3,090 research outputs found

    Orbital density wave induced by electron-lattice coupling in orthorhombic iron pnictides

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    In this paper we explore the magnetic and orbital properties closely related to a tetragonal-orthorhombic structural phase transition in iron pnictides based on both two- and five-orbital Hubbard models. The electron-lattice coupling, which interplays with electronic interaction, is self-consistently treated. Our results reveal that the orbital polarization stabilizes the spin density wave (SDW) order in both tetragonal and orthorhombic phases. However, the ferro-orbital density wave (F-ODW) only occurs in the orthorhombic phase rather than in the tetragonal one. Magnetic moments of Fe are small in the intermediate Coulomb interaction region for the striped antiferromangnetic phase in the realistic five orbital model. The anisotropic Fermi surface in the SDW/ODW orthorhombic phase is well in agreement with the recent angle-resolved photoemission spectroscopy experiments. These results suggest a scenario that the magnetic phase transition is driven by the ODW order mainly arising from the electron-lattice coupling.Comment: 21 pages, 10 figure

    NH3_{3} (1,1) hyperfine intensity anomalies in the Orion A molecular cloud

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    In LTE, the two inner satellite lines (ISLs) and the two outer satellite lines (OSLs) of the NH3_{3} (1,1) transition are each predicted to have equal intensities. However, hyperfine intensity anomalies (HIAs) are observed to be omnipresent in star formation regions, which is still not fully understood. In addressing this issue, we find that the computation method of the HIA by the ratio of the peak intensities may have defects, especially when being used to process the spectra with low velocity dispersions. Therefore we define the integrated HIAs of the ISLs (HIAIS_{\rm IS}) and OSLs (HIAOS_{\rm OS}) by the ratio of their redshifted to blueshifted integrated intensities and develop a procedure to calculate them. Based on this procedure, we present a systematic study of the integrated HIAs in the northern part of the Orion A MC. We find that integrated HIAIS_{\rm IS} and HIAOS_{\rm OS} are commonly present in the Orion A MC and no clear distinction is found at different locations of the MC. The medians of the integrated HIAIS_{\rm IS} and HIAOS_{\rm OS} are 0.921±\pm0.003 and 1.422±\pm0.009, respectively, which is consistent with the HIA core model and inconsistent with the CE model. Selecting those 170 positions where both integrated HIAs deviate by more than 3-σ\sigma from unity, most (166) are characterized by HIAIS_{\rm IS}1, which suggests that the HIA core model plays a more significant role than the CE model. The remaining four positions are consistent with the CE model. We compare the integrated HIAs with the para-NH3_{3} column density (NN(para-NH3_{3})), kinetic temperature (TKT_{\rm K}), total velocity dispersion (σv\sigma_{\rm v}), non-thermal velocity dispersion (σNT\sigma_{\rm NT}), and the total opacity of the NH3_{3} (1,1) line (τ0\tau_{0}). Their correlations can not be fully explained by neither the HIA core nor the CE model.Comment: 12 pages, 10 figures, accepted for publication in A&
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