International audienceThe subtle interplay among electronic degrees of freedom (charge and orbital orderings), spin and lattice distortion that conspire at the Verwey transition in magnetite (Fe3O4) is still a matter of controversy. Here, we provide compelling evidence that these electronic orderings are manifested as a continuous phase transition at the temperature where a spin reorientation takes place at around 130 K, i.e., well above T-V approximate to 121 K. The Verwey transition seems to leave the orbital ordering unaffected whereas the charge ordering development appears to be quenched at this temperature and the temperature dependence below T-V is controlled by the lattice distortions. Finally, we show that the orbital ordering does...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...
Paper presented at the 13th International Ceramics Congress (2014), held in Montecatini Terme (Italy...
Magnetite, $Fe_{3}O_{4}$, is the first magnetic material discovered and utilized by mankind in Ancie...
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...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
[[abstract]]We report experimental evidence for the charge-orbital ordering in magnetite below the V...
The crystal structure of highly stoichiometric magnetite (Fe3O4) below the Verwey transition has bee...
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 TV∼125 K, a thin layer...
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 TV amp; 8764; 125 K, ...
Understanding the driving mechanisms behind metal-insulator transitions (MITs) is a critical step to...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...
Paper presented at the 13th International Ceramics Congress (2014), held in Montecatini Terme (Italy...
Magnetite, $Fe_{3}O_{4}$, is the first magnetic material discovered and utilized by mankind in Ancie...
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...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
The thermal evolution of electronic order in the complex Verwey ground state of magnetite (Fe3O4) ha...
[[abstract]]We report experimental evidence for the charge-orbital ordering in magnetite below the V...
The crystal structure of highly stoichiometric magnetite (Fe3O4) below the Verwey transition has bee...
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 TV∼125 K, a thin layer...
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 TV amp; 8764; 125 K, ...
Understanding the driving mechanisms behind metal-insulator transitions (MITs) is a critical step to...
To elucidate charge and orbital order below the Verwey transition temperature T-V similar to 125 K, ...
Paper presented at the 13th International Ceramics Congress (2014), held in Montecatini Terme (Italy...
Magnetite, $Fe_{3}O_{4}$, is the first magnetic material discovered and utilized by mankind in Ancie...