Kerisit Sebastien, Rosso Kevin M
Chemical and Materials Sciences Division, Pacific Northwest National Laboratory, Richland, Washington 99354, USA.
J Chem Phys. 2007 Sep 28;127(12):124706. doi: 10.1063/1.2768522.
The mobility of electrons injected into iron oxide minerals via abiotic and biotic electron transfer processes is one of the key factors that control the reductive dissolution of such minerals. Building upon our previous work on the computational modeling of elementary electron transfer reactions in iron oxide minerals using ab initio electronic structure calculations and parametrized molecular dynamics simulations, we have developed and implemented a kinetic Monte Carlo model of charge transport in hematite that integrates previous findings. The model aims to simulate the interplay between electron transfer processes for extended periods of time in lattices of increasing complexity. The electron transfer reactions considered here involve the IIIII valence interchange between nearest-neighbor iron atoms via a small polaron hopping mechanism. The temperature dependence and anisotropic behavior of the electrical conductivity as predicted by our model are in good agreement with experimental data on hematite single crystals. In addition, we characterize the effect of electron polaron concentration and that of a range of defects on the electron mobility. Interaction potentials between electron polarons and fixed defects (iron substitution by divalent, tetravalent, and isovalent ions and iron and oxygen vacancies) are determined from atomistic simulations, based on the same model used to derive the electron transfer parameters, and show little deviation from the Coulombic interaction energy. Integration of the interaction potentials in the kinetic Monte Carlo simulations allows the electron polaron diffusion coefficient and density and residence time around defect sites to be determined as a function of polaron concentration in the presence of repulsive and attractive defects. The decrease in diffusion coefficient with polaron concentration follows a logarithmic function up to the highest concentration considered, i.e., approximately 2% of iron(III) sites, whereas the presence of repulsive defects has a linear effect on the electron polaron diffusion. Attractive defects are found to significantly affect electron polaron diffusion at low polaron to defect ratios due to trapping on nanosecond to microsecond time scales. This work indicates that electrons can diffuse away from the initial site of interfacial electron transfer at a rate that is consistent with measured electrical conductivities, but that the presence of certain kinds of defects will severely limit the mobility of donated electrons.
通过非生物和生物电子转移过程注入氧化铁矿物中的电子迁移率,是控制此类矿物还原溶解的关键因素之一。基于我们之前利用从头算电子结构计算和参数化分子动力学模拟对氧化铁矿物中基本电子转移反应进行计算建模的工作,我们开发并实现了一个整合了先前研究结果的赤铁矿电荷输运动力学蒙特卡洛模型。该模型旨在模拟在复杂度不断增加的晶格中长时间内电子转移过程之间的相互作用。这里考虑的电子转移反应涉及通过小极化子跳跃机制在相邻铁原子之间的III-II价态互换。我们的模型预测的电导率的温度依赖性和各向异性行为与赤铁矿单晶的实验数据吻合良好。此外,我们还表征了电子极化子浓度以及一系列缺陷对电子迁移率的影响。基于用于推导电子转移参数的相同模型,通过原子模拟确定了电子极化子与固定缺陷(二价、四价和等价离子取代铁以及铁和氧空位)之间的相互作用势,其与库仑相互作用能的偏差很小。在动力学蒙特卡洛模拟中整合相互作用势,使得在存在排斥性和吸引性缺陷的情况下,能够确定电子极化子扩散系数、密度以及在缺陷位点周围的停留时间作为极化子浓度的函数。在考虑的最高浓度(即约2%的铁(III)位点)之前,扩散系数随极化子浓度的降低遵循对数函数,而排斥性缺陷对电子极化子扩散具有线性影响。发现由于在纳秒到微秒时间尺度上的俘获,吸引性缺陷在低极化子与缺陷比时会显著影响电子极化子扩散。这项工作表明,电子能够以与测量电导率一致的速率从界面电子转移的初始位点扩散开,但某些类型缺陷的存在将严重限制所提供电子的迁移率。