Featherstone J D B
Department of Preventive and Restorative Dental Sciences, University of California, San Francisco, USA.
Aust Dent J. 2008 Sep;53(3):286-91. doi: 10.1111/j.1834-7819.2008.00064.x.
Abstract Dental caries is a transmissible bacterial disease process caused by acids from bacterial metabolism diffusing into enamel and dentine and dissolving the mineral. The bacteria responsible produce organic acids as a by-product of their metabolism of fermentable carbohydrates. The caries process is a continuum resulting from many cycles of demineralization and remineralization. Demineralization begins at the atomic level at the crystal surface inside the enamel or dentine and can continue unless halted with the end-point being cavitation. There are many possibilities to intervene in this continuing process to arrest or reverse the progress of the lesion. Remineralization is the natural repair process for non-cavitated lesions, and relies on calcium and phosphate ions assisted by fluoride to rebuild a new surface on existing crystal remnants in subsurface lesions remaining after demineralization. These remineralized crystals are acid resistant, being much less soluble than the original mineral.
摘要 龋齿是一种可传播的细菌性疾病过程,由细菌代谢产生的酸扩散到牙釉质和牙本质中并溶解矿物质所致。致病细菌在代谢可发酵碳水化合物时会产生有机酸作为副产物。龋病过程是由许多脱矿和再矿化循环导致的连续过程。脱矿始于牙釉质或牙本质内部晶体表面的原子水平,若不停止,可继续发展,最终导致龋洞形成。在这个持续过程中有多种干预可能性,以阻止或逆转病变进展。再矿化是非龋洞性病变的自然修复过程,依赖于钙和磷酸根离子在氟的辅助下,在脱矿后残留的表层下病变中现有晶体残余物上重建新的表面。这些再矿化晶体具有抗酸性,其溶解度远低于原始矿物质。