Takaya Mitsui
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Previous Organizations / Institutes
The organizations / institutes from the scholar's other articles in the past ten years
Research Subjects
Takaya Mitsui has a total of 89 co-authors. Here are the top co-authors by number of shared publications:
- Ryo Masuda
Graduate School of Science and Technology Hirosaki University Hirosaki Japan
12 shared publications Makoto Seto
National Institutes for Quantum Science and Technology , Sayo, Hyogo 679-5148
10 shared publications- Ko Mibu
Nagoya Institute of Technology
5 shared publications - Makoto Seto
Kyoto University
5 shared publications Yasuhiro Kobayashi
Institute for Integrated Radiation and Nuclear Science, Kyoto University, Kumatori, Osaka, Japan
5 shared publicationsNaohisa Hirao
Japan Synchrotron Radiation Research Institute, Sayo, Hyogo 679-5198, Japan
4 shared publications
Latest Publications
- 23 September 2026
- Published by AIP Publishing in Journal of Applied Physics
- Vol. 140 (12)
Quadrupole modulation in magnetic anisotropy in Fe3Si film on Pb(Mg1/3Nb2/3)O3–PbTiO3 under reversible strain
We investigate the microscopic origins of magnetic anisotropy in the ferromagnetic binary alloy Fe3Si film while applying reversible strain on a ferroelectric Pb(Mg,Nb)O3–PbTiO3 substrate. X-ray magnetic circular dichroism with the introduction of reversible strain clearly demonstrates the change in the magnetic easy axis direction, even with an anisotropy energy of 1.6 × 103 J/m3. The strain-dependent Mössbauer spectroscopy detects changes in the quadrupole shift, which are related to variations in the electric field gradient from the valence electron distribution. The density-functional-theory calculation also supports the electron quadrupole contribution to magnetic anisotropy. These results indicate that the strain-dependent changes in the magnetic easy axis in Fe3Si arise from the formation of the charge quadrupole at the strained Fe sites. This characteristic is notably different from that of the ferromagnetic Heusler alloy Co2FeSi, where one of the Fe sites in Fe3Si are replaced by Co. This study provides a significant approach to understanding and designing interfacial multiferroic materials.
- 23 September 2026
- Published by AIP Publishing in Journal of Applied Physics
- Vol. 140 (12)
Quadrupole modulation in magnetic anisotropy in Fe3Si film on Pb(Mg1/3Nb2/3)O3–PbTiO3 under reversible strain
We investigate the microscopic origins of magnetic anisotropy in the ferromagnetic binary alloy Fe3Si film while applying reversible strain on a ferroelectric Pb(Mg,Nb)O3–PbTiO3 substrate. X-ray magnetic circular dichroism with the introduction of reversible strain clearly demonstrates the change in the magnetic easy axis direction, even with an anisotropy energy of 1.6 × 103 J/m3. The strain-dependent Mössbauer spectroscopy detects changes in the quadrupole shift, which are related to variations in the electric field gradient from the valence electron distribution. The density-functional-theory calculation also supports the electron quadrupole contribution to magnetic anisotropy. These results indicate that the strain-dependent changes in the magnetic easy axis in Fe3Si arise from the formation of the charge quadrupole at the strained Fe sites. This characteristic is notably different from that of the ferromagnetic Heusler alloy Co2FeSi, where one of the Fe sites in Fe3Si are replaced by Co. This study provides a significant approach to understanding and designing interfacial multiferroic materials.
- Open Access
- 27 March 2025
- Published by Oxford University Press (OUP) in PNAS Nexus
- Vol. 4 (4) , pgaf060
Thermodynamic signatures of diagonal nematicity in RbFe2As2 superconductor
Electronic nematic states, characterized by broken rotational symmetry, are prevalent in correlated materials. In most iron-based superconductors, the nematic anisotropy aligns with the Fe–Fe direction of the iron square lattice. However, recent investigations propose a unique form of nematicity oriented along the diagonal Fe–As direction in heavily hole-doped AFe2As2 (A=Rb or Cs). Yet, the transport studies focusing on the fluctuations of such nematicity yield conflicting outcomes regarding the presence and orientation of the nematic fluctuations. Here, we report high-resolution heat capacity measurements conducted under in-plane field rotation in RbFe2As2. While no discernible anomaly associated with the nematic transition is found in the temperature dependence of specific heat, the field-angle dependence near the superconducting transition (at ∼2.8 K) reveals clear 2-fold oscillations within the plane, providing thermodynamic evidence for the presence of diagonal nematicity. Moreover, we find that Mössbauer spectroscopy sensitively probes the nematic transition at ∼50 K with no evidence of static magnetism. These findings imply that the diagonal nematicity in RbFe2As2 has a distinct mechanism involving charge degrees of freedom, exhibiting unusual thermodynamic properties of the transition.
- 27 March 2025
- Published by Oxford University Press (OUP) in PNAS Nexus
- Vol. 4 (4) , pgaf060
Open AccessThermodynamic signatures of diagonal nematicity in RbFe2As2 superconductor
Electronic nematic states, characterized by broken rotational symmetry, are prevalent in correlated materials. In most iron-based superconductors, the nematic anisotropy aligns with the Fe–Fe direction of the iron square lattice. However, recent investigations propose a unique form of nematicity oriented along the diagonal Fe–As direction in heavily hole-doped AFe2As2 (A=Rb or Cs). Yet, the transport studies focusing on the fluctuations of such nematicity yield conflicting outcomes regarding the presence and orientation of the nematic fluctuations. Here, we report high-resolution heat capacity measurements conducted under in-plane field rotation in RbFe2As2. While no discernible anomaly associated with the nematic transition is found in the temperature dependence of specific heat, the field-angle dependence near the superconducting transition (at ∼2.8 K) reveals clear 2-fold oscillations within the plane, providing thermodynamic evidence for the presence of diagonal nematicity. Moreover, we find that Mössbauer spectroscopy sensitively probes the nematic transition at ∼50 K with no evidence of static magnetism. These findings imply that the diagonal nematicity in RbFe2As2 has a distinct mechanism involving charge degrees of freedom, exhibiting unusual thermodynamic properties of the transition.
- 1 November 2024
- Published by Springer Nature in Interactions
- Vol. 245 (1) , 1-15
Synchrotron based conversion electron Mössbauer spectroscopy
- 1 November 2024
- Published by Springer Nature in Interactions
- Vol. 245 (1) , 1-15
Synchrotron based conversion electron Mössbauer spectroscopy
- Open Access
- 1 August 2024
- Published by IOP Publishing in Applied Physics Express
- Vol. 17 (8) , 082002
Three-dimensional surface analysis of iron-based materials using synchrotron Mössbauer source
A novel three-dimensional surface analysis system for iron-based solid materials has been developed. This system is composed of a synchrotron Mössbauer source, an X-ray focusing device, a precision stage, a gas flow proportional counter for conversion electron measurements, and multiple multichannel scalers. The performance was evidenced by determining the spatial distribution of the iron oxide abundance on a laser-ablated iron foil surface. This system can be widely utilized as a powerful analytical tool in steel science for corrosion, welding, and laser surface modification.
- 1 August 2024
- Published by IOP Publishing in Applied Physics Express
- Vol. 17 (8) , 082002
Open AccessThree-dimensional surface analysis of iron-based materials using synchrotron Mössbauer source
A novel three-dimensional surface analysis system for iron-based solid materials has been developed. This system is composed of a synchrotron Mössbauer source, an X-ray focusing device, a precision stage, a gas flow proportional counter for conversion electron measurements, and multiple multichannel scalers. The performance was evidenced by determining the spatial distribution of the iron oxide abundance on a laser-ablated iron foil surface. This system can be widely utilized as a powerful analytical tool in steel science for corrosion, welding, and laser surface modification.
- 15 April 2023
- Published by Physical Society of Japan in Journal of the Physical Society of Japan
- Vol. 92 (4)
Magnetic Spin-Flop Transition of ε-FeOOH at 8 GPa
- 15 April 2023
- Published by Physical Society of Japan in Journal of the Physical Society of Japan
- Vol. 92 (4)
Magnetic Spin-Flop Transition of ε-FeOOH at 8 GPa
- 16 May 2022
- Published by Elsevier in Journal of Magnetism and Magnetic Materials
- Vol. 557
Study on FeCr thin film for a spintronic material with negative spin polarization
- 16 May 2022
- Published by Elsevier in Journal of Magnetism and Magnetic Materials
- Vol. 557
Study on FeCr thin film for a spintronic material with negative spin polarization
- 19 November 2021
- Published by Springer Nature in Hyperfine Interactions
- Vol. 242 (1) , 1-15
Direct observation of magnetic Friedel oscillation at Fe(001) surface
- 19 November 2021
- Published by Springer Nature in Hyperfine Interactions
- Vol. 242 (1) , 1-15
Direct observation of magnetic Friedel oscillation at Fe(001) surface
- 12 May 2021
- Published by American Physical Society (APS) in Physical Review B
- Vol. 103 (17) , 174108
Synchrotron Mössbauer spectroscopic and x-ray diffraction study of ferropericlase in the high-pressure range of the lower mantle region
Systematic change of structural transition and high-spin (HS) to low-spin (LS) transition of in synthetic -ferropericlase for pressures up to that of the lower mantle region were investigated using synchrotron x-ray diffraction (XRD) and synchrotron Mössbauer spectroscopic methods. The XRD patterns and the Mössbauer spectra were measured up to 160 GPa at room temperature. The results of the synchrotron XRD analysis indicate that the cubic structure of -ferropericlase is maintained up to 160 GPa. The Mössbauer spectra at 19.8 and 24.0 GPa consist of three doublets assigned to HS at the octahedral site. At pressures from 61 to 136 GPa, a singlet assigned to LS is added to the three HS doublets, and its area ratio with respect to the HS doublets gradually increase with increasing pressure. At pressures above 136 GPa, the Mössbauer spectra consist of only an LS singlet, implying that all Fe at these pressures is in a LS state. The resulting spin crossover pressure interval from 61 to 136 GPa indicates the coexistence of both HS and LS at pressure conditions from the upper part to the bottom of the lower mantle.- 12 May 2021
- Published by American Physical Society (APS) in Physical Review B
- Vol. 103 (17) , 174108
Synchrotron Mössbauer spectroscopic and x-ray diffraction study of ferropericlase in the high-pressure range of the lower mantle region
Systematic change of structural transition and high-spin (HS) to low-spin (LS) transition of in synthetic -ferropericlase for pressures up to that of the lower mantle region were investigated using synchrotron x-ray diffraction (XRD) and synchrotron Mössbauer spectroscopic methods. The XRD patterns and the Mössbauer spectra were measured up to 160 GPa at room temperature. The results of the synchrotron XRD analysis indicate that the cubic structure of -ferropericlase is maintained up to 160 GPa. The Mössbauer spectra at 19.8 and 24.0 GPa consist of three doublets assigned to HS at the octahedral site. At pressures from 61 to 136 GPa, a singlet assigned to LS is added to the three HS doublets, and its area ratio with respect to the HS doublets gradually increase with increasing pressure. At pressures above 136 GPa, the Mössbauer spectra consist of only an LS singlet, implying that all Fe at these pressures is in a LS state. The resulting spin crossover pressure interval from 61 to 136 GPa indicates the coexistence of both HS and LS at pressure conditions from the upper part to the bottom of the lower mantle.- 29 March 2021
- Published by American Physical Society (APS) in Physical Review B
- Vol. 103 (10) , 104435
Perpendicular magnetic anisotropy at the Fe/Au(111) interface studied by Mössbauer, x-ray absorption, and photoemission spectroscopies
The origin of the interfacial perpendicular magnetic anisotropy (PMA) induced in the ultrathin Fe layer on the Au(111) surface was examined using synchrotron-radiation-based Mössbauer spectroscopy (MS), x-ray magnetic circular dichroism (XMCD), and angle-resolved photoemission spectroscopy (ARPES). To probe the detailed interfacial electronic structure of orbital hybridization between the Fe and Au bands, we detected the interfacial proximity effect, which modulates the valence-band electronic structure of Fe, resulting in PMA. MS and XMCD measurements were used to detect the interfacial magnetic structure and anisotropy in orbital magnetic moments, respectively. In situ ARPES also confirms the initial growth of Fe on large spin-orbit coupled surface Shockley states under Au(111) modulated electronic states in the vicinity of the Fermi level. This suggests that PMA in the Fe/Au(111) interface originates from the cooperation effects among the spin, orbital magnetic moments in Fe, and large spin-orbit coupling in Au. These findings pave the way to develop interfacial PMA using hybridization with a large spin-orbit interaction.- 29 March 2021
- Published by American Physical Society (APS) in Physical Review B
- Vol. 103 (10) , 104435
Perpendicular magnetic anisotropy at the Fe/Au(111) interface studied by Mössbauer, x-ray absorption, and photoemission spectroscopies
The origin of the interfacial perpendicular magnetic anisotropy (PMA) induced in the ultrathin Fe layer on the Au(111) surface was examined using synchrotron-radiation-based Mössbauer spectroscopy (MS), x-ray magnetic circular dichroism (XMCD), and angle-resolved photoemission spectroscopy (ARPES). To probe the detailed interfacial electronic structure of orbital hybridization between the Fe and Au bands, we detected the interfacial proximity effect, which modulates the valence-band electronic structure of Fe, resulting in PMA. MS and XMCD measurements were used to detect the interfacial magnetic structure and anisotropy in orbital magnetic moments, respectively. In situ ARPES also confirms the initial growth of Fe on large spin-orbit coupled surface Shockley states under Au(111) modulated electronic states in the vicinity of the Fermi level. This suggests that PMA in the Fe/Au(111) interface originates from the cooperation effects among the spin, orbital magnetic moments in Fe, and large spin-orbit coupling in Au. These findings pave the way to develop interfacial PMA using hybridization with a large spin-orbit interaction.- 3 December 2020
- Published by American Physical Society (APS) in Physical Review Letters
- Vol. 125 (23) , 236806
Magnetic Friedel Oscillation at the Fe(001) Surface: Direct Observation by Atomic-Layer-Resolved Synchrotron Radiation Mössbauer SpectroscopyThe surface magnetism of Fe(001) was studied in an atomic layer-by-layer fashion by using the in situ iron-57 probe layer method with a synchrotron Mössbauer source. The observed internal hyperfine field exhibits a marked decrease at the surface and an oscillatory behavior with increasing depth in the individual upper four layers below the surface. The calculated layer-depth dependencies of the effective hyperfine field , isomer shift , and quadrupole shift agree well with the observed experimental parameters. These results provide the first experimental evidence for the magnetic Friedel oscillations, which penetrate several layers from the Fe(001) surface.- 3 December 2020
- Published by American Physical Society (APS) in Physical Review Letters
- Vol. 125 (23) , 236806
Magnetic Friedel Oscillation at the Fe(001) Surface: Direct Observation by Atomic-Layer-Resolved Synchrotron Radiation Mössbauer SpectroscopyThe surface magnetism of Fe(001) was studied in an atomic layer-by-layer fashion by using the in situ iron-57 probe layer method with a synchrotron Mössbauer source. The observed internal hyperfine field exhibits a marked decrease at the surface and an oscillatory behavior with increasing depth in the individual upper four layers below the surface. The calculated layer-depth dependencies of the effective hyperfine field , isomer shift , and quadrupole shift agree well with the observed experimental parameters. These results provide the first experimental evidence for the magnetic Friedel oscillations, which penetrate several layers from the Fe(001) surface.