[[abstract]]We report experimental evidence for the charge-orbital ordering in magnetite below the Verwey transition temperature TV. Measurements of O K-edge resonant x-ray scattering on magnetite reveal that the O 2p states in the vicinity of the Fermi level exhibit a charge-orbital ordering along the c axis with a spatial periodicity of the doubled lattice parameter of the undistorted cubic phase. Such a charge-orbital ordering vanishes abruptly above TV and exhibits a thermal hysteresis, correlating closely with the Verwey transition in magnetite.[[notice]]補正完畢[[incitationindex]]SCI[[booktype]]紙本[[booktype]]電子
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
To elucidate charge and orbital order below the Verwey transition temperature TV amp; 8764; 125 K, ...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
13 pagesInternational audienceWe propose a model for the Fe atomic displacements in the low-temperat...
13 pagesInternational audienceWe propose a model for the Fe atomic displacements in the low-temperat...
To elucidate charge and orbital order below the Verwey transition temperature TV∼125 K, a thin layer...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
To elucidate charge and orbital order below the Verwey transition temperature TV amp; 8764; 125 K, ...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital o...
13 pagesInternational audienceWe propose a model for the Fe atomic displacements in the low-temperat...
13 pagesInternational audienceWe propose a model for the Fe atomic displacements in the low-temperat...
To elucidate charge and orbital order below the Verwey transition temperature TV∼125 K, a thin layer...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
Magnetite, Fe3 O4, displays a highly complex low-temperature crystal structure that may be charge an...
To elucidate charge and orbital order below the Verwey transition temperature TV amp; 8764; 125 K, ...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...