The magnetic structure and field dependence of the cycloid phase mediating the spin reorientation transition in Ca3_3Ru2_2O7_7

preprint2022arXivOpen access

Abstract

We report a comprehensive experimental investigation of the magnetic structure of the cycloidal phase in Ca3_3Ru2_2O7_7, which mediates the spin reorientation transition, and establishes its magnetic phase diagram. In zero applied field, single-crystal neutron diffraction data confirms the scenario deduced from an earlier resonant x-ray scattering study: between 46.746.7~K <T<49.0< T < 49.0~K the magnetic moments form a cycloid in the a−ba-b plane with a propagation wavevector of (δ,0,1)(δ,0,1) with δ≃0.025δ\simeq 0.025 and an ordered moment of about 1 μBμ_{\rm{B}}, with the eccentricity of the cycloid evolving with temperature. In an applied magnetic field applied parallel to the bb-axis, the intensity of the (δ,0,1)(δ,0,1) satellite peaks decreases continuously up to about μ0H≃5μ_0 H \simeq 5 T, above which field the system becomes field polarised. Both the eccentricity of the cycloid and the wavevector increase with field, the latter suggesting an enhancement of the anti−-symmetric Dzyaloshinskii−-Moriya interaction via magnetostriction effects. Transitions between the various low-temperature magnetic phases have been carefully mapped out using magnetometry and resistivity. The resulting phase diagram reveals that the cycloid phase exists in a temperature window that expands rapidly with increasing field, before transitioning to a polarised paramagnetic state at 5 T. High-field magnetoresistance measurements show that below T≃70T\simeq 70 K the resistivity increases continuously with decreasing temperature, indicating the inherent insulating nature at low temperatures of our high-quality, untwinned, single-crystals. We discuss our results with reference to previous reports of the magnetic phase diagram of Ca3_3Ru2_2O7_7 that utilised samples which were more metallic and/or poly-domain.

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