Formation of Caries-Like Lesions in vitro on the Root Surfaces of Human Teeth in Solutions Simulating Plaque Fluid

被引:13
作者
Shellis, R. P. [1 ,2 ]
机构
[1] Univ Bristol, Sch Dent, Dept Oral & Dent Sci, Bristol BS1 2LY, Avon, England
[2] Univ Bern, Dept Prevent Restorat & Pediat Dent, Bern, Switzerland
关键词
Caries; Dentine; In vitro; Solubility; AMINO-ACID PROFILES; HUMAN DENTAL PLAQUE; HUMAN TOOTH ENAMEL; DISSOLUTION KINETICS; POSITIVE INDIVIDUALS; CONSTANT COMPOSITION; MOLECULAR-WEIGHT; ORGANIC-ACIDS; ACETIC-ACID; DEMINERALIZATION;
D O I
10.1159/000318224
中图分类号
R78 [口腔科学];
学科分类号
1003 ;
摘要
Lesion formation on root surfaces of human posterior teeth was studied in acetate/lactate buffers with a background electrolyte composition based on plaque fluid analyses. Lesion depth after 28 days at 37 degrees C was measured in relation to: the presence or absence of cementum; the concentration of undissociated buffer; the presence or absence of magnesium ions at plaque fluid concentration. Each factor was evaluated at several values of -log(ion activity product for hydroxyapatite): pI(HA). Solutions were formulated to minimize variation in pH, which varied by <= 0.03 for a given comparison (individual pI(HA)) and by 0.42-0.82 over the range of pI(HA) within experiments. Lesions on surfaces from which cementum had been ground were significantly deeper than on intact surfaces, but this is considered to be due to subsurface mechanical damage and not to a solubility difference. Neither the concentration of undissociated buffer nor the presence of magnesium ions significantly affected lesion depth. Lesion depth was strongly influenced by the correlated variations in pI(HA) and pH. At pI(HA) 54 and 55, only extremely shallow lesions formed. From pI(HA) 56, lesion depth increased with increasing pI(HA). The results confirm that the solubility of the mineral of root tissues is higher than that of hydroxyapatite, but indicate that it is probably lower than suggested by Hoppenbrouwers et al. [Arch Oral Biol 1987; 32: 319-322]. For calcium concentrations of 3-12 m M, the critical pH for root tissue mineral was calculated as 5.22-5.66 assuming solubility equivalent to pI(HA) 54 and 5.08-5.51 assuming pI(HA) 55. Copyright (C) 2010 S. Karger AG, Basel
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页码:380 / 389
页数:10
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