Commensurate Stripes and Phase Coherence in Manganites Revealed with Cryogenic Scanning Transmission Electron Microscopy
Ismail El Baggari, Benjamin H. Savitzky, Alemayehu S. Admasu, Jaewook, Kim, Sang-Wook Cheong, Robert Hovden, Lena F. Kourkoutis

TL;DR
This study uses cryogenic scanning transmission electron microscopy to reveal that incommensurate charge order in manganites is actually lattice-commensurate at the atomic level, highlighting the role of lattice coupling and phase coherence.
Contribution
It demonstrates that incommensurate diffraction signals can arise from phase inhomogeneity in a lattice-locked charge order, providing a microscopic understanding of charge order in manganites.
Findings
Charge order is lattice-commensurate at both room and cryogenic temperatures.
Phase inhomogeneity at room temperature transitions to phase coherence at 93K.
Atomic displacements indicate strong charge-lattice coupling.
Abstract
Incommensurate charge order in hole-doped oxides is intertwined with exotic phenomena such as colossal magnetoresistance, high-temperature superconductivity, and electronic nematicity. Here, we map at atomic resolution the nature of incommensurate order in a manganite using scanning transmission electron microscopy at room temperature and cryogenic temperature ( 93K). In diffraction, the ordering wavevector changes upon cooling, a behavior typically associated with incommensurate order. However, using real space measurements, we discover that the underlying ordered state is lattice-commensurate at both temperatures. The cations undergo picometer-scale (6-11 pm) transverse displacements, which suggests that charge-lattice coupling is strong and hence favors lattice-locked modulations. We further unearth phase inhomogeneity in the periodic lattice displacements at room…
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