Abstract

The magnetic and lattice properties of the SS=1/2 quantum-spin-chain ferromagnet, CuAs2_2O4_4, mineral name trippkeite, were investigated. The crystal structure of CuAs2_2O4_4 is characterized by the presence of corrugated CuO2_2 ribbon chains. Measurements of the magnetic susceptibility, heat capacity, electron paramagnetic resonance and Raman spectroscopy were performed. Our experiments conclusively show that a ferromagnetic transition occurs at ∼\sim7.4 K. Ab initio\textit{Ab initio} DFT calculations reveal dominant ferromagnetic nearest-neighbor and weaker antiferromagnetic next- nearest-neighbor spin exchange interactions along the ribbon chains. The ratio of JnnJ_{\rm nn}/JnnnJ_{\rm nnn} is near -4, placing CuAs2_2O4_4 in close proximity to a quantum critical point in the JnnJ_{\rm nn} - JnnnJ_{\rm nnn} phase diagram. TMRG simulations used to analyze the magnetic susceptibility confirm this ratio. Single-crystal magnetization measurements indicate that a magnetic anisotropy forces the Cu2+^{2+} spins to lie in an easy plane perpendicular to the cc-axis. An analysis of the field and temperature dependent magnetization by modified Arrott plots reveals a 3d-XY critical behavior. Lattice perturbations induced by quasi-hydrostatic pressure and temperature were mapped via magnetization and Raman spectroscopy.

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