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M. V. Krasinkova

Publications and source records attributed to M. V. Krasinkova.

2 recordsLinked to original sources

Highly Correlated Electron State and High-Temperature Superconductivity in Iron Pnictides

It is shown that the qualitative model of the high-temperature superconductivity suggested earlier for cuprates and doped picene and based on the idea that the valence electron state depends on the character of the chemical bonds they form and on the Coulomb interaction between the electrons is not only confirmed by the experimental data on iron pnictides but is also improved. From the chemical point of view, the high-temperature superconductivity is associated with additional $π$ bonding along chains of covalently bonded ions via a delocalized $π$ orbital, just like in cuprates. From the physical point of view, as the data on iron pnictides show, the superconductivity is associated with a FeAs layer transition into the state similar to a macroscopic quantum system characterized by a highly correlated electron state, formation of two-dimensional crystals of electron pairs with quantized energy levels, and a strong Coulomb interaction between these crystals. Superconductivity in such a system is accomplished by a two-dimensional Wigner crystal consisting of one-dimensional Wigner crystals formed by bosons, i.e., singlet electron pairs that are in the same quasi-one-dimensional state extending along the ion chain, which corresponds to a delocalized $π$ orbital in chemistry. The model applicability to three different classes of materials (cuprates, picene, iron pnictides) indicates that it can prove useful for development of the theory of superconductivity taking into consideraion the highly correlated state of valence electrons and strong Coulomb interactions between the electrons.

cond-mat.supr-con↗

On the Role of Exchange Interaction in Magnetic Ordering and Conductivity of Manganites

A model of chemical bonding between ions in manganites involving covalent one-electron $σ$ bonding is suggested. The covalent one-electron $σ$ bonding gives rise to a strongly correlated state of electrons resulting from the exchange interaction between electrons when they are simultaneously at cation and anion orbitals. The manifestation of the correlatred state is the spin and spatial ordering of the electrons resulting in the formation of a spin- ordered electron lattice. The conductivity of manganites in this model is the consequence of displacement of the electron lattice (or its part) from one localization site to another and depends on the type of spin ordering of the electrons in the electron lattice and the localization energy determined by the energy of the one-electron $σ$ bond. The model also assumes a strong polarization of an anion by cations, which facilitates the 3s2p hybridization of the anion and transition of one of the pairs of 2p electrons from the singlet state into the triplet state. This transition leads to formation of the spin-polarized electron lattice (electron spins are parallel) and ferromagnetic ordering of manganese ions. In the model, the effect of colossal magnetoresistance is explained by a change of the conductivity mechanism on application of an external magnetic field, i.e., transition from the conductivity mechnism typical of an ionic crystal to the conductivity provided by the spin-polarized electron lattice.

cond-mat.str-el↗