Otto-Schott-Institut, Jena University, Fraunhoferstr. 6, 07743 Jena, Germany.
J Chem Phys. 2012 Jun 14;136(22):224502. doi: 10.1063/1.4717713.
The kinetics of the temperature dependent redox reaction between chromium and manganese (Cr(6+) + 3Mn(2+)⇌Cr(3+) + 3Mn(3+)) in highly viscous silicate melts were studied by UV-vis-NIR spectroscopy at temperatures in the range from 25 to 800 °C. At high temperatures, the reaction is in equilibrium. During cooling, it is continuously shifted to the right. During cooling from Tg+50 K to Tg (Tg = glass transition temperature), a further decrease in the Cr(6+) concentration was obtained which, however, was less pronounced if larger cooling rates were applied. In this temperature range, the kinetics plays an important part. Finally, at a certain temperatures below Tg, the equilibrium was frozen. The temperature, the equilibrium is frozen in decreases with decreasing cooling rate. It also decreases with the glass transition temperature of the respective composition. The activation energies increase with the activation energies of the viscosity of the respective melt. The redox reaction is controlled by the viscosity, i.e., the rearrangement of the glass network and not by diffusion. The reason is a drastic change in the coordination spheres during the reaction which leads to a high inner reorganization energy according to Marcus' Theory.
在 25 至 800°C 的温度范围内,通过紫外可见近红外光谱研究了高粘性硅酸盐熔体中铬和锰之间温度依赖的氧化还原反应(Cr(6+) + 3Mn(2+)⇌Cr(3+) + 3Mn(3+))的动力学。在高温下,反应处于平衡状态。在冷却过程中,它不断向右移动。在从 Tg+50 K 冷却到 Tg(Tg = 玻璃化转变温度)的过程中,Cr(6+)浓度进一步降低,但如果采用较大的冷却速率,这种降低则不太明显。在这个温度范围内,动力学起着重要的作用。最后,在低于 Tg 的某个温度下,平衡被冻结。平衡被冻结的温度随冷却速率的降低而降低。它还随相应组成的玻璃化转变温度降低而降低。活化能随熔体相应粘度的活化能增加而增加。氧化还原反应受粘度控制,即玻璃网络的重排,而不是扩散。原因是反应过程中配位球发生剧烈变化,根据马库斯理论导致高的内部重组能。