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本文基于双时格林函数方法, 通过对不同格点和同格点的高阶格林函数分别采用Tyablikov和Callen退耦近似, 系统研究了双二次型交换作用和各向异性对简单立方晶格反铁磁模型相变的影响. 得到了相变温度的解析表达式, 发现相变温度随着各向异性的增强而升高, 但随着双二次型相互作用的增强而下降.
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关键词:
- 反铁磁 /
- 磁各向异性 /
- 磁序的一般理论和模型 /
- 交换和超交换相互作用
The existence of biquadratic exchange had been well established by Anderson, Huang and Allen. Early investigations indicated that the biquadratic exchange term in spin Hamiltonian was found to have significant effects on the magnetic properties of compounds containing iron-group ions or rare-earth metal ions. Recently, studying the anisotropic magnetic excitation of iron-based superconducting materials indicated that the experimental phenomenon cannot be explained well only by a simple collinear Heisenberg antiferromagnetic model. However, if the nearest neighbor biquadratic spin coupling is introduced, the experiment can be well explained. Similar results had also been obtained in the investigation of the superconducting material FeSe. As a result, exploring the effect of biquadratic exchange interactions on the magnetic properties of magnetic systems is significance. In this paper, we use the double-time Green's function method to study the properties of the spin-1 Heisenberg antiferromagnets with biquadratic exchange interactions and anisotropy on a three-dimensional lattice. We derive the equation of motion of the Green's function by a standard procedure. In the course of this, the higher order Green functions have to be decoupled. For the higher order Green functions of different lattice points, a Tyablikov or random phase approximation decoupling are used to decuple. For the higher order Green functions of the same lattice points, we adopt the Anderson-Callen decoupling to decouple. Based on the above procedures, the analytic expressions of the magnetization and critical temperature are obtained. The effects of biquadratic exchange interactions and anisotropy on the critical temperature are discussed in detailed. Our results show that the critical temperature increases with the increase of the anisotropy for a given biquadratic interaction. Regardless of the value of the anisotropy, the critical temperature always decreases with the increase of the biquadratic interaction. As the value of anisotropic parameter$\eta = 0$ , there is an obvious linear relationship between the critical temperature and the biquadratic interaction. However, when the anisotropy of the system becomes weaker, there is no such linear relationship between them. By comparing similar ferromagnetic models, it is found that the results of this paper are significantly different from those of the ferromagnetic model. When the biquadratic interaction is equal to 0, our results agree with other theoretical results.-
Keywords:
- antiferromagnetic /
- magnetic anisotropy /
- general theory and models of magnetic ordering /
- exchange and superexchange interactions
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[12] Köbler U, Mueller R M, Schnelle W, Fischer K 1998 J. Magn. Magn. Mater. 188 333Google Scholar
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[15] Chen H H, Levy P M 1973 Phys. Rev. B 7 4267Google Scholar
[16] Iwashita T, Uryu N 1976 Phys. Rev. B 14 3090Google Scholar
[17] Oitmaa J, Hamer C J 2013 Phys. Rev. B 87 224431Google Scholar
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[19] Chaddha G S, Sharma A 1999 J. Magn. Magn. Mater. 191 373Google Scholar
[20] Stanek D, Sushkov O P, Uhrig G S 2011 Phys. Rev. B 84 064505Google Scholar
[21] Wang H Y 2012 Green’s Function in Condensed Matter Physics (Beijing: Alpha Science International Ltd and Science Press) p348
[22] 王怀玉, 夏青 2007 物理学报 56 5466Google Scholar
Wang H Y, Xia Q 2007 Acta Phys. Sin. 56 5466Google Scholar
[23] Callen H B 1963 Phys. Rev. 130 890Google Scholar
[24] Pan K K 2009 Phys. Rev. B 79 134414Google Scholar
[25] Gaunt D S, Guttman A J. 1974 Phase Transitions and Critical Phenomena (New York: Academic Press) p456
[26] Pan K K 2005 Phys. Rev B 71 134524Google Scholar
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[1] Anderson P W 1959 Phys. Rev. 115 2Google Scholar
[2] Huang N L, Orbach R 1964 Phys. Rev. Lett. 12 275
[3] Allan G A T, Betts D D 1967 Proc. Phys. Soc. London 91 341Google Scholar
[4] Joseph R I 1965 Phys. Rev. 138 1441Google Scholar
[5] Millet P, Mila F, Zhang F C, Mambrini M, Van Oosten A B, Pashchenko V A, Sulpice A, Stepanov A 1999 Phys. Rev. Lett. 83 4176Google Scholar
[6] Mila F, Zhang F C 2000 Eur. Phys. J. B 16 7Google Scholar
[7] Luo C, Datta T, Yao D X 2016 Phys. Rev. B 93 235148Google Scholar
[8] Wysocki A L, Belashchenko K D, Antropov V P 2011 Nat. Phys. 7 485Google Scholar
[9] Ergueta P B, Nevidomskyy A H 2015 Phys. Rev. B 92 165102Google Scholar
[10] Zhuo W Z, Qin M H, Dong S, Li X G, Liu J M 2016 Phys. Rev. B 93 094424Google Scholar
[11] Yu R, Si Q M 2015 Phys. Rev. Lett. 115 116401Google Scholar
[12] Köbler U, Mueller R M, Schnelle W, Fischer K 1998 J. Magn. Magn. Mater. 188 333Google Scholar
[13] Köbler U, Hoser A, Kawakami M, Chatterji T, Rebizant J 1999 J. Magn. Magn. Mater. 205 343Google Scholar
[14] Yu R, Nevidomskyy A H 2016 J. Phys. Condens. Matter 28 495702Google Scholar
[15] Chen H H, Levy P M 1973 Phys. Rev. B 7 4267Google Scholar
[16] Iwashita T, Uryu N 1976 Phys. Rev. B 14 3090Google Scholar
[17] Oitmaa J, Hamer C J 2013 Phys. Rev. B 87 224431Google Scholar
[18] Rabuffo I, De Cesare L, D’Auria A C, Mercaldo M T 2019 Eur. Phys. J. B 92 154Google Scholar
[19] Chaddha G S, Sharma A 1999 J. Magn. Magn. Mater. 191 373Google Scholar
[20] Stanek D, Sushkov O P, Uhrig G S 2011 Phys. Rev. B 84 064505Google Scholar
[21] Wang H Y 2012 Green’s Function in Condensed Matter Physics (Beijing: Alpha Science International Ltd and Science Press) p348
[22] 王怀玉, 夏青 2007 物理学报 56 5466Google Scholar
Wang H Y, Xia Q 2007 Acta Phys. Sin. 56 5466Google Scholar
[23] Callen H B 1963 Phys. Rev. 130 890Google Scholar
[24] Pan K K 2009 Phys. Rev. B 79 134414Google Scholar
[25] Gaunt D S, Guttman A J. 1974 Phase Transitions and Critical Phenomena (New York: Academic Press) p456
[26] Pan K K 2005 Phys. Rev B 71 134524Google Scholar
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