NMR Evidence of Tomonaga–Luttinger Liquid Behavior in Lednevite Mineral Cu[PO3(OH)] ⋅ H2O

We report nuclear magnetic resonance (NMR) studies on lednevite mineral Cu[PO 3 (OH)] ⋅ H 2 O. Nuclear spin-lattice relaxation rate reveals signature of one-dimensional Tomonaga–Luttinger liquid (TTL) behavior. In particular, over a wide temperature range, it is consistent with theoretical predictions for Tomonaga–Luttinger liquid: 1/ T 1 T ( T ) ~ T (1/2 K ) – 2 , with a Luttinger parameter, K = 0.27(3), and negative exponent – a hallmark of Tomonaga–Luttinger liquid spin dynamics. This finding provides a microscopic evidence for unconventional quasi-1D conductivity in lednevite mineral.

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Publication Details

Journal
Journal of Experimental and Theoretical Physics Letters
Published
2026-09-14
DOI
https://doi.org/10.1134/s0021364026608146
Primary Topic
Clay minerals and soil interactions
Type
article
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article

NMR Evidence of Tomonaga–Luttinger Liquid Behavior in Lednevite Mineral Cu[PO3(OH)] ⋅ H2O

С.В. Журенко, A. A. Gippius, K. S. Pervakov, A. A. Gippius et al.
Journal of Experimental and Theoretical Physics Letters
Clay minerals and soil interactions
article

NMR Evidence of Tomonaga–Luttinger Liquid Behavior in Lednevite Mineral Cu[PO3(OH)] ⋅ H2O

С.В. Журенко, A. A. Gippius, K. S. Pervakov, A. A. Gippius, A. V. Tkachev
article en

Abstract

We report nuclear magnetic resonance (NMR) studies on lednevite mineral Cu[PO 3 (OH)] ⋅ H 2 O. Nuclear spin-lattice relaxation rate reveals signature of one-dimensional Tomonaga–Luttinger liquid (TTL) behavior. In particular, over a wide temperature range, it is consistent with theoretical predictions for Tomonaga–Luttinger liquid: 1/ T 1 T ( T ) ~ T (1/2 K ) – 2 , with a Luttinger parameter, K = 0.27(3), and negative exponent – a hallmark of Tomonaga–Luttinger liquid spin dynamics. This finding provides a microscopic evidence for unconventional quasi-1D conductivity in lednevite mineral.

Journal of Experimental and Theoretical Physics Letters
Openalex Percentile: Top 21%
Clay minerals and soil interactions
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