Lee Doh-Kwon, Kogel Lutz, Ebbinghaus Stefan G, Valov Ilia, Wiemhoefer Hans-Dieter, Lerch Martin, Janek Juergen
Institute of Physical Chemistry, Justus-Liebig-University, Heinrich-Buff-Ring 58, D-35392, Giessen, Germany.
Phys Chem Chem Phys. 2009 May 7;11(17):3105-14. doi: 10.1039/b818474g. Epub 2009 Mar 3.
A crystallographic cage structure endows mayenite (Ca(12)Al(14)O(33) or 12CaO.7Al(2)O(3); C(12)A(7)) with remarkable properties, making it either an oxygen solid electrolyte or an inorganic electride upon reduction. In order to better understand the transport properties of C(12)A(7), we measured the equilibrium total conductivity as well as the electronic partial conductivity of single crystal mayenite as functions of activity of oxygen or water vapor at different temperatures in the range 1073 < or =T/K < or = 1273. A point defect model based on the assumption that the framework Ca(12)Al(14)O(32) acts as a pseudo-donor describes well the isothermal conductivity vs. oxygen activity, enabling us to deconvolute the ionic and electronic partial conductivities. The ionic transference number evaluated therefrom clearly demonstrates how C(12)A(7) is converted from a solid electrolyte to an electride depending on the oxygen content. In addition, besides the well known degradation of ionic conductivity by water uptake, a short-term increase of conductivity upon abrupt hydration was recognized and interpreted as due to the transient increase in the concentration of oxygen interstitial along with proton in the initial stage of hydration. For the fully hydrated C(12)A(7), the conductivity relaxation curves upon switching of oxygen activity in a fixed water vapor pressure appear non-monotonic showing the extrema only in the plateau conductivity regime. A defect structure based hypothesis is proposed to explain the 2-fold re-equilibration kinetics.
一种晶体笼状结构赋予钙铝石(Ca(12)Al(14)O(33) 或 12CaO·7Al(2)O(3);C(12)A(7))显著的性能,使其在还原时成为氧固体电解质或无机电子化物。为了更好地理解 C(12)A(7) 的传输性质,我们测量了单晶钙铝石在 1073≤T/K≤1273 范围内不同温度下作为氧或水蒸气活度函数的平衡总电导率以及电子分电导率。基于框架 Ca(12)Al(14)O(32) 作为准施主的假设的点缺陷模型很好地描述了等温电导率与氧活度的关系,使我们能够解卷积离子和电子分电导率。由此评估的离子迁移数清楚地表明了 C(12)A(7) 如何根据氧含量从固体电解质转变为电子化物。此外,除了众所周知的因吸水导致离子电导率下降外,还认识到在突然水合时电导率会短期增加,并将其解释为水合初始阶段氧间隙原子与质子浓度的瞬态增加所致。对于完全水合的 C(12)A(7),在固定水蒸气压力下切换氧活度时的电导率弛豫曲线呈现非单调,仅在平台电导率区域出现极值。提出了一种基于缺陷结构的假设来解释这种双重再平衡动力学。