Tweaking the spin-wave dispersion and suppressing the incommensurate phase in LiNiPO4 by iron substitution

TitleTweaking the spin-wave dispersion and suppressing the incommensurate phase in LiNiPO4 by iron substitution
Publication TypeJournal Article
Year of Publication2009
AuthorsLi JY, Jensen TBS, Andersen NH, Zarestky JL, McCallum RW, Chung JH, Lynn JW, Vaknin D
Journal TitlePhysical Review B
Date Published05/01
ISBN Number1098-0121
Accession NumberISI:000266501100088
Keywordscommensurate-incommensurate transformations, energy gap, exchange interactions (electron), frustration, heisenberg model, iron compounds, lithium compounds, magnetic structure, magnetic transitions, neutron diffraction, nickel compounds, spin hamiltonians

Elastic and inelastic neutron-scattering studies of Li(Ni1-xFex)PO4 single crystals reveal anomalous spin-wave dispersions along the crystallographic direction parallel to the characteristic wave vector of the magnetic incommensurate phase. The anomalous spin-wave dispersion (magnetic soft mode) indicates the instability of the Ising-type ground state that eventually evolves into the incommensurate phase as the temperature is raised. The pure LiNiPO4 system (x=0) undergoes a first-order magnetic phase transition from a long-range incommensurate phase to an antiferromagnetic (AFM) ground state at T-N=20.8 K. At 20% Fe concentrations, although the AFM ground state is to a large extent preserved as that of the pure system, the phase transition is second order, and the incommensurate phase is completely suppressed. Analysis of the dispersion curves using a Heisenberg spin Hamiltonian that includes interplane and in-plane nearest- and next-nearest-neighbor couplings reveals frustration due to strong competing interactions between nearest- and next-nearest-neighbor sites, consistent with the observed incommensurate structure. The Fe substitution only slightly lowers the extent of the frustration, sufficient to suppress the incommensurate phase. An energy gap in the dispersion curves gradually decreases with the increase in Fe content from similar to 2 meV for the pure system (x=0) to similar to 0.9 meV for x=0.2.

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