Evidence for Antiferromagnetism in Cu3 (CO3)2 (OH)2

Abstract
We have used the proton resonance to study the magnetic behavior of the mineral azurite —Cu3 (CO3)2 (OH)2. Below 30°K the temperature dependence of the splitting of the proton resonance lines by the copper ions shows strong exchange effects. At 1.86°K a transition takes place and the resonance pattern below the transition indicates an antiferromagnetic state.

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