Abstract
By using the first-principles electronic and magnetic structure calculations for the iron pnictides EuFeAs and EuFeP, we find that the ground state of EuFeAs is a collinear antiferromagnetic (AFM) order in the Fe layer and an A-type AFM order with Eu spin lying in the basal plane (along 110), while for EuFeP the Fe ions do not carry local moment but the Eu ones order ferromagnetically pointing along the axis (along 001), which are in good agreement with experiments. We further find that the magnetic order in Fe layer is closely related to the Fe-As-Fe bond angle. When the Fe-As-Fe bond angle decreases to a small value, the system favors ferromagnetic order.
- Received 18 August 2012
DOI:https://doi.org/10.1103/PhysRevB.86.155119
©2012 American Physical Society