Vogel G L, Zhang Z, Chow L C, Schumacher G E
American Dental Association Health Foundation, Paffenbarger Research Center, National Institute of Standards and Technology, Gaithersburg, MD 20899, USA.
Caries Res. 2001 Mar-Apr;35(2):116-24. doi: 10.1159/000047442.
Labile reservoirs are important in maintaining ion concentrations in oral fluids, especially after a fluoride dentifrice application, where a persistent increase in fluid fluoride can mitigate or reverse caries progression. In this study, the effect of experimental and conventional fluoride rinses on the in vitro and in vivo water-induced release of fluoride, calcium, phosphate, acetate and hydrogen ions from oral reservoirs was examined. At the start of each experiment, 13 subjects rinsed either with a conventional 228-ppm fluoride NaF rinse, a 228-ppm fluoride controlled-release rinse (CR rinse) or received no rinse. Sixty minutes later upper and lower molar plaque samples and 1-min saliva samples were collected. The subjects then rinsed with deionized water for 1 min, and 7 min later, a second set of samples was collected (in vivo study). Plaque fluid and clarified saliva were then recovered from samples by centrifugation, and the remaining plaque mass was sequentially extracted with water and acid to measure the water-extracted and total whole-plaque fluoride (in vitro study). All the samples were analyzed using microtechniques for pH, free calcium, phosphate, organic acids (plaque fluid) and fluoride (plaque fluid, centrifuged saliva and plaque extracts). Results showed that in vivo water rinsing decreased acetate and phosphate in plaque fluid, and fluoride in plaque fluid and saliva, but had no effect on plaque fluid pH. In vivo water rinsing, however, increased plaque fluid free calcium, apparently due to water-induced loss of calcium-binding ions. Water- or fluoride-rinse-induced changes in plaque fluid concentration were greater at the lower molar site, suggesting that rinse pooling may influence ion distribution. Before the water rinse, plaque fluid, saliva and whole-plaque total fluoride values were 1.7, 2 and 4 times higher after the CR rinse compared to the NaF rinse. Furthermore, the CR rinse deposited approximately 11 times more water-extracted fluoride compared to the NaF rinse, suggesting a 'more efficient' precipitation of 'labile' or 'loosely bound fluoride'. The results presented here, and in previous studies, suggest the possibility of formulating effective fluoride dentifrices with a lower fluoride content than is currently in use.
不稳定储存库对于维持口腔液体中的离子浓度很重要,尤其是在使用含氟牙膏后,此时口腔液体中氟含量的持续增加可以减轻或逆转龋齿的进展。在本研究中,检测了实验性和传统含氟漱口水对体外和体内口腔储存库中氟、钙、磷酸盐、乙酸盐和氢离子的水诱导释放的影响。在每个实验开始时,13名受试者分别用传统的228 ppm氟化钠漱口水、228 ppm控释含氟漱口水(控释漱口水)漱口,或不进行漱口。60分钟后,收集上下磨牙的牙菌斑样本和1分钟的唾液样本。然后受试者用去离子水漱口1分钟,7分钟后,收集第二组样本(体内研究)。然后通过离心从样本中回收牙菌斑液和澄清唾液,并用去离子水和酸依次提取剩余的牙菌斑块,以测量水提取的和全牙菌斑中的总氟含量(体外研究)。使用微量技术对所有样本进行pH值、游离钙、磷酸盐、有机酸(牙菌斑液)和氟(牙菌斑液、离心唾液和牙菌斑提取物)分析。结果表明,体内用水漱口可降低牙菌斑液中的乙酸盐和磷酸盐含量,以及牙菌斑液和唾液中的氟含量,但对牙菌斑液的pH值没有影响。然而,体内用水漱口会增加牙菌斑液中的游离钙,这显然是由于水导致钙结合离子流失所致。在较低磨牙部位,水或含氟漱口水引起的牙菌斑液浓度变化更大,这表明漱口水积聚可能会影响离子分布。在用水漱口前,与氟化钠漱口水相比,控释漱口水后的牙菌斑液、唾液和全牙菌斑总氟含量分别高出1.7、2和4倍。此外,与氟化钠漱口水相比,控释漱口水沉积的水提取氟约多11倍,这表明“不稳定”或“松散结合氟”的“沉淀效率更高”。此处呈现的结果以及先前研究的结果表明,有可能配制出氟含量低于目前使用水平的有效含氟牙膏。