Dr. Alaska Subedi(CNRS, France)
April 11(Thu) - April 11(Thu), 2019
15:00
Seminar Room #201, Science building #3
Rare-earth nickelates RNiO3 exhibit a unique phase diagram where a metal-insulator transition is accompanied by structural and magnetic transitions. It has experimentally been established that all rare-earth nickelates except LaNiO3 are metallic paramagnets with an orthorhombic structure at high temperatures. At low temperature,the metal-insulator and an orthorhombic to monoclinic structural transitions occur simultaneously. The transition temperature can be lowered by increasing the size of the rare-earth ion, and it approaches zero for LaNiO3. I will present a theory to describe the structural, electronic and magnetic transitions in these materials and discuss how LaNiO3 differs from the rest of the members of the family.