Abstract

The high-field magnetic properties and magnetic order of the gem mineral green dioptase Cu6[_6[Si6_6O18]⋅6_{18}]\cdot 6H2_2O have been studied by means of single-crystal neutron diffraction in magnetic fields up to 21 21~T and magnetization measurements up to 30 30~T. In zero field, the Cu2+^{2+}-moments in the antiferromagnetic chains are oriented along the cc-axis with a small off-axis tilt. For a field applied parallel to the cc-axis, the magnetization shows a spin-flop-like transition at B∗=12.2 B^*=12.2~T at 1.5 1.5~K. Neutron diffraction experiments show a smooth behavior in the intensities of the magnetic reflections without any change in the periodicity of the magnetic structure. Bulk and microscopic observations are well described by a model of ferromagnetically coupled antiferromagnetic XXZXXZ spin-12\frac{1}{2} chains, taking into account a change of the local easy-axis direction. We demonstrate that the magnetic structure evolves smoothly from a deformed Néel state at low fields to a deformed spin-flop state in a high field via a strong crossover around B∗B^*. The results are generalized for different values of interchain coupling and spin anisotropy.

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