Abstract
The many surface reconstructions of (110)-oriented lanthanum strontium manganite (, LSMO) were followed as a function of the oxygen chemical potential () and the surface cation composition. Decreasing causes Mn to migrate across the surface, enforcing phase separation into -site-rich areas and a variety of composition-related, structurally diverse -site-rich reconstructions. The composition of these phase-separated structures was quantified with scanning tunneling microscopy, and these results were used to build a two-dimensional phase diagram of the LSMO(110) equilibrium surface structures.
- Received 19 September 2020
- Revised 27 May 2021
- Accepted 30 August 2021
DOI:https://doi.org/10.1103/PhysRevMaterials.5.L092401
©2021 American Physical Society