TenHuisen K S, Brown P W
Department of Materials Science and Engineering, Penn State University, University Park 16802, USA.
Biomaterials. 1999 Mar;20(5):427-34. doi: 10.1016/s0142-9612(98)00186-0.
Controlling the incorporation of Na and fluoride in apatite-based dental restoratives and analogs of bone formed under physiologic conditions may be desirable in controlling their long-term in vivo responses. Formation of these analogs was investigated. Hydrolysis of alpha-tricalcium phosphate (alpha-TCP) was carried out at physiologic temperature in NaF solutions and the solids product(s) were analyzed. alpha-TCP hydrolysis was complete within 48 h and the only solid products identified were apatites. Changes in solution chemistry were determined at 48 h and 4 weeks. Na and Ca concentrations were determined by spectrometric methods, P and F concentrations were determined by ion chromatography; pH values were obtained. The extent of fluoride and sodium incorporation in the apatites formed varied depending on the NaF concentration of the solution. Both increased with increasing NaF concentration. Apatite compositions ranged from Ca9.06(HPO4)0.94(PO4)5.06OH1.06 for hydrolysis in water to Ca9.28Na0.56(HPO4)(x)(PO4)(6-x)F0.920Hy for hydrolysis in 0.1 M NaF solution. The proportions of PO4, HPO4 and OH in Na- and F-containing apatites are indeterminate but obey the equation (y = constant+x). The (Ca+Na)/P ratio of the apatite formed by alpha-TCP hydrolysis in 0.1M NaF approaches 1.67 indicating the vacant Ca sites become almost completely filled by the Na ions. The surface areas of these apatites initially remain constant with increasing NaF concentrations; at elevated concentrations apatite surface areas decrease with increasing NaF concentration. This is consistent with the removal of Na from solution by its incorporation in the apatites, not by its adsorption onto their surfaces.
在控制基于磷灰石的牙科修复材料以及生理条件下形成的骨类似物中钠和氟的掺入量,对于控制它们在体内的长期反应可能是很有必要的。对这些类似物的形成进行了研究。在生理温度下,于氟化钠溶液中进行了α-磷酸三钙(α-TCP)的水解,并对固体产物进行了分析。α-TCP的水解在48小时内完成,鉴定出的唯一固体产物是磷灰石。在48小时和4周时测定了溶液化学性质的变化。通过光谱法测定钠和钙的浓度,通过离子色谱法测定磷和氟的浓度;获得了pH值。所形成的磷灰石中氟和钠的掺入程度因溶液中氟化钠的浓度而异。两者都随氟化钠浓度的增加而增加。磷灰石的组成范围从在水中水解得到的Ca9.06(HPO4)0.94(PO4)5.06OH1.06到在0.1M氟化钠溶液中水解得到的Ca9.28Na0.56(HPO4)(x)(PO4)(6 - x)F0.920Hy。含钠和氟的磷灰石中PO4、HPO4和OH的比例不确定,但符合方程(y =常数 + x)。在0.1M氟化钠中由α-TCP水解形成的磷灰石的(Ca + Na)/P比值接近1.67,表明空的钙位点几乎完全被钠离子填充。随着氟化钠浓度的增加,这些磷灰石的表面积最初保持不变;在较高浓度下,磷灰石表面积随氟化钠浓度的增加而减小。这与通过将钠掺入磷灰石而不是通过其吸附在磷灰石表面来从溶液中去除钠是一致的。