Frustration and Dzyaloshinsky-Moriya anisotropy in the kagome francisites Cu3Bi(SeO3)2O2X (X = Br, Cl)

被引:52
|
作者
Rousochatzakis, Ioannis [1 ]
Richter, Johannes [2 ]
Zinke, Ronald [2 ]
Tsirlin, Alexander A. [3 ]
机构
[1] Max Planck Inst Phys Komplexer Syst, D-01187 Dresden, Germany
[2] Univ Magdeburg, Inst Theoret Phys, D-39016 Magdeburg, Germany
[3] NICPB, EE-12618 Tallinn, Estonia
关键词
TOTAL-ENERGY CALCULATIONS; WEAK FERROMAGNETISM; GROUND-STATE; ORDER; DISORDER; CRYSTAL; LATTICE;
D O I
10.1103/PhysRevB.91.024416
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We investigate the antiferromagnetic canting instability of the spin-1/2 kagome ferromagnet, as realized in the layered cuprates Cu3Bi(SeO3)(2)O2X (X = Br, Cl). While the local canting can be explained in terms of competing exchange interactions, the direction of the ferrimagnetic order parameter fluctuates strongly even at short distances on account of frustration which gives rise to an infinite ground state degeneracy at the classical level. In analogy with the kagome antiferromagnet, the accidental degeneracy is fully lifted only by nonlinear 1/S corrections, rendering the selected uniform canted phase very fragile even for spins-1/2, as shown explicitly by coupled-cluster calculations. To account for the observed ordering, we show that the minimal description of these systems must include the microscopic Dzyaloshinsky-Moriya interactions, which we obtain from density-functional band-structure calculations. The model explains all qualitative properties of the kagome francisites, including the detailed nature of the ground state and the anisotropic response under a magnetic field. The predicted magnon excitation spectrum and quantitative features of the magnetization process call for further experimental investigations of these compounds.
引用
收藏
页数:15
相关论文
共 50 条
  • [41] DIELECTRIC AND PYROELECTRIC STUDIES ON [N(CH(3))(4)](3)BI(2)X(9) (X=CL, BR)
    JAKUBAS, R
    BATOR, G
    MROZ, J
    ACTA PHYSICA POLONICA A, 1995, 87 (03) : 663 - 669
  • [42] Bi6(SeO3)3O5Br2: A new bismuth oxo-selenite bromide
    Berdonosov, Peter S.
    Olenev, Andrei V.
    Kirsanova, Maria A.
    Lebed, Julia B.
    Dolgikh, Valery A.
    JOURNAL OF SOLID STATE CHEMISTRY, 2012, 196 : 232 - 237
  • [43] Georgbokiite Cu5O2(SeO3)2Cl2 -: a new mineral from volcanic exhalations
    Vergasova, LP
    Semenova, TF
    Filatov, SK
    Krivovichev, SV
    Shuvalov, RR
    Anan'ev, VV
    DOKLADY AKADEMII NAUK, 1999, 364 (04) : 527 - 531
  • [44] Cu3(SeO3)2Cl2:: a new oxochloride of copper(II) and selenium(IV)
    Millet, P
    Bastide, B
    Johnsson, M
    SOLID STATE COMMUNICATIONS, 2000, 113 (12) : 719 - 723
  • [45] Tb3O2Cl[SeO3]2 and Tb5O4Cl3[SeO3]2:: Oxide chloride oxoselenates(IV) of trivalent terbium with "lone-pair" channel or layer structures
    Wontcheu, J
    Schleid, T
    ZEITSCHRIFT FUR ANORGANISCHE UND ALLGEMEINE CHEMIE, 2005, 631 (2-3): : 309 - 315
  • [46] X-ray structure of (SnMe3)SeO3[SnMe3(H2O)]
    DiasseSarr, A
    Diop, L
    Mahon, MF
    Molloy, KC
    MAIN GROUP METAL CHEMISTRY, 1997, 20 (04): : 223 - 229
  • [47] Three new copper-lead selenite bromides obtained by chemical vapor transport: Pb5Cu+4(SeO3)4Br6, Pb8Cu2+(SeO3)4Br10, and the synthetic analogue of the mineral sarrabusite, Pb5Cu2+(SeO3)4(Br,Cl)4
    Oleg I. Siidra
    Vasili Yu. Grishaev
    Evgeni V. Nazarchuk
    Roman A. Kayukov
    Mineralogy and Petrology, 2023, 117 : 281 - 291
  • [48] Three new copper-lead selenite bromides obtained by chemical vapor transport: Pb5Cu+4(SeO3)4Br6, Pb8Cu2+(SeO3)4Br10, and the synthetic analogue of the mineral sarrabusite, Pb5Cu2+(SeO3)4(Br,Cl)4
    Siidra, Oleg I. I.
    Grishaev, Vasili Yu.
    Nazarchuk, Evgeni V. V.
    Kayukov, Roman A. A.
    MINERALOGY AND PETROLOGY, 2023, 117 (02) : 281 - 291
  • [49] FERROELECTRIC DISPERSION OF NAD3XH3(1-X)(SEO3)2
    LEVSTIK, A
    LUTHER, G
    MUSER, HE
    FERROELECTRICS, 1980, 23 (1-2) : 15 - 18
  • [50] DIELECTRIC PARAMETERS OF NA(HXD1-X)3(SEO3)2 CRYSTALS
    ZHEREBTS.LI
    ROSTUNTS.AI
    SOVIET PHYSICS CRYSTALLOGRAPHY, USSR, 1968, 13 (03): : 444 - &