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pH循环处理后的牙釉质和牙本质标本不同深度处的酸敏感性。

Acid susceptibility at various depths of pH-cycled enamel and dentine specimens.

作者信息

Lagerweij M D, ten Cate J M

机构信息

Academic Centre for Dentistry Amsterdam, ACTA, Department of Cariology, Endodontology, Pedodontology, Amsterdam, The Netherlands.

出版信息

Caries Res. 2006;40(1):33-7. doi: 10.1159/000088903.

Abstract

pH-cycling and in situ studies have shown that fluctuations in de-/remineralisation conditions or in fluoride usage can lead to laminations inside enamel or dentine lesions. Layers with different mineral content are thought to reflect the history of fluoride administrations. Studying the dissolution properties of such lesions at various depths -- using bulk specimens -- is presumably hampered by limited diffusion of acids through the lesion pores. Therefore, in this study the acid susceptibility of enamel and dentine lesions and the underlying sound tissues was studied by exposing sections to acid buffers from the cut rather than from the external surface. Specimens were obtained from a previous study of the effects of high-fluoride (0, 1,000, 2,000, 3,000/5,000 ppm F) toothpastes on enamel and dentine de-/remineralisation. Sections were subjected to acid buffers for 3 and 7 days and the changes in mineral content were monitored by contact microradiography. For enamel lesions a significant difference in dissolution over depth was observed between the groups subjected to the different fluoride schemes. At 7 days a dose response was found between the different fluoride groups and the lesion parameters. In the no-fluoride group dissolution in the original lesion and the sound tissue were similar. All dentine lesions which had been treated with fluoride showed inhibition of dissolution, but the inhibition did not increase with higher fluoride concentrations. Deeper into the dentine tissue there was some protection, but it was not statistically significant. We conclude that penetration of fluoride through the lesion pores determines the dissolution pattern of a lesion at various depths.

摘要

pH 循环和原位研究表明,脱矿/再矿化条件或氟化物使用量的波动会导致牙釉质或牙本质病变内部出现分层。不同矿物质含量的层被认为反映了氟化物施用的历史。使用大块标本研究此类病变在不同深度的溶解特性,可能会受到酸通过病变孔隙扩散受限的阻碍。因此,在本研究中,通过将切片从切割面而非外表面暴露于酸性缓冲液中,研究了牙釉质和牙本质病变以及下方健康组织的酸敏感性。标本取自先前一项关于高氟(0、1000、2000、3000/5000 ppm F)牙膏对牙釉质和牙本质脱矿/再矿化影响的研究。将切片置于酸性缓冲液中 3 天和 7 天,并通过接触式显微放射照相术监测矿物质含量的变化。对于牙釉质病变,在接受不同氟化物方案的组之间,观察到溶解随深度存在显著差异。在 7 天时,发现不同氟化物组与病变参数之间存在剂量反应。在无氟组中,原始病变和健康组织中的溶解情况相似。所有用氟化物处理过的牙本质病变都表现出溶解受到抑制,但抑制作用并未随着氟化物浓度的升高而增强。在牙本质组织更深层有一定的保护作用,但无统计学意义。我们得出结论,氟化物通过病变孔隙的渗透决定了病变在不同深度的溶解模式。

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