Laboratory for Electrochemical Interfaces, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, MA 02139, USA.
J Phys Condens Matter. 2013 Jan 30;25(4):045004. doi: 10.1088/0953-8984/25/4/045004. Epub 2012 Dec 10.
Understanding the stability and reactivity of iron sulfide phases is key to developing predictive capabilities for assessing their corrosion and catalytic activity. The differences between the free surface and the bulk interior of such phases are of particular importance in this context. Here, we employ density functional theory to investigate the formation energetics and electronic structure of intrinsic Fe and S vacancies in bulk pyrite (FeS(2)) and on the pyrite (100) surface. The formation energies of intrinsic bulk vacancies of all charge states are found to be high, ranging from 1.7 to 3.7 eV. While the formation energies of surface vacancies are lower, varying from 1.4 to 2.1 eV for S vacancies and from 0.3 to 1.7 eV for Fe vacancies, they are too large to result in significant sub-stoichiometry in bulk pyrite at moderate temperatures. On the basis of charged defect formation energies and defect equilibria calculations, intrinsic charge carriers are expected to outnumber point defects by several orders of magnitude, and therefore, pure pyrite is not expected to demonstrate p-type or n-type conductivity. The presence of surface states is observed to cause a reduction in the band gap at the (100) surface, which was captured computationally and experimentally using tunneling spectroscopy measurements in this work. The vacancy-induced defect states behave as acceptor-like or donor-like defect states within the bulk band gap. The findings on the stoichiometry and the electronic structure of active sites on the (100) surface have important implications for the reactivity of pyrite.
了解硫化亚铁相的稳定性和反应性是开发预测其腐蚀和催化活性能力的关键。在这种情况下,这些相的自由表面和体相内部之间的差异尤为重要。在这里,我们采用密度泛函理论研究了在黄铁矿(FeS2)体相和黄铁矿(100)表面上本征 Fe 和 S 空位的形成能和电子结构。所有电荷态的本征体相空位的形成能都很高,范围在 1.7 到 3.7 eV 之间。虽然表面空位的形成能较低,范围在 1.4 到 2.1 eV 之间的 S 空位和在 0.3 到 1.7 eV 之间的 Fe 空位,但它们太大,无法在中等温度下导致黄铁矿体相中出现显著的亚化学计量。基于带电缺陷形成能和缺陷平衡计算,本征电荷载流子预计比点缺陷多几个数量级,因此,纯黄铁矿预计不会表现出 p 型或 n 型导电性。表面态的存在导致(100)表面的能带隙减小,这在本工作中通过隧道谱测量从计算和实验上进行了捕捉。空位诱导的缺陷态在体带隙内表现为受主型或施主型缺陷态。(100)表面活性位的化学计量和电子结构的研究结果对黄铁矿的反应性具有重要意义。