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20摄氏度时,人牙釉质的羟基磷灰石溶度积与pH值在4.6至7.6范围内的函数关系。

The hydroxyapatite solubility product of human dental enamel as a function of pH in the range 4.6-7.6 at 20 degrees C.

作者信息

Larsen M J, Jensen S J

机构信息

Department of Oral Anatomy, Dental Pathology and Operative Dentistry, Royal Dental College Aarhus, Denmark.

出版信息

Arch Oral Biol. 1989;34(12):957-61. doi: 10.1016/0003-9969(89)90052-6.

Abstract

Samples of 200 mg powdered enamel apatite were suspended in 10 ml of aqueous solutions made from phosphoric acid and calcium hydroxide for 60 days at 20 degrees C. Calcium and phosphate concentrations were determined by spectroscopy; pH and the concentrations of fluoride and carbonate by electrometry. The solubility product of hydroxyapatite varied linearly from 10-56.9 at pH 4.6 to 10-52.8 at pH 7.6. The carbonate concentration in the aqueous phase was too low to account for calcium carbonate complex formation of significance to the solubility product. After the equilibration, X-ray diffraction analysis of the powder showed that the salt was unchanged pure apatite with no trace of a transformation to brushite or any other calcium phosphate. A re-equilibration of some of the powder samples for another 60 days produced similar solubility products. Thus the change of the solubility product was most likely attributable to a pH-induced change of the ionic composition of the enamel crystal surface.

摘要

将200毫克粉末状牙釉质磷灰石样品悬浮于由磷酸和氢氧化钙制成的10毫升水溶液中,在20℃下放置60天。通过光谱法测定钙和磷酸盐浓度;通过电位测定法测定pH值以及氟化物和碳酸盐的浓度。羟基磷灰石的溶度积在pH 4.6时从10⁻⁵⁶.⁹线性变化至pH 7.6时的10⁻⁵².⁸。水相中碳酸盐浓度过低,无法解释对溶度积有显著影响的碳酸钙络合物的形成。平衡后,对该粉末进行X射线衍射分析表明,该盐为未发生变化的纯磷灰石,没有向透钙磷石或任何其他磷酸钙转变的痕迹。对一些粉末样品再平衡60天产生了相似的溶度积。因此,溶度积的变化很可能归因于pH值引起的牙釉质晶体表面离子组成的变化。

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