Hamai Ryo, Maeda Hirotaka, Sawai Hikaru, Shirosaki Yuki, Kasuga Toshihiro, Miyazaki Toshiki
Graduate School of Life Science and Systems Engineering, Kyushu Institute of Technology, 2-4, Hibikino, Wakamatsu-ku, Kitakyushu, 808-0196, Japan.
J Mater Chem B. 2018 Jan 7;6(1):174-182. doi: 10.1039/c7tb02363d. Epub 2017 Dec 12.
Organic-inorganic composites are novel bone substitutes that can ameliorate the mismatch of Young's moduli between natural bone and implanted ceramics. Phosphate groups contribute to the formation of apatite in a simulated body fluid (SBF) and the adhesion of osteoblast-like cells. Therefore, modification of a polymer with these functional groups is expected to enhance the ability of the organic-inorganic composite to bond with bone. Two phosphate groups have been used, phosphonic acid (-C-POH) and phosphoric acid (-O-POH). However, the effects of structural differences between these phosphate groups have not been clarified. In this study, the apatite formation of copolymers modified with Ca and either -C-POH or -O-POH was examined. The mechanism of apatite formation is discussed based on analytical and computational approaches. The copolymers containing -O-POH, but not those containing -C-POH, formed apatite in the SBF, although both released similar amounts of Ca into the SBF. Adsorption of HPO from -O-POH in the SBF following Ca adsorption was confirmed by zeta-potential measurement and X-ray photoelectron spectroscopy. The measurement of the complex formation constant revealed that the -O-PO Ca complex was thermodynamically unstable enough to convert into CaHPO, which was not the case with -C-PO Ca. The formation of CaHPO-based clusters was found to be a key factor for apatite nucleation. In conclusion, this study revealed that modification with -O-POH was more effective for enhancing apatite formation compared with -C-POH.
有机-无机复合材料是新型骨替代物,可改善天然骨与植入陶瓷之间杨氏模量的不匹配。磷酸基团有助于在模拟体液(SBF)中形成磷灰石,并促进成骨样细胞的黏附。因此,用这些官能团对聚合物进行改性有望增强有机-无机复合材料与骨结合的能力。已经使用了两种磷酸基团,即膦酸(-C-POH)和磷酸(-O-POH)。然而,这些磷酸基团之间结构差异的影响尚未明确。在本研究中,考察了用钙和-C-POH或-O-POH改性的共聚物的磷灰石形成情况。基于分析和计算方法讨论了磷灰石形成的机制。含有-O-POH的共聚物在SBF中形成了磷灰石,而含有-C-POH的共聚物则没有,尽管两者向SBF中释放的钙量相似。通过zeta电位测量和X射线光电子能谱证实了在钙吸附后,SBF中-O-POH的HPO 吸附情况。配合物形成常数的测量表明,-O-PO Ca配合物在热力学上不稳定,足以转化为CaHPO ,而-C-PO Ca则不然。发现基于CaHPO 的簇的形成是磷灰石成核的关键因素。总之,本研究表明,与-C-POH相比,用-O-POH改性对增强磷灰石形成更有效。