. 2004 May;7(2):79-97. doi: 10.1111/j.1601-6343.2004.00281.x.
To study the effect of different orthodontic force levels on cementum, investigating from the point of view of its physical properties, alterations in the mineral components, type and location of the resorption craters and the exploration in 3D of space.
In vivo human premolars subjected to heavy and light forces were employed for this study. After a period of movement they were analyzed for hardness and elasticity. Also, the mineral composition measuring Ca, P and F of the cementum root surface was investigated. A new method for volumetric analysis of resorption craters was developed.
There were no significant differences for hardness and elastic modulus between the light and heavy force groups and no significant effects for different tooth positions. Significant inter-individual variation in the Ca, P and F concentrations was noted. Force-related data showed that mean volume of the resorption crater in light-force group was 3.49-fold greater than the control group, and the heavy-force group 11.59-fold more than control group. The heavy force group had 3.31-fold greater total resorption volume then light force group. Buccal cervical and lingual apical regions demonstrated significantly more resorption craters than the other regions. The 2D measurements were strongly correlated to 3D measurements.
The application of light and heavy forces did not show any statistically significant differences in hardness and elastic modulus when compared with untreated teeth. The inconsistent increase or decrease of Ca, P and F contents between control and experimental teeth at sites of compression and tension were difficult to explain. There was more resorption by volume in the heavy force group as compared with the light group and controls. Our data also suggested that the high-pressure zones might be more susceptible to resorption after 28 days of force application.
从物理性质、矿物质成分变化、吸收凹坑的类型和位置以及三维空间探索的角度,研究不同正畸力水平对牙骨质的影响。
本研究采用体内受重力和轻力作用的人类前磨牙。经过一段时间的移动后,对其硬度和弹性进行分析。此外,还研究了测量牙骨质根面钙、磷和氟的矿物质成分。开发了一种用于吸收凹坑体积分析的新方法。
轻力组和重力组之间的硬度和弹性模量无显著差异,不同牙位也无显著影响。注意到钙、磷和氟浓度存在显著的个体间差异。与力相关的数据显示,轻力组吸收凹坑的平均体积比对照组大3.49倍,重力组比对照组大11.59倍。重力组的总吸收体积比轻力组大3.31倍。颊侧颈部和舌侧根尖区域的吸收凹坑明显多于其他区域。二维测量与三维测量高度相关。
与未处理的牙齿相比,施加轻力和重力在硬度和弹性模量方面未显示出任何统计学上的显著差异。对照牙和实验牙在压缩和拉伸部位钙、磷和氟含量的不一致增减难以解释。与轻力组和对照组相比,重力组的吸收体积更大。我们的数据还表明,在施加力28天后,高压区可能更容易发生吸收。