Department of Physics & Astronomy, University of British Columbia, Vancouver, British Columbia V6T 1Z1, Canada.
Phys Rev Lett. 2013 Mar 1;110(9):097004. doi: 10.1103/PhysRevLett.110.097004.
We revisit the normal-state electronic structure of Sr(2)RuO(4) by angle-resolved photoemission spectroscopy with improved data quality, as well as ab initio band structure calculations in the local-density approximation with the inclusion of spin-orbit coupling. We find that the current model of a single surface layer (√2×√2)R45° reconstruction does not explain all detected features. The observed depth-dependent signal degradation, together with the close quantitative agreement with the slab calculations based on the surface crystal structure as determined by low-energy electron diffraction, reveal that-at a minimum-the subsurface layer also undergoes a similar although weaker reconstruction. This model accounts for all features-a key step in understanding the electronic structure-and indicates a surface-to-bulk progression of the electronic states driven by structural instabilities. Finally, we find no evidence for other phases stemming from either topological bulk properties or, alternatively, the interplay between spin-orbit coupling and the broken symmetry of the surface.
我们通过角分辨光电子能谱(ARPES)重新研究了 Sr(2)RuO(4) 的正常态电子结构,同时还进行了包含自旋轨道耦合的局域密度近似下的第一性原理能带结构计算。我们发现,目前的单层(√2×√2)R45°重构模型并不能解释所有检测到的特征。观察到的深度相关信号衰减,以及与基于低能电子衍射确定的表面晶体结构的基于薄片计算的定量吻合度,表明-至少-亚表面层也经历了类似但较弱的重构。该模型解释了所有的特征-这是理解电子结构的关键步骤-并表明电子态的表面到体的进展是由结构不稳定性驱动的。最后,我们没有发现源自拓扑体性质或自旋轨道耦合与表面对称性破缺相互作用的其他相的证据。