Site-Specific Structure at Multiple Length Scales in Kagome Quantum Spin Liquid Candidates

TL;DR

This study uses advanced synchrotron techniques and calculations to characterize the structure of kagome quantum spin liquid candidates, revealing site-specific details that support their potential as ideal QSL materials.

Contribution

It introduces new methodologies for site-specific diffraction and spectroscopy, providing detailed structural insights into Zn-barlowite and herbertsmithite QSL candidates, and clarifies defect effects on QSL physics.

Findings

Zn does not substitute onto kagome layers, preserving QSL physics.

Cu and Zn occupy distinct interlayer sites in Zn-barlowite.

Structural differences influence the magnetic properties and defect resistance.

Abstract

Realizing a quantum spin liquid (QSL) ground state in a real material is a leading issue in condensed matter physics research. In this pursuit, it is crucial to fully characterize the structure and influence of defects, as these can significantly affect the fragile QSL physics. Here, we perform a variety of cutting-edge synchrotron X-ray scattering and spectroscopy techniques, and we advance new methodologies for site-specific diffraction and L-edge Zn absorption spectroscopy. The experimental results along with our first-principles calculations address outstanding questions about the local and long-range structures of the two leading kagome QSL candidates, Zn-substituted barlowite Cu$_3$Zn$_{x}$Cu$_{1-x}$(OH)$_6$FBr and herbertsmithite Cu$_3$Zn(OH)$_6$Cl$_2$. On all length scales probed, there is no evidence that Zn substitutes onto the kagome layers, thereby preserving the QSL physics of the kagome lattice. Our calculations show that antisite disorder is not energetically favorable and is even less favorable in Zn-barlowite compared to herbertsmithite. Site-specific X-ray diffraction measurements of Zn-barlowite reveal that Cu$^{2+}$ and Zn$^{2+}$ selectively occupy distinct interlayer sites, in contrast to herbertsmithite. Using the first measured Zn L-edge inelastic X-ray absorption spectra combined with calculations, we discover a systematic correlation between the loss of inversion symmetry from pseudo-octahedral (herbertsmithite) to trigonal prismatic coordination (Zn-barlowite) with the emergence of a new peak. Overall, our measurements suggest that Zn-barlowite has structural advantages over herbertsmithite that make its magnetic properties closer to an ideal QSL candidate: its kagome layers are highly resistant to nonmagnetic defects while the interlayers can accommodate a higher amount of Zn substitution.