Orbital Magnetic Quadrupole Moment
- Orbital magnetic quadrupole moment is a rank-2 magnetic multipole defined by the second spatial moment of orbital currents, crucial for understanding magnetic field gradient responses.
- Its formulations range from gauge-covariant bulk theories and Berry-phase methods to boundary manifestations in higher-order topological phases, highlighting diverse computational and experimental approaches.
- Material estimates and response theories reveal that the MQM underpins key effects such as magnetoelectric and gravito-magnetoelectric responses, thus playing a critical role in modern condensed matter physics.
Orbital magnetic quadrupole moment (MQM) is the rank-2 magnetic multipole associated with the second spatial moment of orbital current distributions and, in periodic crystals, with the response of the local free-energy density to a magnetic-field gradient. In the contemporary literature it appears under the notations , , and , and more than one normalization convention is used. The concept has acquired several distinct but connected formulations: a gauge-invariant bulk theory for Bloch bands, a boundary-based characterization in higher-order topological phases, and response-theoretic roles in magnetoelectric, gravito-magnetoelectric, and nonlinear anomalous thermoelectric phenomena (Shitade et al., 2018, Gao et al., 2018, Gliozzi et al., 2022, Shinada et al., 2023).
1. Classical tensor and thermodynamic definition
For a finite current distribution , the magnetic quadrupole tensor is written in the cited literature in two closely related forms. One convention uses
while another uses
The coexistence of these expressions indicates that notation and normalization vary across subliteratures (Gao et al., 2018, Gliozzi et al., 2022).
As with the electric quadrupole, origin independence requires the net dipole to vanish. In the higher-order-topology formulation this appears as the condition that the net magnetic dipole
vanish, while in the crystalline-response formulation the same issue motivates abandoning direct use of the position operator in favor of a thermodynamic definition (Gliozzi et al., 2022).
In periodic crystals the position operator is ill-defined in the Bloch basis, so the orbital MQM is defined as a response of the local free-energy density to a weak, spatially inhomogeneous magnetic field. One formulation introduces
and another writes the local gradient expansion
In this sense the MQM is the coefficient conjugate to the first spatial derivative of the magnetic field rather than to the field itself (Gao et al., 2018, Shinada et al., 2023).
A complementary wave-packet interpretation is also available. In the Berry-phase framework,
where 0 is the packet center and 1 is the orbital angular-momentum operator. The fully gauge-invariant evaluation of this second moment reproduces the Brillouin-zone expression for 2 (Shinada et al., 2023).
2. Microscopic formulations in periodic Bloch bands
A fully gauge-invariant quantum-mechanical formula for the orbital MQM in crystalline solids was derived by gauge-covariant gradient expansion. In that construction one starts from the two-point Keldysh Green’s function with a Wilson line, rewrites the Dyson equation with the gauge-covariant Moyal product, expands in gradients of the electromagnetic field, and identifies the coefficient of 3 in the thermodynamic potential. The resulting tensor is
4
with the kernels 5, 6, and 7 defined by interband-projector matrix elements of Bloch derivatives and the Hamiltonian. The first term is a Fermi-sea itinerant contribution, while the second and third are local contributions. The formula is stated to hold for insulators and metals, and at zero and finite temperature (Shitade et al., 2018).
A complementary Bloch-band expression emphasizes explicitly geometric objects. Summing over occupied bands 8, one obtains a gauge-invariant formula in which 9 contains three types of terms: an interband term proportional to 0, a Hessian term involving 1, and a metric term involving 2. Here 3 is the Berry connection, 4 the interband orbital moment, 5 the band-energy Hessian, and 6 the quantum metric. The same work also gives an equivalent compact “interband-Berry-velocity” form, with the metric and Hessian pieces required for full gauge invariance under 7 (Gao et al., 2018).
The Berry-phase formulation of the uniform tensor 8 in metals and insulators likewise yields a Brillouin-zone integral built from the Berry connection 9, the quantum metric 0, the interband orbital object 1, the Fermi function 2, and the grand-potential density 3. In this form, the MQM is not a purely Fermi-surface quantity: it contains both occupation and grand-potential pieces, and the latter are essential for thermodynamic consistency (Shinada et al., 2023).
These formulations collectively establish the orbital MQM as a bona fide bulk quantity of band theory, albeit one whose implementation depends strongly on whether the physical problem is a generic periodic crystal or a higher-order topological phase.
3. Boundary manifestation in higher-order topological phases
In three-dimensional higher-order topological phases, the diagonal components of the MQM manifest as surface-localized magnetization and hinge currents. For an orthorhombic crystal with vanishing bulk magnetization 4, a nonzero bulk 5 produces a surface magnetization density on a face 6 with outward normal 7,
8
and a hinge current on the intersection of faces 9,
0
This boundary description is the direct magnetic analogue of the way an electric quadrupole produces boundary charge structure (Gliozzi et al., 2022).
A central point is that the hinge current is generally not equal to the difference of surface magnetizations that intersect at the hinge. The mismatch is precisely quantified by the bulk MQM. In practice, one may glue arbitrary surface layers, such as 2D Chern insulators, which contribute extra surface magnetizations 1 and hinge currents 2 satisfying the Ampère law
3
Appropriate combinations of 4 and 5 then cancel the decoration-dependent pieces and isolate the bulk quadrupole contribution (Gliozzi et al., 2022).
The resulting bulk-sensitive quantities are the three independent quadrupole differences
6
7
8
Each 9 is invariant under any surface decoration with zero net 0, and therefore functions as a bulk characterization of the higher-order phase (Gliozzi et al., 2022).
A microscopic computation of the required surface magnetizations uses slab geometry. For a slab infinite in 1 but finite in 2, the layer-resolved magnetization is
3
with
4
and 5 the projector onto sites in layer 6. The surface magnetization on the 7 face is then
8
Analogous formulas apply to 9- and 0-slabs (Gliozzi et al., 2022).
Within this framework, the MQM can distinguish phases in some intrinsic and boundary-obstructed higher-order topological insulators. The formalism also shows that a fully bulk formula valid for higher-order phases remains an open question, so the boundary-based construction is not merely calculational convenience but part of the present conceptual structure of the subject (Gliozzi et al., 2022).
4. Relation to magnetoelectric and gravito-magnetoelectric response
One of the main outcomes of the modern theory is that the orbital MQM is directly tied to magnetoelectric (ME) response. In a zero-temperature insulator, the gauge-covariant theory gives the Maxwell relation
1
and the band-theory approach gives the equivalent statement
2
Thus the MQM is identified as the microscopic origin of the linear ME effect in insulating crystals (Shitade et al., 2018, Gao et al., 2018).
The same connection acquires a thermal analogue in the orbital gravito-magnetoelectric effect (OGME), where a temperature gradient induces orbital magnetization according to
3
A naive Kubo treatment based only on the current–energy–density correlator leads to
4
but this expression diverges like 5 at low temperature. The correction is supplied by the equilibrium magnetization current arising from 6 in the perturbed Hamiltonian, which injects precisely the magnetic-quadrupole term 7. The full intrinsic response is
8
Once this correction is included, the 9 divergences cancel, and the intrinsic OGME acquires a finite entropy-density representation (Shinada et al., 2023).
The same analysis proves the Mott relation. With the zero-temperature intrinsic orbital ME tensor written as
0
the intrinsic OGME satisfies
1
and therefore, at low temperature,
2
An analogous Mott relation holds for the extrinsic OGME and extrinsic OME (Shinada et al., 2023).
This response-theoretic role corrects a common misconception that the Kubo formula alone captures the intrinsic thermal magnetoelectric response. In the cited analysis, the MQM is the missing bulk correction required both to eliminate an unphysical zero-temperature divergence and to recover the correct thermodynamic relation (Shinada et al., 2023).
5. Symmetry structure, quantization, and representative models
The orbital MQM transforms as a rank-2 pseudotensor. In the Bloch-band formulation, under time reversal 3 one has 4, 5, and 6, implying 7; under inversion 8, 9 flips 0 while leaving 1 axial, again giving 2. Hence 3 is even under combined 4, and only states that break 5 and 6 separately but preserve 7 can host a nonzero quadrupole. For any group containing 8 or 9 separately, 0 (Gao et al., 2018).
Magnetic-point-group constraints for the OGME sharpen this classification. In any pure 1-symmetric group the extrinsic response vanishes because 2, while the intrinsic response can remain nonzero. In any group with full 3, only the extrinsic response survives and the intrinsic one is forbidden. A subset of groups, including 4 and 5, allows a monopole (Chern–Simons) term, so that 6; in all others 7 (Shinada et al., 2023).
In higher-order topology, derivatives of the bulk quadrupole differences define quantized invariants
8
Along a given hinge, 9 counts net chiral hinge modes. On a gapped surface, 00 is the half-integer magneto-electric polarizability. Consequently, 01 whenever surfaces and hinges are gapped and the bulk 02 can be fractional. For a 03-protected intrinsic chiral HOTI, the individual slopes satisfy
04
so that 05; numerically, 06 reproduces the usual 07 invariant. For a boundary-obstructed HOTI with all three surfaces gapped by two-fold rotations, numerics give 08 (Gliozzi et al., 2022).
Several model systems illustrate these symmetry principles. In a minimal two-band tilted Dirac-cone model,
09
only 10 survives because mirror-11 symmetry forces 12 while the 13 tilt breaks mirror-14. At 15 and 16,
17
so 18 jumps as 19 crosses the Dirac point, and a finite gap smooths the jump (Gao et al., 2018).
In the 20-symmetric three-orbital CuO21 loop-current model,
22
the magnetic point group is 23, so only 24 and 25 survive. Numerically, 26 at low 27 shows sharp peaks at each Dirac-point energy 28, and 29 at fixed 30 is strictly proportional to 31 for 32, in accord with the Mott law (Shinada et al., 2023).
A related multipolar-ordering literature treats the magnetic quadrupole as a rank-2, time-reversal-odd, axial tensor with five independent components and shows that spontaneous odd-parity magnetic quadrupole order in a three-orbital system produces antisymmetric spin-orbital polarization in momentum space, or spin-orbital momentum locking. Under 33 these components transform as 34, 35, 36, and 37. This establishes a symmetry bridge between quadrupolar order, momentum-space textures, and cross-correlated responses such as the magnetoelectric effect and current-induced distortion (Hayami et al., 2021).
6. Computation, material estimates, and open issues
For higher-order topological phases, the practical computation of the MQM proceeds under explicit assumptions. Zero bulk magnetization is enforced by requiring 38 so that 39. Surfaces must be gapped, or gapped by benign decorations, so that 40 is well-defined. Hinges must carry well-localized currents, and conservation together with 41 symmetry ensures that parallel hinges have equal current. The Bloch gauge must be smooth in the two-dimensional Brillouin zone of the slab. One then computes layer-resolved 42 in a large slab, integrates half the slab to obtain 43, computes hinge currents 44 in a geometry with two open directions, combines them through the quadrupole differences 45, and numerically differentiates with respect to 46 to extract 47 (Gliozzi et al., 2022).
In crystalline antiferromagnets, the gauge-covariant theory yields concrete material estimates for the orbital part of the magnetoelectric susceptibility. For BaMn48As49, focusing on the nonzero diagonal component in the AFM-ordered state with 50, one finds
51
while the spin contribution is
52
For CeMn53Ge54Si55 with 56, the estimates include
57
and
58
These values support the statement that the orbital contribution can be comparable with, or even dominant over, the spin contribution (Shitade et al., 2018).
For the thermal response problem, possible detection routes have been proposed rather than established. In the loop-current context, experimental detection might proceed by torque-magnetometry in a well-controlled 59 field, or by ultrafast pump-probe schemes that effectively create transient 60’s and then read off 61. Since 62 couples to 63, one may also envisage applying small inhomogeneous magnetic fields and measuring the ensuing orbital polarization. These suggestions are consistent with the response definition but remain proposals in the cited discussion (Shinada et al., 2023).
Two conceptual boundaries of the present theory are explicit. First, in higher-order topological phases a fully bulk formula valid for higher-order phases remains an open question, so boundary signatures continue to play a defining role. Second, the various formulations emphasize different physical regimes: Bloch-band thermodynamics for periodic crystals, boundary reconstruction for higher-order topology, and correlation-function corrections for thermal responses. A plausible implication is that the orbital MQM is best viewed not as a single computational object but as a unifying multipolar response concept whose precise representation depends on which aspect of orbital magnetism is physically accessible.