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通过氟磷灰石核磁共振分析氟对羟基磷灰石脱矿质作用的影响。

Effects of fluoride on hydroxyapatite demineralisation analysed by F MAS-NMR.

作者信息

Ferizoli Bajram, Cresswell-Boyes Alexander J, Anderson Paul, Lynch Richard J M, Hill Robert G

机构信息

Dental Physical Sciences Unit, Centre for Oral Bioengineering, Institute of Dentistry, Barts and the London School of Medicine and Dentistry, Queen Mary University of London, London, United Kingdom.

出版信息

Front Dent Med. 2023 May 24;4:1171827. doi: 10.3389/fdmed.2023.1171827. eCollection 2023.

Abstract

INTRODUCTION

Fluoride plays a major role in inhibiting enamel dissolution and promoting fluorapatite formation. Porous hydroxyapatite (HAP) discs can be used as an enamel analogue in artificial demineralisation/remineralisation studies.

METHOD

The aim of the study was to monitor the fluoride-mineral phases formed on HAP surfaces as a function of fluoride concentration ([F]) under demineralising conditions, using F magic angle spinning nuclear magnetic resonance (MAS-NMR) spectroscopy, and compare the results with a previous study using an enamel substrate. Porous HAP blocks were immersed in demineralisation solutions (0.1 M acetic acid, pH 4.0) with increasing [F] (0-1450 ppm).

RESULTS

At below 50 ppm [F], F MAS-NMR showed fluoride-substituted apatite formation; above 50 ppm [F], calcium fluoride (CaF) was formed in increasing proportions. These results mirrored those of previous similar studies with an enamel substrate. Further increases in fluoride caused no further measurable reduction in demineralisation but increased the proportion of CaF formed. The total calcium concentration [Ca] and total phosphorus [P] concentrations in the solution were measured by inductively coupled plasma atomic emission spectroscopy. At high fluoride concentrations, the solution total [P] increased, and the molar Ca:P ratios decreased to values consistent with the formation of CaF. However, Ca:P ratios found at low [F] were higher than those in the previous enamel study and consistent with the formation of a partially fluoridated apatite.

CONCLUSIONS

Under demineralising conditions, CaF formed on HAP at an [F] of 50 ppm and above, whereas fluoridated apatite formed at an [F] below 50 ppm. The results were consistent with those obtained when an enamel substrate was used.

摘要

引言

氟化物在抑制牙釉质溶解和促进氟磷灰石形成方面发挥着重要作用。多孔羟基磷灰石(HAP)盘可作为人工脱矿/再矿化研究中的牙釉质类似物。

方法

本研究的目的是在脱矿条件下,使用氟魔角旋转核磁共振(MAS-NMR)光谱监测在HAP表面形成的氟化物矿物相随氟化物浓度([F])的变化,并将结果与先前使用牙釉质基质的研究进行比较。将多孔HAP块浸入氟化物浓度([F])不断增加(0-1450 ppm)的脱矿溶液(0.1 M乙酸,pH 4.0)中。

结果

当[F]低于50 ppm时,氟MAS-NMR显示形成了氟取代的磷灰石;当[F]高于50 ppm时,氟化钙(CaF)的形成比例不断增加。这些结果与先前使用牙釉质基质的类似研究结果一致。氟化物的进一步增加并未导致脱矿有进一步可测量的减少,但增加了CaF的形成比例。通过电感耦合等离子体原子发射光谱法测量溶液中的总钙浓度[Ca]和总磷[P]浓度。在高氟浓度下,溶液中的总[P]增加,钙磷摩尔比降低至与CaF形成一致的值。然而,在低[F]时发现的钙磷比高于先前牙釉质研究中的值,并且与部分氟化磷灰石的形成一致。

结论

在脱矿条件下,当[F]为50 ppm及以上时,HAP上形成CaF,而当[F]低于50 ppm时形成氟化磷灰石。结果与使用牙釉质基质时获得的结果一致。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/963e/11797780/282ed72e8a58/fdmed-04-1171827-g001.jpg

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