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光学相干断层扫描对釉质脱矿的早期检测。

Early detection of enamel demineralization by optical coherence tomography.

机构信息

Department of Electrical Engineering, Chang Gung University, Taoyuan, 33302, Taiwan.

Department of Neurosurgery, Chang Gung Memorial Hospital, Linkou, 33305, Taiwan.

出版信息

Sci Rep. 2019 Nov 20;9(1):17154. doi: 10.1038/s41598-019-53567-7.

Abstract

Enamel is the outermost layer of the tooth that protects it from invasion. In general, an acidic environment accelerates tooth demineralization, leading to the formation of cavities. Scanning electron microscopy (SEM) is conventionally used as an in vitro tool for the observation of tooth morphology changes with acid attacks. Yet, SEM has intrinsic limitations for the potential application of in vivo detection in the early demineralization process. In this study, a high-resolution optical coherence tomography (OCT) system with the axial and transverse resolutions of 2.0 and 2.7 μm in teeth has been utilized for characterizing the effect of the acidic environment (simulated by phosphoric acid) on the enamel topology. The scattering coefficient and the surface roughness of enamel can be directly derived from the OCT results, enabling a quantitative evaluation of the topology changes with demineralization. The dynamic process induced by the acid application is also recorded and analyzed with OCT, depicting the evolution of the demineralization process on enamel. Notably, the estimated enamel scattering coefficient and surface roughness significantly increase with the application time of acid and the results illustrate that the values of both parameters after demineralization are significantly larger than those obtained before the demineralization, illustrating both parameters could be effective to differentiate the healthy and demineralized teeth and determine the severity. The obtained results unambiguously illustrate that demineralization of the tooth surface can be successfully detected by OCT and further used as an indicator of early-stage cavity formation.

摘要

牙釉质是牙齿的最外层,可保护牙齿免受侵害。一般来说,酸性环境会加速牙齿脱矿,导致龋齿的形成。扫描电子显微镜(SEM)通常被用作体外工具,用于观察牙齿在酸蚀作用下形态的变化。然而,SEM 在用于体内早期脱矿过程的潜在检测方面存在固有局限性。在这项研究中,利用轴向和横向分辨率分别为 2.0 和 2.7μm 的高分辨率光学相干断层扫描(OCT)系统来研究酸性环境(用磷酸模拟)对牙釉质拓扑结构的影响。牙釉质的散射系数和表面粗糙度可以直接从 OCT 结果中得出,从而可以定量评估脱矿过程中拓扑结构的变化。利用 OCT 还可以记录和分析酸应用引起的动态过程,描绘脱矿过程在牙釉质上的演变。值得注意的是,酸应用引起的散射系数和表面粗糙度随着酸的应用时间而显著增加,结果表明,脱矿后这两个参数的值明显大于脱矿前的值,这表明这两个参数可以有效地区分健康和脱矿的牙齿,并确定其严重程度。研究结果明确表明,OCT 可以成功检测牙齿表面的脱矿情况,并进一步作为早期龋齿形成的指标。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa97/6868170/ffdf45eb5256/41598_2019_53567_Fig1_HTML.jpg

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