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Uncharacteristic phase separation trends with the ionic size in cobaltites
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Citations
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References
2009
Year
Magnetic PropertiesSingle CrystalsEngineeringMagnetic ResonanceIonic SizeChemistryMagnetic MaterialsElastic NeutronMagnetismMineral-fluid InteractionQuantum MaterialsPhase SeparationMaterials ScienceSolid-state IonicPhysicsCobalt Perovskite SystemCrystallographyCondensed Matter TheorySolid-state PhysicQuantum MagnetismFerromagnetismPhase EquilibriumNatural SciencesCondensed Matter PhysicsApplied PhysicsGeochemistry
Using elastic neutron scattering on single crystals of ${\text{La}}_{1\ensuremath{-}x}{A}_{x}{\text{CoO}}_{3}$ ($A={\text{Ca}}^{2+}$, ${\text{Sr}}^{2+}$, and ${\text{Ba}}^{2+}$), we found the development of magnetic superstructures below the global magnetic transition to be strongly dependent on the size of the $A$-site dopant, $⟨{r}_{A}⟩$, in an unusual way. Upon reducing the $⟨{r}_{A}⟩$ (i.e., as with Ca doping), only a commensurate ferromagnetic cluster phase is evident. On expanding the $⟨{r}_{A}⟩$, the tendency toward coexistence of competing ferromagnetic and antiferromagnetic orders increases giving rise to an inhomogeneous ground state. The antiferromagnetic ordered state, initially incommensurate, continuously strengthens and becomes commensurate with long-range order and a characteristic cubic wave vector of ${\stackrel{P\vec}{Q}}_{c}=(0.25,0.25,0.25)$ with $x$. The two competing order parameters become comparable in magnitude indicative of the phase-separated nature of the cobalt perovskite system.
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