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横向显微放射照相术在酸蚀致矿物质流失测量中的应用。

Application of transverse microradiography for measurement of mineral loss by acid erosion.

作者信息

Hall A F, Sadler J P, Strang R, de Josselin de Jong E, Foye R H, Creanor S L

机构信息

Glasgow Dental Hospital and School, Scotland, UK.

出版信息

Adv Dent Res. 1997 Nov;11(4):420-5. doi: 10.1177/08959374970110040701.

Abstract

This paper describes a novel application of transverse microradiography for the detection and quantification of mineral loss due to acid erosion in thin tooth sections. Sixty-four specimens were randomly divided into eight equal-sized groups and exposed to an orthophosphoric-acid-based erosive fluid (pH = 3) for 0, 0.25, 0.5, 1, 2, 5, 12, or 24 hrs. We made microdensitometric scans separately across both enamel and dentin to derive data for the total mineral loss and the minimum mineral content within the eroded area. We then analyzed specimens using a profilometer to determine (1) the area above a plot of penetration depth against distance and (2) the maximum depth of penetration. Correlation coefficients for comparisons between microradiographic and profilometric data for both enamel and dentin specimens varied between 0.87 and 0.96. Two-sample t tests demonstrated that the microradiographic technique could detect early erosion, i.e., discriminate between erosion times of less than 1 hr. It was concluded that this application of transverse microradiography was a useful and acceptable method for the measurement of early mineral loss in vitro, occurring as a result of acid erosion.

摘要

本文描述了横向显微放射成像技术在检测和量化薄牙切片中酸蚀导致的矿物质流失方面的一种新应用。64个标本被随机分成8个大小相等的组,并暴露于基于正磷酸的侵蚀性液体(pH = 3)中0、0.25、0.5、1、2、5、12或24小时。我们分别对牙釉质和牙本质进行了显微密度扫描,以获取侵蚀区域内总矿物质流失和最低矿物质含量的数据。然后,我们使用轮廓仪分析标本,以确定(1)穿透深度与距离关系图上方的面积,以及(2)最大穿透深度。牙釉质和牙本质标本的显微放射成像数据与轮廓仪数据之间比较的相关系数在0.87至0.96之间。双样本t检验表明,显微放射成像技术可以检测早期侵蚀,即区分侵蚀时间小于1小时的情况。得出的结论是,横向显微放射成像技术的这种应用是一种用于体外测量酸蚀导致的早期矿物质流失的有用且可接受的方法。

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