Abstract
Optimally doped manganite (LSMO)] is a ferromagnetic material with perspective use in applications due to colossal magnetoresistance and around room temperature. However, utilizing LSMO in thin-film form and complex heterostructures is limited due to the appearance of a magnetic dead layer, but interfacing LSMO with other transition metal oxides (TMOs) can reduce the magnetic dead layer. For instance, the LSMO layer in proximity to (SRO) remains magnetic down to 1–2 u.c. To illuminate this effect, we study the magnetic properties and orbital anisotropy of ultrathin LSMO deposited on (STO) compared with and without an SRO intermediate layer by resonant x-ray spectroscopy. We found that two events occur at the LSMO-SRO interface: Orbital rearrangement and charge transfer. Both effects cooperate, enhancing in-plane double exchange in ultrathin LSMO. Based on quantitative analysis and theoretical simulation of the x-ray spectra, magnetic stability mechanisms in LSMO/SRO are discussed in detail.
- Received 27 July 2021
- Accepted 8 November 2021
DOI:https://doi.org/10.1103/PhysRevMaterials.5.124404
©2021 American Physical Society