埋伏牙颊根管解剖特征的CBCT评价。

Mahdiye Rayisi, Kianoosh Malekzadeh, Masoomeh Afsa
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引用次数: 1

摘要

问题说明:上牙带管(GC)是一种从未出牙的毛囊延伸到充满牙板残余的牙槽骨嵴的管。这条管被认为是引导牙齿萌出并与一些病理状况有关。目的:本研究旨在确定在锥形束计算机断层扫描(CBCT)图像上不能正常出牙的牙齿中是否存在GC及其解剖学特征。材料和方法:本横断面研究评估了来自29名女性和21名男性的77颗埋伏恒牙和多生牙的CBCT图像。研究了GC的检测频率、其相对于冠和根的位置、根管起源的牙齿解剖表面、根管开放的邻近皮质表以及根管的长度。结果:53.2%的牙有GC。41.5%的牙齿解剖角度为咬合/切牙,82.9%的牙齿为冠。51.2%的GCs在腭/舌皮层打开,63.4%的GCs不在牙长轴上。85.7%的牙在冠形成阶段检出GC。结论:虽然GC作为一种出牙通道被引入,但该通道在阻生牙中也存在。这意味着该根管的存在并不能保证牙齿的正常萌出,而且GC的解剖特征可能会影响萌出过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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CBCT Assessment of the Anatomical Characteristics of Gubernacular Canal in Impacted Teeth.

Statement of the problem: Gubernacular canal (GC) is a canal that extends from the follicle of unerupted permanent teeth to the alveolar bone crest filled with remnants of the dental lamina. This canal is thought to guide tooth eruption and be related to some pathologic conditions.

Purposes: This study aimed to determine the presence of GC and its anatomical characteristics in teeth, which failed to erupt normally on cone beam computed tomography (CBCT) images.

Materials and method: This cross-sectional study evaluated CBCT images of 77 impacted permanent and supernumerary teeth obtained from 29 females and 21 males. The frequency of GC detection, its location in relation to the crown and root, the anatomical surface of the tooth from which the canal has originated, and the adjacent cortical table to which the canal opens, along with the length of the GC were studied.

Results: GC was observed in 53.2% of teeth. The anatomical tooth aspect of origin was occlusal/ incisal in 41.5% and crown in 82.9% of teeth. Moreover, 51.2% of GCs opened in palatal/lingual cortex and 63.4% of canals were not located along the tooth long axis. Finally, GC was detected in 85.7% of teeth undergoing the crown formation stage.

Conclusion: Although GC was introduced as an eruption pathway, this canal is also present in impacted teeth. This means that presence of this canal does not promise the normal eruption of tooth and the anatomical characteristics of GC may influence the eruption process.

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