Stoichiometry and Thermodynamic Solubility Properties of Dentin Mineral of Human Permanent and Deciduous Teeth

H. Komatsu, Kaori Sato, T. Aoba
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引用次数: 6

Abstract

Acquisition of substantial amounts of CO32-, HPO42- and other impurities is universally encountered in bioapatites from mammals. To date, however, there is a paucity of information about the stoichiometry and, on that basis, solubility product of dentin mineral. In this report, we summarize our experimental approach toward the determination of the stoichiometry model and thermodynamic solubility products of human dentin apatites. Dentin samples were collected separately from the coronal portion of permanent premolars (extracted for orthodontic reasons) and exfoliated deciduous teeth. Both pooled materials were pulverized with an agate-mortar, and then plasma-ashed at approx. 60°C to remove the organic matter. The stoichiometry model selected for these crystals was (Ca) 5-x (Mg) q (Na) u (HPO4) v (CO3) w (PO4) 3-y (OH) 1-z. These stoichiometric coefficients were analytically determined by assessing separately the labile or surface pools of the ionic species on the crystal surface and their stable pools in the bulk crystal lattice. The dentin mineral was equilibrated in dilute phosphoric solutions (100mg/100ml) at 25°C for a maximum of 28 days under constant partial pressures of CO2. The results showed that there are appreciable differences in the crystal stoichiometry between the permanent and deciduous dentin mineral and that the solubility product constants (KDN) were 4.11×10-45 for permanent dentin and 1.74×10-43 for deciduous dentin, which were determined under 1.8% CO2/N2. Notably, the solubility properties of the dentin mineral remained relatively constant in the range of 1.0 through 3.3% CO2/N2, whereas the discrete solubility data were obtained below and above the corresponding partial pressure of CO2.
恒牙和乳牙牙本质矿物的化学计量学和热力学溶解度
在哺乳动物的生物磷灰石中普遍存在大量的CO32-、HPO42-和其他杂质。然而,迄今为止,关于牙本质矿物的化学计量学和在此基础上的溶解度积的资料还很缺乏。在这篇报告中,我们总结了我们测定牙本质磷灰石的化学计量模型和热力学溶解度产物的实验方法。牙本质样本分别从恒前磨牙(因正畸原因拔出)的冠状部分和脱落的乳牙上采集。这两种混合材料都用玛瑙砂浆粉碎,然后在大约。60℃去除有机物。这些晶体的化学计量模型为(Ca) 5-x (Mg) q (Na) u (HPO4) v (CO3) w (PO4) 3-y (OH) 1-z。这些化学计量系数是通过分别评估晶体表面上离子的不稳定或表面池和它们在大块晶格中的稳定池来分析确定的。牙本质矿物在25°C的稀磷溶液(100mg/100ml)中平衡,在CO2的恒定分压下平衡最多28天。结果表明,恒牙本质与乳牙本质矿物的晶体化学计量学存在明显差异,恒牙本质的溶解度积常数(KDN)为4.11×10-45,乳牙本质的溶解度积常数(KDN)为1.74×10-43,这是在1.8% CO2/N2条件下测定的。值得注意的是,牙本质矿物的溶解度在1.0 ~ 3.3% CO2/N2范围内保持相对恒定,而在相应的CO2分压下和高于相应的CO2分压时获得离散的溶解度数据。
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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