Institute of High Temperature Electrochemistry, Ekaterinburg 620137, Russia.
Phys Chem Chem Phys. 2019 Feb 27;21(9):4779-4790. doi: 10.1039/c9cp00172g.
Oxygen surface exchange and diffusion in Pr1.75Sr0.25Ni0.75Co0.25O4±δ have been investigated using two methods: pulsed isotope exchange (PIE) and oxygen isotope exchange with gas phase equilibration (IE GPE). Oxygen surface exchange kinetics is considered in the framework of two-step models including two consecutive stages: dissociative adsorption of oxygen and incorporation of oxygen adatoms into the crystal lattice. The rates of oxygen heterogeneous exchange (rH) as well as the rates of dissociative adsorption (ra) and oxygen incorporation (ri) have been calculated. The applicability of the two-step model is discussed based on the concept of a novel two-step mechanism with distributed rates of dissociative adsorption and incorporation of oxygen. It is shown that the two-step model can be applicable for the description of oxygen exchange kinetics in Pr1.75Sr0.25Ni0.75Co0.25O4±δ only at temperatures below 750 °C. Above this temperature, only the statistical model with distributed rates can be used. At low temperatures (<750 °C), the oxygen incorporation rate is found to be smaller than the rate of oxygen dissociative adsorption. Thus, under these experimental conditions the stage of oxygen incorporation is considered to be rate-determining. When increasing the temperature, the difference between ra and ri decreases and the stages become competing. The oxygen isotope exchange kinetic profiles obtained using the IE GPE method are found to be complicated and include a surface exchange stage as well as at least two diffusion relaxation processes. The reasons for the existence of these two processes are discussed.
采用两种方法研究了 Pr1.75Sr0.25Ni0.75Co0.25O4±δ 中的氧表面交换和扩散:脉冲同位素交换(PIE)和气相平衡氧同位素交换(IE GPE)。氧表面交换动力学是在两步模型的框架内考虑的,包括两个连续的阶段:氧的离解吸附和氧原子进入晶格。计算了氧非均相交换(rH)以及离解吸附(ra)和氧掺入(ri)的速率。基于具有分布的离解吸附和氧掺入速率的新两步机制的概念,讨论了两步模型的适用性。结果表明,两步模型仅在低于 750°C 的温度下适用于描述 Pr1.75Sr0.25Ni0.75Co0.25O4±δ 中的氧交换动力学。在该温度以上,只能使用具有分布速率的统计模型。在低温(<750°C)下,发现氧掺入速率小于氧离解吸附速率。因此,在这些实验条件下,氧掺入阶段被认为是决定速率的阶段。随着温度的升高,ra 和 ri 之间的差异减小,各个阶段变得相互竞争。用 IE GPE 方法获得的氧同位素交换动力学曲线很复杂,包括表面交换阶段以及至少两个扩散弛豫过程。讨论了这两个过程存在的原因。