Elastic neutron-scattering studies of single-crystal LaFeAsO reveal that upon cooling, an onset of the tetragonal (T)-to-orthorhombic (O) structural transition occurs at T S ≈156 K, and it exhibits a sharp transition at T P ≈148 K. We argue that in the temperature range T S to T P , T and O structures may dynamically coexist possibly due to nematic spin correlations recently proposed for the iron pnictides, and we attribute T P to the formation of long-range O domains from the finite local precursors. The antiferromagnetic structure emerges at T N ≈140 K, with the iron moment direction along the O a axis. We extract the iron magnetic form factor and use the tabulated ⟨j 0 ⟩ of Fe, Fe2+, and Fe3+ to obtain a magnetic moment size of ∼0.8 μ B at 9.5 K.
Keywords
Physics and Astronomy, Materials Science and Engineering
Disciplines
Condensed Matter Physics | Materials Science and Engineering
CommentsThis article is from Physical Review B 82 (2010) Elastic neutron-scattering studies of single-crystal LaFeAsO reveal that upon cooling, an onset of the tetragonal ͑T͒-to-orthorhombic ͑O͒ structural transition occurs at T S Ϸ 156 K, and it exhibits a sharp transition at T P Ϸ 148 K. We argue that in the temperature range T S to T P , T and O structures may dynamically coexist possibly due to nematic spin correlations recently proposed for the iron pnictides, and we attribute T P to the formation of long-range O domains from the finite local precursors. The antiferromagnetic structure emerges at T N Ϸ 140 K, with the iron moment direction along the O a axis. We extract the iron magnetic form factor and use the tabulated ͗j 0 ͘ of Fe, Fe 2+ , and Fe 3+ to obtain a magnetic moment size of ϳ0.8 B at 9.5 K.