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Magnetic ordering in out-of-plane artificial spin systems based on the Archimedean lattices
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Artificial spin systems, sometimes referred to as artificial spin ices, are arrays of coupled nanoscale magnets that order according to the lattice geometry, nanomagnet shape and magnetic anisotropy. Here we characterize a family of artificial spin systems that are formed by placing arrays of out-of-plane nanomagnets on the vertices of the Archimedean lattices. On demagnetizing these nanomagnet arrays using a magnetic field protocol and subsequently imaging the magnetic configuration using magnetic force microscopy, we observe different types of magnetic order. We compare our experimental results with those predicted by Monte Carlo simulations to assign an effective temperature to each lattice. We find that, for all of the lattices, the assigned effective temperature is above the transition temperature. This reflects the difficulty of obtaining system-spanning order in lattices with out-of-plane nanomagnets. We consider to what extent further-neighbor interactions affect the phase diagram and spin-spin correlations in each lattice, illustrating our results with four example lattices. We can divide the lattices into three main categories: bipartite lattices that admit a perfect antiferromagnetic ground state, frustrated lattices where ordering proceeds via a single step, and frustrated lattices with two-step-ordering. Our work highlights the diversity of magnetic ordering that can be hosted in two-dimensional artificial spin systems with out-of-plane nanomagnets, and demonstrates the importance of including long-range interactions to explain the magnetic ordering. Such insights will be important for incorporating artificial spin systems into novel computing applications.
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Realizing Blume-Capel Degrees of Freedom with Toroidal Moments in a Ruby Artificial Spin Ice
A Ruby-lattice artificial spin ice realizes Blume-Capel degrees of freedom via toroidal moments on triangular and hexagonal plaquettes, with a two-step ordering into a ferrotoroidic ground state.
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