University of Missouri-Kansas City School of Dentistry, United States.
Dent Mater. 2010 May;26(5):433-42. doi: 10.1016/j.dental.2010.01.002. Epub 2010 Feb 6.
Measuring the structure, composition or suitability for bonding of the acid-etched dentin substrate, especially in its hydrated state, has been a formidable problem. The purpose of this study was to determine the morphological and structural profiles of the dentin demineralized layer measured in its natural wet state using environmental scanning electron microscopy (ESEM) and micro-Raman imaging.
The occlusal 1/3 of the crown was removed from nine extracted, unerupted human third molars. Dentin surfaces were abraded with 600-grit SiC sandpaper under water to create smear layers. The prepared dentin surfaces were randomly selected for treatment with the self-etching agent (Adper Prompt L-Pop) or the total-etching agent 35% H(3)PO(4) gel (with/without agitation). Micro-Raman spectra and imaging were acquired at 1-1.5microm spatial resolution at positions perpendicular to the treated surfaces; since this technique is non-destructive, the same specimens were also imaged with ESEM. Specimens were kept wet throughout spectral acquisition and ESEM observations.
ESEM could be used to reveal demineralized layers in acid-etched dentin, but the resolution was low and no collagen fibrils were disclosed. The detailed chemical maps/profiles of demineralized dentin layers under wet conditions could be obtained using Raman imaging. It was shown that the mineral existed in the superficial layer of all etched dentin covered with smear layers. The mineral was much easier to be removed underneath the superficial layer. The depth, degree, and profile of dentin demineralization were dependent on the types of acids (self-etching vs. total etching) and application procedures (with vs. without agitation).
Most current adhesives are applied using wet bonding techniques in which the dentin is kept fully hydrated throughout the bonding. Our ability to fully characterize the hydrated, etched dentin substrates is very important for understanding bonding under in vivo conditions.
测量酸蚀牙本质基质的结构、组成或适合键合的特性,尤其是在其水合状态下,这一直是一个艰巨的问题。本研究的目的是使用环境扫描电子显微镜(ESEM)和微拉曼成像来确定在自然湿状态下测量的牙本质脱矿层的形态和结构特征。
从九颗未萌出的第三磨牙的冠部 1/3 处去除牙釉质。在水下用 600 目 SiC 砂纸打磨牙本质表面以形成玷污层。随机选择制备的牙本质表面用自酸蚀剂(Adper Prompt L-Pop)或 35% H(3)PO(4)凝胶全酸蚀剂(有/无搅拌)处理。以垂直于处理表面的位置,以 1-1.5μm 的空间分辨率采集微拉曼光谱和成像;由于该技术是非破坏性的,因此相同的标本也可以用 ESEM 成像。在光谱采集和 ESEM 观察过程中,标本始终保持湿润。
ESEM 可用于显示酸蚀牙本质中的脱矿层,但分辨率较低,且未显示胶原纤维。使用拉曼成象可以获得湿条件下脱矿牙本质层的详细化学图谱/轮廓。结果表明,在所有覆盖有玷污层的酸蚀牙本质的表面层中都存在矿物质。在表面层下,矿物质更容易被去除。牙本质脱矿的深度、程度和轮廓取决于酸的类型(自酸蚀与全酸蚀)和应用程序(有搅拌与无搅拌)。
目前大多数胶粘剂都是在湿粘结技术中使用的,在这种技术中,粘结过程中牙本质始终保持完全水合。我们全面描述水合、酸蚀牙本质基质的能力对于理解体内粘结条件下的粘结非常重要。