Magnetic Field Response of Dipolar-Octupolar Quantum Spin Ice
Zhengbang Zhou, Félix Desrochers, Yong Baek Kim
TL;DR
This work analyzes dipolar-octupolar quantum spin ice in Ce-based pyrochlores under magnetic fields using gauge mean-field theory (GMFT) and projective symmetry group (PSG) analysis. Spins are mapped to a $U(1)$ gauge theory with spinon matter, allowing exploration beyond perturbative limits and yielding flux backgrounds determined by symmetry. Phase diagrams for field directions [110], [111], and [001] reveal both conventional 0-flux and $oldsymbol{\pi}$-flux QSI phases, plus a novel staggered flux state unique to the [110] field, with first-order field-induced transitions and field-direction–dependent signatures. The predicted static and dynamical spin structure factors provide concrete neutron-scattering fingerprints to guide experiments on Ce$_2$(Zr,Sn,Hf)$_2$O$_7$ and to test the DO-QSI scenario.
Abstract
Dipolar-octupolar (DO) pyrochlore systems Ce$_2$(Zr,Sn,Hf)$_2$O$_7$ have garnered much attention as recent investigations suggest that they may stabilize a novel quantum spin ice (QSI), a quantum spin liquid (QSL) with an emergent $U(1)$ gauge field. In particular, the experimentally estimated microscopic exchange parameters place Ce$_2$Zr$_2$O$_7$ in the $π$-flux QSI regime, and recent neutron scattering experiments have corroborated some key theoretical predictions. On the other hand, to make a definitive conclusion, more multifaceted experimental signatures are desirable. In this regard, recent neutron scattering investigation of the magnetic field dependence of the spin correlations in Ce$_2$Zr$_2$O$_7$ may provide valuable information. However, there have not been any comprehensive theoretical studies for comparison. In this work, we provide such information using gauge mean-field theory (GMFT), allowing for theoretical investigation beyond the perturbative regime. In particular, we construct the phase diagrams for the [110], [111], and [001] field directions. Furthermore, we demonstrate the distinctive evolution of the equal-time and dynamical spin structure factors as a function of the magnetic field for each field direction. These predictions will help future experiments confirm the true nature of the DO-QSI.
