Exotic Magnetic Field-Induced Spin-Superstructures in a Mixed Honeycomb-Triangular Lattice System

V. Ovidiu Garlea, Liurukara D. Sanjeewa, Michael A. McGuire, Cristian D. Batista, Anjana M. Samarakoon, David Graf, Barry Winn, Feng Ye, Christina Hoffmann, Joseph W. Kolis

Research output: Contribution to journalArticlepeer-review

20 Scopus citations

Abstract

The temperature-magnetic field phase diagram of the mixed honeycomb-triangular lattice system K2Mn3(VO4)2CO3 is investigated by means of magnetization, heat-capacity, and neutron-scattering measurements. The results indicate that triangular and honeycomb magnetic layers undergo sequential magnetic orderings and act as nearly independent magnetic sublattices. The honeycomb sublattice orders at about 85 K in a Neél-type antiferromagnetic structure, while the triangular sublattice displays two consecutive ordered states at much lower temperatures, 3 and 2.2 K. The ground state of the triangular sublattice consists of a planar "Y" magnetic structure that emerges from an intermediate collinear "up-up-down" state. Applied magnetic fields parallel or perpendicular to the c axis induce exotic ordered phases characterized by various spin-stacking sequences of triangular layers that yield bilayer, three-layer, or four-layer magnetic superstructures. The observed superstructures cannot be explained in the framework of quasiclassical theory based only on nearest-neighbor interlayer coupling and point towards the presence of effective second-nearest-neighbor interactions mediated by fluctuations of the magnetic moments in the honeycomb sublattice.

Original languageEnglish
Article number011038
JournalPhysical Review X
Volume9
Issue number1
DOIs
StatePublished - Feb 26 2019

Funding

FundersFunder number
Directorate for Mathematical and Physical Sciences1157490, 1410727

    Fingerprint

    Dive into the research topics of 'Exotic Magnetic Field-Induced Spin-Superstructures in a Mixed Honeycomb-Triangular Lattice System'. Together they form a unique fingerprint.

    Cite this