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Published on: March 24, 2019
Local inhomogeneous state in multiferroic SmCrO3.
G N P Oliveira1, R C Teixeira2, R P Moreira2
1IFIMUP-Instituto de Física de Materiais Avançados, Nanotecnologia e Fotónica, Departamento de Física e Astronomia da Faculdade de Ciências da Universidade do Porto, Rua do Campo Alegre, 687, 4169-007, Porto, Portugal. goliveira@fc.up.pt.
Researchers investigated rare-earth orthochromites, specifically samarium chromium oxide (SmCrO3), to understand their ferroelectric order. They discovered an emerging local distortion near room temperature, indicating a complex, inhomogeneous polar state rather than a simple structural phase transition.
Area of Science:
- Solid State Physics
- Materials Science
- Crystallography
Background:
- Rare-earth orthochromites (RCrO3) with distorted perovskite structures exhibit debated ferroelectric order origins.
- The question of whether these materials are magnetically driven improper ferroelectrics, similar to rare-earth manganites and orthoferrites, remains a key research area.
Purpose of the Study:
- To investigate the atomic-scale behavior of samarium chromium oxide (SmCrO3) to elucidate the origin of its ferroelectric order.
- To determine if the ferroelectric phase in SmCrO3 arises from a simple structural transition or a more complex phenomenon.
Main Methods:
- Atomic-scale study of the samarium chromium oxide (SmCrO3) system.
- Electric Field Gradient (EFG) measurements.
- First-principles calculations.
Main Results:
- A distortion of the samarium (Sm) local environment emerges near room temperature within the paramagnetic phase.
- The observed emergent phase in SmCrO3 is not consistent with the previously reported Pna21 structure.
- A local inhomogeneous state, characterized by the coexistence of regular non-polar and polar distorted environments, develops at low temperatures.
Conclusions:
- The ferroelectric order in SmCrO3 does not stem from a simple structural phase transition to a Pna21 structure.
- A complex, low-temperature inhomogeneous state with coexisting polar and non-polar environments is responsible for the observed phenomena.
- This finding challenges existing models for ferroelectricity in rare-earth orthochromites.
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