Intrinsic Gyrotropic Magnetic Current of Orbital Origin
Koushik Ghorai, Sankar Sarkar, Amit Agarwal
TL;DR
The paper addresses the origin of intrinsic gyrotropic magnetic currents (IGMC) in gyrotropic materials, emphasizing an orbital counterpart to the previously identified spin-driven magnetic displacement current. It develops a density-matrix formalism that couples both orbital minimal coupling and spin-Zeeman interactions, introducing the magnetic Berry connection polarizability (MBCP) and its orbital variant, which drive an intrinsic, Fermi-sea–driven GMC. The GMC is decomposed into Fermi-surface oscillations, dynamic charge polarization, and chiral magnetic velocity, with IGMC comprising the polarization and velocity channels; in ${\mathcal{PT}}$-symmetric CuMnAs, the CMV channel is symmetry-forbidden, making IGMC purely dispersion-driven and orbital-dominated. The study demonstrates that IGMC in CuMnAs is tunable via the Néel vector orientation and reverses sign with Néel-vector reversal, establishing IGMC as a direct probe of antiferromagnetic order and highlighting the dominant role of orbital mechanisms in gyrotropic responses. Overall, the work provides a unified, symmetry-aware framework linking orbital magnetism, Berry connection corrections, and gyrotropic transport with potential experimental observables such as measurable voltages in CuMnAs.
Abstract
In gyrotropic crystals, an oscillating magnetic field induces a charge response known as the gyrotropic magnetic current. While its conventional origin is attributed to magnetic field modified band energy and shift in the Fermi-surface, a recent study identified an additional spin-driven magnetic displacement contribution. Here, we complete the picture by identifying the orbital counterpart of the magnetic displacement current. Using a density-matrix formulation that incorporates both minimal coupling and spin-Zeeman interactions, we derive the electronic equations of motion in the presence of an oscillating magnetic field and uncover a previously unexplored orbital contribution to the wavepacket velocity. Physically, this contribution arises from the time variation of the magnetic-field induced charge polarization. In the low frequency transport regime, this mechanism becomes purely intrinsic. We illustrate this intrinsic gyrotropic current of orbital origin in the ${\cal P}{\cal T}$-symmetric antiferromagnet CuMnAs. We show that the intrinsic gyrotropic magnetic current reverses sign upon Néel vector reversal, establishing it as a direct probe of antiferromagnetic order in CuMnAs and other $\mathcal{PT}$-symmetric antiferromagnets.
