Spin Configuration in the 1/3 Magnetization Plateau of Azurite Determined by NMR
| dc.creator | Aimo, F. | |
| dc.creator | Kramer, S. | |
| dc.creator | Klanjsek, M. | |
| dc.creator | Horvatic, M. | |
| dc.creator | Berthier, C. | |
| dc.creator | Kikuchi, H. | |
| dc.date | 2009-01-07 | |
| dc.date | 2009-02-25 | |
| dc.date.accessioned | 2026-07-07T12:59:26Z | |
| dc.date.available | 2026-07-07T12:59:26Z | |
| dc.description | High magnetic field $^{63,65}$Cu NMR spectra were used to determine the local spin polarization in the 1/3 magnetization plateau of azurite, Cu$_3$(CO$_3$)$_2$(OH)$_2$, which is a model system for the distorted diamond antiferromagnetic spin-1/2 chain. The spin part of the hyperfine field of the Cu2 (dimer) sites is found to be field independent, negative and strongly anisotropic, corresponding to $\approx$10 % of fully polarized spin in a $d$-orbital. This is close to the expected configuration of the "quantum" plateau, where a singlet state is stabilized on the dimer. However, the observed non-zero spin polarization points to some triplet admixture, induced by strong asymmetry of the diamond bonds $J_1$ and $J_3$. | |
| dc.description | Phys. Rev. Lett. 102, in press (2009) | |
| dc.identifier | https://arxiv.org/abs/0901.0859 | |
| dc.identifier | http://arxiv.org/abs/0901.0859 | |
| dc.identifier | Physical Review Letters 102 (2009) 127205 | |
| dc.identifier | doi:10.1103/PhysRevLett.102.127205 | |
| dc.identifier.uri | http://salesiana.dossiersoluciones.com/handle/123456789/225569 | |
| dc.subject | Strongly Correlated Electrons | |
| dc.title | Spin Configuration in the 1/3 Magnetization Plateau of Azurite Determined by NMR | |
| dc.type | text |