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高、低氟地区正畸诱导牙根吸收陷窝与牙根牙骨质表面粗糙度的比较:三维共聚焦显微镜研究。

Comparison of surface roughness of root cementum and orthodontically induced root resorption craters from high- and low-fluoridation areas: a 3D confocal microscopy study.

机构信息

Department of Orthodontics and Paediatric Dentistry, Faculty of Medicine and Health, University of Sydney, Sydney Dental Hospital SLHD, Level 2, 2 Chalmers Street, Surry Hills, Sydney, NSW, 2010, Australia.

Adelaide Dental School, University of Adelaide, Adelaide, Australia.

出版信息

Prog Orthod. 2022 Jun 27;23(1):20. doi: 10.1186/s40510-022-00415-6.

Abstract

BACKGROUND

Fluoride has a major role in strengthening the structure of enamel against acids. Despite differences between caries and root resorption processes, both events inherently involve acidic dissolution of dental tissues. The aim of the present study was to investigate the effects of water fluoridation levels on the surface roughness of root cementum and resorption craters. The findings provided more insight into the influence of fluoride on the surfaces of intact cementum surface and resorption craters.

METHODS

Twenty-eight orthodontic patients were recruited from two cities in Turkey, with high (≥ 2 ppm) and low (≤ 0.05 ppm) water fluoridation. These patients needed bilateral maxillary first premolar extraction as part of their orthodontic treatment and were allocated into two study groups (n = 14 in each group) based on water fluoridation exposure level: the high-fluoride group (HF) and low-fluoride group (LF). 150 g of buccal tipping forces was applied to all maxillary first premolar teeth for 12 weeks with a beta-titanium spring which was reactivated every 4 weeks. All maxillary premolars were removed at the end of the experiment for surface roughness assessment using three-dimensional confocal microscopy and the associated software. The buccal root surface and the largest buccal resorption crater were investigated.

RESULTS

Resorption craters were significantly rougher in LF group compared to HF group (p = 0.002). Craters were rougher than the intact root surfaces (p = 0.000). Cervical and apical regions were significantly rougher than the middle region (p = 0.000 and p = 0.024, respectively).

CONCLUSIONS

Higher water fluoridation level of ≥ 2 ppm resulted in significantly smoother root resorption craters than low water fluoridation level of ≤ 0.05 ppm when the teeth were subjected to 150 g of buccal tipping force. Fluoride seems to have a protective role at the interface of root resorption, and further mineral or histological studies may shed light on the exact protective process against root resorption.

摘要

背景

氟化物在增强牙釉质对抗酸的结构方面起着重要作用。尽管龋齿和根吸收过程存在差异,但这两个事件都涉及到牙本质的酸性溶解。本研究旨在探讨水氟化物水平对根牙骨质表面粗糙度和吸收陷窝的影响。研究结果为氟化物对完整牙骨质表面和吸收陷窝表面的影响提供了更深入的了解。

方法

从土耳其的两个城市招募了 28 名正畸患者,这些城市的水氟化物含量较高(≥2ppm)和较低(≤0.05ppm)。这些患者需要双侧上颌第一前磨牙拔牙作为正畸治疗的一部分,并根据水氟化物暴露水平分为两组(每组 14 名):高氟化物组(HF)和低氟化物组(LF)。用β钛合金弹簧向所有上颌第一前磨牙施加 150g 的颊向倾斜力,每 4 周重新激活一次。实验结束时,所有上颌前磨牙均被取出,使用三维共聚焦显微镜及其相关软件评估表面粗糙度。研究了颊侧根表面和最大颊侧吸收陷窝。

结果

LF 组的吸收陷窝明显比 HF 组粗糙(p=0.002)。陷窝比完整的牙根表面粗糙(p=0.000)。颈区和根尖区明显比中区粗糙(p=0.000 和 p=0.024)。

结论

当牙齿受到 150g 的颊向倾斜力时,水氟化物水平较高(≥2ppm)导致根吸收陷窝明显比水氟化物水平较低(≤0.05ppm)更光滑。氟化物在根吸收界面似乎具有保护作用,进一步的矿物质或组织学研究可能揭示根吸收的具体保护过程。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3494/9234018/d9edfb1b1ba1/40510_2022_415_Fig1_HTML.jpg

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