In-plane orbital magnetization as a probe for symmetry breaking in strained twisted bilayer graphene
Ohad Antebi, Ady Stern, and Erez Berg

TL;DR
This paper demonstrates that in-plane orbital magnetization can effectively detect symmetry breaking in strained twisted bilayer graphene, revealing large magnetization signals in valley-polarized states due to symmetry violations.
Contribution
It introduces in-plane orbital magnetization as a sensitive probe for symmetry breaking in strained twisted bilayer graphene, highlighting large magnetization values linked to valley polarization.
Findings
Large in-plane orbital magnetization signals occur in valley-polarized states.
Symmetry breaking due to strain enhances magnetization, detectable at small heterostrain.
Magnetization magnitude reflects the Dirac velocity of single-layer graphene.
Abstract
Three symmetries prevent a twisted bilayer of graphene from developing an in-plane spontaneous magnetization in the absence of a magnetic field - time reversal symmetry, symmetry to rotation and symmetry to rotation. In contrast, there are experimental and theoretical indications that, at certain electron densities, time reversal and symmetries are broken spontaneously, while the symmetry is often broken due to strain. We show that in-plane orbital magnetization is a very sensitive probe to the simultaneous breaking of these three symmetries, exhibiting surprisingly large values (of the order of one Bohr magneton per moir\'{e} unit cell) for valley polarized states at rather small values of heterostrain. We attribute these large values to the large magnitude of the characteristic magnetization of individual Bloch states, which we find to reflect…
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