Abstract
We present a combined experimental and theoretical study of the mineral atacamite . Density-functional theory yields a Hamiltonian describing anisotropic sawtooth chains with weak 3D connections. Experimentally, we fully characterize the antiferromagnetically ordered state. Magnetic order shows a complex evolution with the magnetic field, while, starting at 31.5 T, we observe a plateaulike magnetization at about . Based on complementary theoretical approaches, we show that the latter is unrelated to the known magnetization plateau of a sawtooth chain. Instead, we provide evidence that the magnetization process in atacamite is a field-driven canting of a 3D network of weakly coupled sawtooth chains that form giant moments.
- Received 19 April 2019
- Revised 25 March 2021
- Accepted 30 March 2021
DOI:https://doi.org/10.1103/PhysRevLett.126.207201
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