Interaction between Saliva, Pellicle, and Dental Erosion.

Monographs in oral science Pub Date : 2025-01-01 Epub Date: 2025-05-28 DOI:10.1159/000543558
Christian Hannig, Matthias Hannig
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Abstract

The dynamic interplay of the oral fluids with the tooth surface is of essential relevance for the modulation of the de- and remineralization of tooth hard substances. It is generally accepted textbook knowledge that the buffering and clearance properties of the saliva are key factors in the prevention of erosive mineral loss. This becomes especially evident when the patients suffer from xerostomia. Furthermore, biomolecules in the oral fluids ensure the formation of the pellicle layer on all solid surfaces. While the enamel pellicle has been shown to diminish erosive attacks to a certain extent, it is unclear if the dentinal pellicle yields the same efficiency. In this context, two aspects seem to be marginalized in research: the dentine surface and the impact of protein adsorption and infiltration in demineralized tooth structures, despite the fact that both are essential for the understanding and modulation of erosive processes. Successful and sustainable prevention strategies are only possible if we understand these dynamic interactions. Therefore, future research should focus on the interaction of proteins with dentine and enamel during repeated de- and remineralization processes.

唾液、牙膜与牙蚀的相互作用。
口腔液体与牙齿表面的动态相互作用对于调节牙齿硬物质的脱矿和再矿化至关重要。人们普遍接受的教科书知识是,唾液的缓冲和清除特性是防止侵蚀性矿物质流失的关键因素。当患者患有口干症时,这一点尤为明显。此外,口服液中的生物分子确保在所有固体表面形成膜层。虽然牙釉质膜已被证明在一定程度上减少侵蚀,但尚不清楚牙本质膜是否能产生同样的效果。在这种背景下,两个方面的研究似乎被边缘化:牙本质表面和蛋白质在脱矿牙齿结构中的吸附和浸润的影响,尽管这两个方面对于理解和调节侵蚀过程至关重要。只有当我们了解这些动态的相互作用时,才有可能制定成功和可持续的预防战略。因此,未来的研究重点应放在反复脱矿和再矿化过程中蛋白质与牙本质和牙釉质的相互作用上。
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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