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Growth and Electrostatic/chemical Properties of Metal/LaAlO3/SrTiO3 Heterostructures
Published on: February 8, 2018
Revisiting La0.5Sr1.5MnO4 lattice distortion and charge ordering with multi-beam resonant diffraction
Wen Chung Liu1, Yi Hua Chiu1, Ying Yu Kung1
1Department of Physics, Tsing Hua University, Hsinchu, 30013, Taiwan.
Sinusoidal distortions in La0.5Sr1.5MnO4 were observed using multi-beam resonant X-ray diffraction. This method can resolve distortion modes and probe charge disproportion at manganese sites.
Area of Science:
- Condensed Matter Physics
- Materials Science
- Crystallography
Background:
- La0.5Sr1.5MnO4 exhibits complex phases at low temperatures.
- Understanding lattice distortions is crucial for its electronic properties.
Purpose of the Study:
- To observe and characterize sinusoidal wave-type distortions in La0.5Sr1.5MnO4.
- To demonstrate the capability of multi-beam resonant X-ray diffraction (MRXD) for resolving distortion modes.
- To investigate charge disproportion between manganese sites.
Main Methods:
- Multi-beam resonant X-ray diffraction (MRXD) with (7/4 7/4 0) fractional primary diffraction.
- Measurement of two four-beam diffractions with opposite asymmetry at 6.5545 keV.
- Comparison with simulations based on dynamical X-ray diffraction theory.
- Analysis of MRXD profile sensitivity to incident X-ray energy near the Mn K edge.
Main Results:
- Observed sinusoidal wave-type distortions in the low-temperature orthorhombic phase of La0.5Sr1.5MnO4.
- Demonstrated that MRXD can resolve distortion modes perpendicular to momentum transfer via a single azimuthal scan.
- Confirmed the sensitivity of MRXD to charge disproportion between manganese sites, indicating a small charge disproportion feature.
Conclusions:
- MRXD is a powerful technique for characterizing lattice distortions in materials.
- The study provides insights into the low-temperature phase of La0.5Sr1.5MnO4.
- The findings contribute to understanding the relationship between structure and electronic properties in manganites.
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