Origin of the classical magnetization discontinuities of the dodecahedron
Abstract
The classical antiferromagnetic Heisenberg model on the dodecahedron has been shown to have three magnetization discontinuities in an external field. Here it is shown that the highest-field discontinuity can be directly traced back to the strong magnetization jump leading to saturation at the Ising limit, which originates from the magnetic response of an isolated pentagon and the frustrated connectivity of the dodecahedron. This discontinuity survives up to the limit and disappears shortly before the ferromagnetic Ising interaction fully polarizes the spins. The two lower-field jumps of the model result from the competition of discontinuities that emerge from the magnetization plateau surviving away from the Ising limit.
Keywords
Cite
@article{arxiv.2311.17205,
title = {Origin of the classical magnetization discontinuities of the dodecahedron},
author = {N. P. Konstantinidis},
journal= {arXiv preprint arXiv:2311.17205},
year = {2025}
}
Comments
9 pages, 16 figures