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Charge ordering

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Through Phase transition, Oxide and Charge (physics)


This long range order phenomena was first discovered in magnetite (Fe3O4) by Verwey in 1939. He observed an increase of the electrical resistivity by two orders of magnitude at TCO=120K, suggesting a phase transition which is now well known as the Verwey transition. He was the first to propose the idea of an ordering process in this context. The charge ordered structure of magnetite was solved in 2011 by a group led by Paul Attfield with the results published in Nature. Periodic lattice distortions associated with charge order were later mapped in the manganite lattice to reveal striped domains containing topological disorder.

Theoretical description

The extended one-dimensional Hubbard model delivers a good description of the charge order transition with the on-site and nearest neighbor Coulomb repulsion U and V. It emerged that V is a crucial parameter and important for developing the charge order state. Further model calculations try to take the temperature and an interchain interaction into account. The extended Hubbard model for a single chain including inter-site and on-site interaction V and U as well as the parameter δd for a small dimerization which can be typically found in the (TMTTF)2X compounds is presented as follows:

H=−t∑i∑σ([1+(−1)iδd]ci,σ†ci+1,σ+h.c)+U∑ini,↑ni,↓+V∑ini,ni+1

where t describes the transfer integral or the kinetic energy of the electron and ci,σ† and ci+1,σ are the creation and annihilation operator, respectively, for an electron with the spin σ=↑,↓ at the ith or i+1th site. ni,↓,↑ denotes the density operator. For non-dimerized systems, δd can be set to zero Normally, the on-site Coulomb repulsion U stays unchanged only t and V can vary with pressure.

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