高温独居石体系的计算模型研究

L. Motsomone, RG Diale, P. Ngoepe, R. Koen, H. Chauke
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摘要

独居石被广泛认为是核能发电可裂变原料的潜在来源,因为它通常在矿物矿石结构中含有大量的钍(Th)、铀(U)和稀土元素(ree)。目前,人们正在开发一种新的高温裂解工艺,以改善这些阳离子从坚固的独居石晶格中解放出来。目前从矿物中提取稀土元素的工艺过程复杂,使用了刺激性的化学物质。因此,这些过程有很大的优化空间。考虑到这一点,利用密度泛函理论(DFT)的第一性原理计算研究了独居石体系、t-CeSiO4和m-LaSiO4的稳定性,以更好地了解其固有的分子结构和温度对构象的影响。计算出的t-CeSiO4模型的晶格参数与实验值吻合良好(在3%以内),并认为系统的m-LaSiO4足够暴露于模拟反应条件下。在0 K时,t-CeSiO4比m-LaSiO4结构更稳定。采用LAMMPS代码中的半经验嵌入原子法原子间势研究了t-CeSiO4在高温下的晶格扩展。计算得到的a和b晶格参数在2200 K时呈线性扩展,而c晶格参数在同一温度范围内呈收缩。这一发现提供了对高温下独居石分子结构变化的深入了解,可能有助于等离子体裂解优化实验方法。
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Computational modelling studies for high temperature monazite systems
Monazite is widely considered as a potential source of fissile feedstock for nuclear power generation, as it generally contains significant quantity of thorium (Th), uranium (U) and rare earth elements (REEs) within the mineral ore structure. Currently, a new process of high-temperature cracking of monazite is under development to improve the liberation of these cations from the robust monazite lattice. The current process for extraction of the REEs from the mineral involves complicated processes which makes use of harsh chemicals. These process therefore has significant scope for optimisation. With this in mind, the stability of monazite systems, t-CeSiO4 and m-LaSiO4 was investigated using first-principle calculation employing density functional theory (DFT) to gain a better understanding of the inherent molecular structures and the influence of temperature on conformation. The calculated lattice parameters for the model of t-CeSiO4 were found to be in good agreement with the experimental values (within 3%) and deemed a sufficient m-LaSiO4 of the system to be exposed to simulated reaction conditions. The elastic properties suggested that t-CeSiO4 is the more stable structure compared to m-LaSiO4 structure at 0 K. Semi-empirical embedded atom method interatomic potentials incorporated in the LAMMPS code were also employed to investigate the lattice expansion of t-CeSiO4 at high temperatures. It was found that calculated a and b lattice parameters expand with a linear ratio to a temperature of 2200 K whereas the c parameter was found to contract in the same temperature range. The findings provided an in depth understanding of the monazite molecular structure change at higher temperatures that may be helpful in plasma cracking optimisation experimental methodologies.
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