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利用扫频光学相干断层扫描技术评估变形链球菌诱导的颈椎脱矿作用。

Assessment of cervical demineralization induced by Streptococcus mutans using swept-source optical coherence tomography.

作者信息

Tezuka Hiroki, Shimada Yasushi, Matin Khairul, Ikeda Masaomi, Sadr Alireza, Sumi Yasunori, Tagami Junji

机构信息

Graduate School of Tokyo Medical and Dental University , Department of Cariology and Operative Dentistry, Tokyo, Japan.

Graduate School of Tokyo Medical and Dental University, Department of Cariology and Operative Dentistry, Tokyo, Japan; Tsurumi University, School of Dental Medicine, Endowed Department of International Oral Health Science, 2-1-3 Tsurumi, Tsurumi-ku, Yokohama-shi 230-8501, Japan.

出版信息

J Med Imaging (Bellingham). 2016 Jan;3(1):014504. doi: 10.1117/1.JMI.3.1.014504. Epub 2016 Mar 8.

Abstract

Exposed root surfaces due to gingival recession are subject to biofilm stagnation that can result in caries formation. Cervical enamel and dentin demineralization induced by a cariogenic biofilm was evaluated using swept-source optical coherence tomography (SS-OCT). The cementoenamel junction (CEJ) sections of extracted human teeth were subjected to demineralization for 1, 2, or 3 weeks. A suspension of Streptococcus mutans was applied to form a cariogenic biofilm using an oral biofilm reactor. After incubation, demineralization was observed by SS-OCT. For the analysis of SS-OCT signal, the value of the area under the curve (AUC) of the signal profile was measured. Statistical analyses were performed with 95% level of confidence. Cervical demineralization was displayed as a bright zone in SS-OCT. The demineralization depth of dentin was significantly deeper than that of enamel ([Formula: see text]). Enamel near the CEJ demonstrated a significant increase of AUC over the other enamel region after the demineralization. The gaps along the dentinoenamel junction were additionally observed in SS-OCT. SS-OCT was capable of monitoring the cervical demineralization induced by a cariogenic biofilm and is considered to be a promising modality for the diagnosis of cervical demineralization.

摘要

牙龈退缩导致的牙根暴露表面易出现生物膜停滞,进而可能导致龋齿形成。使用扫频光学相干断层扫描(SS-OCT)评估致龋生物膜诱导的颈部釉质和牙本质脱矿情况。将拔除的人牙的牙骨质釉质界(CEJ)切片进行1、2或3周的脱矿处理。使用口腔生物膜反应器应用变形链球菌悬液以形成致龋生物膜。孵育后,通过SS-OCT观察脱矿情况。为了分析SS-OCT信号,测量信号轮廓的曲线下面积(AUC)值。进行置信水平为95%的统计分析。颈部脱矿在SS-OCT中显示为明亮区域。牙本质的脱矿深度明显深于釉质([公式:见原文])。脱矿后,CEJ附近的釉质与其他釉质区域相比,AUC显著增加。在SS-OCT中还额外观察到沿牙釉质界的间隙。SS-OCT能够监测致龋生物膜诱导的颈部脱矿,被认为是诊断颈部脱矿的一种有前景的方式。

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