Moreno E C, Aoba T
Forsyth Dental Center, Boston, MA 02115.
J Biol Buccale. 1990 Sep;18(3):195-201.
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.
在25摄氏度下,于二氧化碳分压受控(在与氮气的混合物中为0.005%至3.33%)的条件下,研究了人牙釉质在稀磷酸溶液(0.07毫摩尔/升至1.54毫摩尔/升)中的溶解度。牙釉质矿物质被视为含有酸式磷酸盐的碳酸磷灰石,其化学计量式为[Ca]5 - x - y[HPO4]v[PO4]3 - x[CO3]w[OH]l - x - y。在平衡过程中,如在电子显微镜下观察到的那样,会析出第二个磷灰石相。提出了与调整后的化学计量式和第二个相的析出相一致的溶解度模型。即使在最低二氧化碳分压下析出,后者的碳酸盐含量似乎也与牙釉质矿物质的碳酸盐含量相似,这表明约0.3的摩尔碳酸盐含量可稳定磷灰石晶格。根据所采用的牙釉质矿物质化学计量式Ca4.34(HPO4).08(CO3).29(PO4)2.63(OH).05,计算出其溶度积常数为Ksp = 1.74(±0.081)×10(-6),以平均活度积表示。