Vergari L, Wu H, Scarlat R O
Department of Nuclear Engineering, University of California Berkeley, 2521 Hearst. Ave, Berkeley, California 94720, United States.
Department of Nuclear, Plasma and Radiological Engineering, University of Illinois Urbana-Champaign, 104 S. Wright Street, Urbana, Illinois 61801, United States.
ACS Appl Eng Mater. 2024 Jun 17;2(6):1483-1502. doi: 10.1021/acsaenm.3c00764. eCollection 2024 Jun 28.
This study demonstrates that the reaction of LiBeF (FLiBe) with graphite both in the liquid phase and the gas phase of the molten salt leads to the formation of covalent and semi-ionic carbon-fluorine bonds at the graphite surface and is accompanied by surface microstructural changes, removal of C-O groups, and deposition of metallic beryllium, based on XPS, Raman, and glow discharge mass spectroscopy characterization. At 700 °C, the observed surface density of C-F is higher after 240 h than after 12 h of exposure to molten FLiBe salt; the kinetics of covalent C-F formation is slower than that of semi-ionic C-F formation, and the relative amount of semi-ionic C-F content increases with depth. The graphite sample exposed to the cover gas exhibits less surface fluorination than the salt-exposed sample, with predominantly semi-ionic C-F. Based on these observations and the observed LiF/BeF ratio by surface XPS, the hypotheses that fluorination of the salt-exposed graphite occurs via a gas-phase mechanism or that it requires salt intrusion are refuted; future studies are warranted on the transport of C-F semi-ionic and covalent species in graphite at high temperatures.
本研究表明,在熔盐的液相和气相中,LiBeF(FLiBe)与石墨的反应会导致在石墨表面形成共价和半离子型碳氟键,并伴随着表面微观结构变化、C-O基团的去除以及金属铍的沉积,这是基于X射线光电子能谱(XPS)、拉曼光谱和辉光放电质谱表征得出的结论。在700°C下,暴露于熔融FLiBe盐240小时后观察到的C-F表面密度高于暴露12小时后的;共价C-F形成的动力学比半离子型C-F形成的慢,且半离子型C-F含量的相对量随深度增加。暴露于覆盖气体中的石墨样品比暴露于盐中的样品表现出更少的表面氟化,主要为半离子型C-F。基于这些观察结果以及通过表面XPS观察到的LiF/BeF比率,盐暴露石墨的氟化通过气相机制发生或需要盐侵入的假设被推翻;未来有必要对高温下石墨中C-F半离子型和共价型物种的传输进行研究。