Magnetoconductivity and quantum oscillations in intercalated graphite CaC6 with the Fermi surface reconstructed by the uniaxial charge density wave

Abstract

We report a magnetoconductivity tensor σ for the intercalated graphite CaC6, in the ground state of the uniaxial charge density wave (CDW), under conditions of coherent magnetic breakdown due to strong external magnetic field B perpendicular to the conducting plane. The uniaxial charge density wave reconstructs initially closed Fermi surface into an open one, accompanied with formation of a pseudo-gap in the electron density of states around the Fermi energy. The magnetoconductivity tensor is calculated within the quantum density matrix and semiclassical magnetic breakdown approach focused on modification of the main, so-called classical contribution to magnetoconductivity by magnetic breakdown, neglecting the higher order corrections. In the presence of magnetic breakdown, in spite of open Fermi surface configuration, all classical magnetoconductivity components, the one along the CDW apex σxx 1/B2, perpendicular to the CDW apex σyy const, as well as the Hall conductivity σxy 1/B, undergo strong quantum oscillations vs. inverse magnetic field. Those oscillations do not appear as a mere additive correction, but rather alter the classical result becoming an inherent part of it, turning it to essentially non-classical.

0

Turn this paper into a full lesson

ArcXiv compiles a staged curriculum from this paper: 8-12 lessons across beginner → advanced, synthesised section guides, visuals, flashcards, a quiz, exercises, and on-demand deep dives per section. Grounded in the abstract, never invented.

Discussion (0)

Sign in to join the discussion.

Loading comments…