Crystal Growth and Physical Properties of Orthorhombic Kagome Lattice Magnets $R$Fe$_6$Ge$_6$ ($R$=Y, Tb, Dy)
Abhijeet Nayak, Sk Jamaluddin, Fan Wu, Emily Rapp, Resham Babu Regmi, Mohamed El Gazzah, Bence G. Márkus, László Forró, Madhav P. Ghimire, Allen Oliver, Kateryna Foyevtsova, Igor I. Mazin, Nirmal J. Ghimire
TL;DR
This study reports the growth and comprehensive characterization of orthorhombic Cmcm $R$Fe$_6$Ge$_6$ ($R$=Y,Tb,Dy) kagome magnets, unveiling a distorted Fe kagome network coupled to ordered $R$–Ge$_2$ chains. Fe moments order antiferromagnetically above ~400 K with ferromagnetic kagome planes, while Tb and Dy moments order at low temperatures with Tb exhibiting a single transition and Dy two transitions influenced by crystal-field effects; Y remains nonmagnetic in the $f$-subsystem. DFT calculations reveal a large $N(E_F)$ that drives Fe magnetism and a three-scale lattice-energy landscape controlling 1D chain disorder and in-plane chain alignment, suggesting a triangular Ising model description for the intraplanar ordering. The combination of structural distortions, high DOS at the Fermi level, and complex low-temperature magnetism makes this family a fertile platform for exploring the interplay between lattice geometry and electronic/magnetic properties, including potential Fermi-surface instabilities through chemical substitution.
Abstract
Kagome magnets represent a promising class of materials that exhibit intriguing electronic and magnetic properties, and they have recently garnered significant attention. While most kagome-lattice compounds are hexagonal, we report here single-crystal growth and physical property measurements of $R$Fe$_6$Ge$_6$ ($R$ = Y, Dy, Tb) compounds, which crystallize in an orthorhombic structure. The structure can be derived from a hexagonal prototype $R$Fe$_3$Ge$_2$ by replacing every other $R$ atom with a covalent Ge$_2$ dimer. Ordering of these dimers renders the structure orthorhombic, slightly distorts the kagome net, and makes the three Fe sites formally inequivalent. The iron and rare-earth sublattices order independently. Fe moments order above 400 K, forming ferromagnetic kagome planes stacked antiferromagnetically, while rare-earth moments order below 9 K. TbFe$_6$Ge$_6$ exhibits a single magnetic ordering transition associated with the Tb atoms, whereas DyFe$_6$Ge$_6$ shows two distinct magnetic phase transitions, strongly influenced by crystal electric field effects on the Dy$^{3+}$ ions. Density functional theory (DFT) calculations indicate that the ferromagnetic ordering of the Fe planes is driven by a high density of states at the Fermi energy. They also reveal three dramatically different structural energy scales: $R$ and Ge$_2$ form alternating 1D chains perpendicular to the kagome planes, and violating this alternation incurs a large energy cost. Aligning these chains is less costly, and achieving a two-dimensional order of anti-aligned chains requires very little energy. These compounds represent a unique class of materials, offering new opportunities to investigate the interplay between the distinct crystal lattice geometry and the underlying electronic and magnetic properties.
