Magnetically-controlled Vortex Dynamics in a Ferromagnetic Superconductor
Ferromagnetic superconductors are exceptionally rare because the strong ferromagnetic exchange field usually destroys singlet superconductivity. EuFe$_2$(As$_{1-x}$P$_x$)$_2$, an iron-based superconductor with a maximum critical temperature of $\sim$25 K, is a unique material that exhibits full coex...
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Zusammenfassung: | Ferromagnetic superconductors are exceptionally rare because the strong
ferromagnetic exchange field usually destroys singlet superconductivity.
EuFe$_2$(As$_{1-x}$P$_x$)$_2$, an iron-based superconductor with a maximum
critical temperature of $\sim$25 K, is a unique material that exhibits full
coexistence with ferromagnetic order below $T_\mathrm{FM} \approx 19$ K. The
interplay between the two leads to a narrowing of ferromagnetic domains at
higher temperatures and the spontaneous nucleation of vortices/antivortices at
lower temperatures. Here we demonstrate how the underlying magnetic structure
directly controls the superconducting vortex dynamics in applied magnetic
fields. Just below $T_\mathrm{FM}$ we observe a pronounced
temperature-dependent peak in both the coercivity and the creep activation
energy, the latter becoming rapidly suppressed in large applied magnetic
fields. We attribute this behaviour to the formation of vortex polarons arising
from the unique interaction between free vortices and magnetic stripe domains.
We present a theoretical description of the properties of vortex polarons that
explains our main observations, showing how they lead to vortex trapping and an
attractive vortex-vortex interaction at short distances. In stark contrast,
strong magnetic irreversibility at low temperatures is linked to a critical
current governed by giant flux creep over an activation barrier for
vortex-antivortex annihilation near domain walls. Our work reveals unexplored
new routes for the magnetic enhancement of vortex pinning with particularly
important applications in high-current conductors for operation at high
magnetic fields. |
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DOI: | 10.48550/arxiv.2412.04098 |