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Giant and anisotropic magnetostriction in $β$-O$_{2}$ at 110 T

Published 14 Apr 2025 in cond-mat.str-el, cond-mat.mtrl-sci, and cond-mat.soft | (2504.10085v1)

Abstract: Magnetostriction is a crystal's deformation under magnetic fields, usually in the range of $10{-6}$ - $10{-3}$, where the lattice change occurs with the change of spin and orbital state through spin-lattice couplings. In strong magnetic fields beyond 100 T, the significant Zeeman energy competes with the lattice interactions, where one can expect considerable magnetostriction. However, directly observing magnetostriction above 100 T is challenging, because generating magnetic fields beyond 100 T accompanies the destruction of the coil with a single-shot $\mu$-second pulse. Here, we observed the giant and anisotropic magnetostriction of $\sim$1 % at 110 T in the spin-controlled crystal of $\beta$-O${2}$, by combining the single-shot diffraction of x-ray free-electron laser (XFEL) and the state-of-the-art portable 100 T generator. The magnetostriction of $\sim$1 % is the largest class as a deformation of the unit cell. It is a response of the soft lattice of $\beta$-O${2}$ originating, not only in the competing van der Waals force and exchange interaction, but also the soft state of spin and lattice frustrated on the triangular network. Meanwhile, the anisotropy originates from the strong two-dimensionality of the spin system. Giant magnetostriction in crystals should become more ubiquitous and diverse beyond 100 T, where our XFEL experiment above 100 T opens a novel pathway for their exploration, providing fundamental insights into the roles of spin in stabilizing crystal structures.

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