One Rudolf Peierls' surprise: the quantum-to-classical transition in the context of solid-state physics

In solid state physics, it is an unsaid (tacit) assumption that the Bloch theorem is applicable to a crystal lattice even if it is of the macroscopic dimensions, provided periodicity is maintained. However, in a realistic situation, electrons in a periodic potential of ions constitute an open quantum system and are subjected to decoherence and dissipation. A natural question arises: up to what distances electrons in a periodic potential can be considered as constituting an effective closed quantum system? And what is the cause of decoherence? To answer some of these questions, the seminal theory of Ovchinnikov and Erikhman of decoherence due to ionic motion is revisited and an oversight of the authors is corrected. Correct conditions for decoherence to occur are worked out. Length scale up to which the motion of ions remains coherent is also calculated. Finally, a realistic physical picture is discussed.

Publication Details

Journal
ArXiv.org
Published
2025-08-27
Primary Topic
Geochemistry and Geologic Mapping
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article
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article

One Rudolf Peierls' surprise: the quantum-to-classical transition in the context of solid-state physics

ArXiv.org
Geochemistry and Geologic Mapping
article

One Rudolf Peierls' surprise: the quantum-to-classical transition in the context of solid-state physics

article en

Abstract

In solid state physics, it is an unsaid (tacit) assumption that the Bloch theorem is applicable to a crystal lattice even if it is of the macroscopic dimensions, provided periodicity is maintained. However, in a realistic situation, electrons in a periodic potential of ions constitute an open quantum system and are subjected to decoherence and dissipation. A natural question arises: up to what distances electrons in a periodic potential can be considered as constituting an effective closed quantum system? And what is the cause of decoherence? To answer some of these questions, the seminal theory of Ovchinnikov and Erikhman of decoherence due to ionic motion is revisited and an oversight of the authors is corrected. Correct conditions for decoherence to occur are worked out. Length scale up to which the motion of ions remains coherent is also calculated. Finally, a realistic physical picture is discussed.

ArXiv.org
Openalex Percentile: Top 60%
Geochemistry and Geologic Mapping
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