超出了目前硅酸盐陶瓷和骨骼之间的结合的解释

A. Osaka
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引用次数: 1

摘要

Hench, Kokubo, Yamamuro等人在20世纪80年代研究的材料与骨组织之间强键的形成,重新审视了磷灰石沉积在中孔或微孔硅胶上的一些见解,通过在四乙氧基硅烷,聚乙二醇和水的体系中进行相分离而得到。对硅胶的磷灰石沉积能力的测试表明,Kokubo模拟体液中钙离子、磷酸盐离子和羟基离子的增加对磷灰石成核速率的影响不同,表明有必要修改原来的磷灰石成核简单模型:钙离子吸附触发成核。本文综述了钛表面经过化学(h2o2)和加热(CHT)处理制备的锐钛矿层中磷灰石的形成过程,指出钙离子和磷酸盐离子的平衡聚集对磷灰石成核具有重要意义。建议将CHT层作为骨结合测试的参考材料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
BEYOND CURRENT INTERPRETATION OF BONDING BETWEEN SILICATE CERAMICS AND BONE
: The formation of strong bond between material and bone tissue, studied by Hench, Kokubo, Yamamuro, or others in 1980's is revisited to obtain some insight into apatite deposition on meso- or microporous silica gel, derived by phase separation in the system tetraethoxysilane, polyethylene glycol, and water. Testing the apatite-depositing ability on the silica gels indicated that the increase in calcium, phosphate, and hydroxyl ions in Kokubo's simulated body fluid differently affected the apatite nucleation rate, and suggested necessity of modifying the original simplistic model of apatite nucleation: calcium ion adsorption triggered nucleation. Apatite formation was reviewed on anatase layer prepared on Ti due to chemical (H 2 O 2 ) and heating treatments (CHT procedure), and balanced clustering of calcium and phosphate ions is significant for the apatite nucleation. CHT layer is proposed as a reference material for bone-bonding testing.
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