Solubility of human enamel mineral.

Journal de biologie buccale Pub Date : 1990-09-01
E C Moreno, T Aoba
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Abstract

The solubility of human enamel was investigated in dilute phosphoric acid solutions (0.07 mMols/L to 1.54 mMols/L) under controlled partial pressures of CO2 (0.005% to 3.33% in mixtures with N2) at 25 degrees C. The enamel mineral was considered as carbonatoapatite containing acid phosphate having the stoichiometry [Ca]5-x-y[HPO4]v[PO4]3-x[CO3]w[OH]l-x-y. During equilibration, a second apatitic phase precipitated, as observed under the electronmicroscope. Solubility models are advanced consistent with the adapted stoichiometry and the precipitation of the second phase. The latter appears to have a carbonate content similar to that of the enamel mineral even when precipitated under the lowest partial pressure of CO2, suggesting that a molar content of about 0.3 of carbonate stabilizes the apatitic lattice. Based on the adopted stoichiometry of enamel mineral, Ca4.34 (HPO4).08 (CO3).29 (PO4)2.63 (OH).05, its solubility product constant was calculated as Ksp = 1.74 (+/- 0.081)x10(-6), expressed as the mean activity product.

人牙釉质矿物的溶解度。
研究了人牙釉质在25℃的稀磷酸溶液(0.07 mMols/L ~ 1.54 mMols/L)中,在控制CO2分压(与N2混合时为0.005% ~ 3.33%)下的溶解度。牙釉质矿物被认为是含有酸性磷酸盐的碳酸磷灰石,其化学计量量为[Ca]5-x-y[HPO4]v[PO4]3-x[CO3]w[OH] L -x-y。在电子显微镜下观察到,在平衡过程中,第二个磷灰石相析出。提出了与适应化学计量学和第二相析出相一致的溶解度模型。即使在最低的CO2分压下沉淀,后者的碳酸盐含量也与珐琅矿物相似,这表明大约0.3摩尔含量的碳酸盐可以稳定磷灰石晶格。采用化学计量法测定牙釉质矿物Ca4.34 (HPO4).08(二氧化碳)29(PO4) 2.63(哦)。05,其溶解度积常数计算为Ksp = 1.74 (+/- 0.081)x10(-6),表示为平均活度积。
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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