Kazan Federal University, Kazan, Russia.
A.A. Baikov Institute of Metallurgy and Materials Science, Russian Academy of Sciences, Moscow, Russia.
Radiat Res. 2021 Feb 1;195(2):200-210. doi: 10.1667/RADE-20-00194.1.
Octacalcium phosphate (OCP) {Ca8H2(PO4)6×5H2O] has attracted increasing attention over the last decade as a transient intermediate to the biogenic apatite for bone engineering and in studies involving the processes of pathological calcification. In this work, OCP powders obtained by hydrolysis of dicalcium phosphate dehydrate were subjected to X- and γ-ray irradiation and studied by means of stationary and pulsed electron paramagnetic resonance at 9, 36 and 94 GHz microwave frequencies. Several types of paramagnetic centers were observed in the investigated samples. Their spectroscopic parameters (components of the g and hyperfine tensors) were determined. Based on the extracted parameters, the induced centers were ascribed to H0, CO33-, CO2- and nitrogen-centered (presumably NO32-) radicals. The spectroscopic parameters of the nitrogen-centered stable radical in OCP powders were found to be markedly different from those in hydroxyapatite. According to X-ray diffraction data, γ-ray irradiation allowed the phase composition of calcium phosphates to change; all minor phases with the exception of OCP and hydroxyapatite disappeared, while the OCP crystal lattice parameters changed after irradiation. The obtained results could be used for the tracing of mineralization processes from their initiation to completion of the final product, identification of the OCP phase, and to follow the influence of radiation processes on phase composition of calcium phosphates.
八钙磷酸盐(OCP){Ca8H2(PO4)6×5H2O]在过去十年中作为生物磷灰石的短暂中间体,在骨工程和涉及病理钙化过程的研究中引起了越来越多的关注。在这项工作中,通过二水磷酸氢钙水解得到的 OCP 粉末经过 X 射线和γ射线辐照,并在 9、36 和 94 GHz 微波频率下通过静态和脉冲电子顺磁共振进行研究。在研究的样品中观察到几种类型的顺磁中心。确定了它们的光谱参数(g 和超精细张量的分量)。基于提取的参数,将诱导中心归因于 H0、CO33-、CO2-和氮中心(可能是 NO32-)自由基。OCP 粉末中氮中心稳定自由基的光谱参数与羟磷灰石明显不同。根据 X 射线衍射数据,γ射线辐照允许改变磷酸钙的相组成;除 OCP 和羟磷灰石外,所有次要相都消失了,而 OCP 晶格参数在辐照后发生了变化。所获得的结果可用于从起始到最终产物完成的矿化过程的追踪、OCP 相的鉴定以及辐射过程对磷酸钙相组成的影响。