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使用电子探针微分析技术研究再矿化/脱矿循环对体外富士IX Fast矿物分布的影响。

Effect of remineralization/demineralization cycles on mineral profiles of Fuji IX Fast in vitro using electron probe microanalysis.

作者信息

Ab-Ghani Z, Ngo H, McIntyre J

机构信息

Universiti Sains Malaysia, Malaysia.

出版信息

Aust Dent J. 2007 Dec;52(4):276-81. doi: 10.1111/j.1834-7819.2007.tb00502.x.

Abstract

BACKGROUND

There have been cononcerns about the dissolution of conventional glass ionomer cement (GIC) and its possible degradation when exposed to an acidic environment over time. The objective of this study was to investigate the effects of exposure of Fuji IX Fast to the simulated acidic aspects of the oral environment in terms of any change in the elemental composition of strontium (Sr), phosphorus (P), calcium (Ca) and fluorine (F) which resulted at the surface of this material.

METHODS

Sixty-five cylindrical block of Fuji IX Fast were prepared using split moulds. The demineralizing solution was an acetate buffered demineralizing solution at pH 403. The remineralizing solution was a buffered solution containing 1.5 mM Ca, 0.9 mM P and 10 ppm F at pH 7. The blocks of Fuji IX Fast were subjected either to two-day alternating cycles of remineralization and demineralization for up to 24 days (test); 6 two-day cycles of demineralizing or remineralizing solution separately, or deionized distilled water alone (controls) or were left untreated (base line control). Mineral profiles of Ca, P, Sr and F within 100 microm of the material surface were assessed following 8, 16 and 24 days of treatment (test); 4, 8 or 12 days (controls) or for baseline control samples, using electron probe microanalysis (EPMA).

RESULTS

There were significant changes in mineral profile in the test specimens in terms of Sr and Ca concentrations. A molecule for molecule exchange of these elements resulted between GIC and eluant solutions. Fluoride loss from the GIC occurredto the level comparable with uptake levels recorded in eluant solutions from previous studies. The ionic exchanges appeared to be the result of dissolution followed by an equilibrium-driven diffusion. These exchanges were superficial though substantial.

CONCLUSIONS

Simulated exposure of Fuji IX to the oral environment resulted in an exchange of Ca from the bathing solutions into Fuji IX to replace any Sr which was lost to the GIC. Fluorine loss from the GIC followed previously described patterns. The possible clinical significance of this exchange was discussed.

摘要

背景

人们一直担心传统玻璃离子水门汀(GIC)在长期暴露于酸性环境时的溶解情况及其可能的降解。本研究的目的是就富士IX快速型材料表面锶(Sr)、磷(P)、钙(Ca)和氟(F)的元素组成变化,研究其暴露于口腔环境模拟酸性条件下的影响。

方法

使用分体模具制备65个富士IX快速型圆柱形块体。脱矿溶液是pH值为4.03的醋酸盐缓冲脱矿溶液。再矿化溶液是pH值为7的含有1.5 mM钙、0.9 mM磷和10 ppm氟的缓冲溶液。富士IX快速型块体分别进行为期两天的再矿化和脱矿交替循环,长达24天(测试);分别进行6个为期两天的脱矿或再矿化溶液循环,或仅用去离子蒸馏水(对照),或不进行处理(基线对照)。在处理8、16和24天(测试)后;4、8或12天(对照)或基线对照样品后,使用电子探针微分析(EPMA)评估材料表面100微米内的钙、磷、锶和氟的矿物质分布。

结果

测试样品中矿物质分布在锶和钙浓度方面有显著变化。这些元素在GIC和洗脱液之间发生了分子对分子的交换。GIC中的氟损失到了与先前研究中洗脱液记录的吸收水平相当的程度。离子交换似乎是溶解后由平衡驱动的扩散的结果。这些交换虽然很明显,但只是表面的。

结论

富士IX模拟暴露于口腔环境导致浴液中的钙与富士IX发生交换,以取代GIC中损失的任何锶。GIC中的氟损失遵循先前描述的模式。讨论了这种交换可能的临床意义。

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