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体外再矿化后牙本质的机械回收——压痕研究。

Mechanical recovery of dentin following remineralization in vitro--an indentation study.

机构信息

Division of Biomaterials and Bioengineering, Department of Preventive and Restorative Dental Sciences, University of California, San Francisco, CA 94143-0758, USA.

出版信息

J Biomech. 2011 Jan 4;44(1):176-81. doi: 10.1016/j.jbiomech.2010.09.005.

Abstract

This study sought to gain insights into the steps leading to remineralization and mechanical recovery of hydrated dentin. Mechanical recovery in water was hypothesized to result from effective mineral matrix binding and to occur from the innermost regions outwards due to an increase in the number of nucleation sites. Partially demineralized (0.05 M acetate, pH=5.0, 8h) dentin was remineralized using calcium and phosphate solutions of 10.1 or 9.8 degree of saturation (DS) for hydroxyapatite (pH=7.4) for 4, 8 or 24h. Remineralization used a constant solution composition approach, which allowed for a continuous mineral growth with relatively constant thermodynamic driving forces. Crystal growth rates (R) were calculated using concentrations of calcium and phosphate. Before and after de- and re-mineralization, specimens had their surface and cross-section elastic moduli measured using AFM-nanoindentation in water. DS=10.1 provided higher R and higher mechanical recovery at the surface (p<0.0001). Cross-sectional measurements showed that subsurface mechanical recovery occurred from the innermost demineralized areas gradually outwards for both groups with no statistical differences at different DS, thus suggesting that remineralization is driven by mineral growth within nucleation sites with preserved collagen fibrils. Further, mechanical recovery appeared to initially obey a heterogeneous pattern, which vanished with time. This study provides evidence of mechanical recovery of hydrated dentin after remineralization and novel insights into the steps leading to mechanical recovery of carious dentin.

摘要

本研究旨在深入了解牙本质再矿化和机械恢复的步骤。假设水合牙本质的机械恢复是由于有效矿化基质结合的结果,并由于成核位点数量的增加而从最内层向外发生。用钙和磷酸盐溶液(pH=7.4)对部分脱矿(0.05 M 乙酸盐,pH=5.0,8h)的牙本质进行再矿化,溶液的饱和度(DS)为 10.1 或 9.8 用于羟磷灰石。再矿化采用恒定溶液组成方法,允许相对恒定的热力学驱动力下连续的矿物生长。使用钙和磷酸盐的浓度计算晶体生长速率(R)。在脱矿和再矿化前后,使用 AFM 纳米压痕在水中测量标本的表面和横截面弹性模量。DS=10.1 提供了更高的 R 和更高的表面机械恢复(p<0.0001)。横截面测量显示,两组的亚表面机械恢复均从最内层脱矿区逐渐向外进行,不同 DS 之间无统计学差异,这表明再矿化是由保留胶原纤维的成核位点内的矿物质生长驱动的。此外,机械恢复似乎最初遵循非均匀模式,随着时间的推移而消失。本研究为牙本质再矿化后牙本质水合的机械恢复提供了证据,并为龋齿牙本质机械恢复的步骤提供了新的见解。

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