Smart Tyler J, Ping Yuan
Department of Physics, University of California-Santa Cruz, Santa Cruz, CA 95064, United States of America.
J Phys Condens Matter. 2017 Oct 4;29(39):394006. doi: 10.1088/1361-648X/aa7e3d. Epub 2017 Jul 7.
Hematite (α-FeO) is a promising candidate as a photoanode material for solar-to-fuel conversion due to its favorable band gap for visible light absorption, its stability in an aqueous environment and its relatively low cost in comparison to other prospective materials. However, the small polaron transport nature in α-FeO results in low carrier mobility and conductivity, significantly lowering its efficiency from the theoretical limit. Experimentally, it has been found that the incorporation of oxygen vacancies and other dopants, such as Sn, into the material appreciably enhances its photo-to-current efficiency. Yet no quantitative explanation has been provided to understand the role of oxygen vacancy or Sn-doping in hematite. We employed density functional theory to probe the small polaron formation in oxygen deficient hematite, N-doped as well as Sn-doped hematite. We computed the charged defect formation energies, the small polaron formation energy and hopping activation energies to understand the effect of defects on carrier concentration and mobility. This work provides us with a fundamental understanding regarding the role of defects on small polaron formation and transport properties in hematite, offering key insights into the design of new dopants to further improve the efficiency of transition metal oxides for solar-to-fuel conversion.
赤铁矿(α-Fe₂O₃)因其对可见光吸收具有合适的带隙、在水环境中的稳定性以及与其他潜在材料相比成本相对较低,是一种很有前景的用于太阳能转化为燃料的光阳极材料候选物。然而,α-Fe₂O₃中的小极化子传输特性导致载流子迁移率和电导率较低,显著降低了其效率,使其低于理论极限。在实验中,人们发现将氧空位和其他掺杂剂(如Sn)掺入该材料可显著提高其光电流效率。然而,尚未提供定量解释来理解氧空位或Sn掺杂在赤铁矿中的作用。我们采用密度泛函理论来探究缺氧赤铁矿、N掺杂以及Sn掺杂赤铁矿中的小极化子形成情况。我们计算了带电缺陷形成能、小极化子形成能和跳跃激活能,以了解缺陷对载流子浓度和迁移率的影响。这项工作为我们提供了关于缺陷在赤铁矿中小极化子形成和传输特性方面作用的基本理解,为设计新的掺杂剂以进一步提高过渡金属氧化物用于太阳能转化为燃料的效率提供了关键见解。