期刊
PHYSICAL REVIEW LETTERS
卷 85, 期 24, 页码 5166-5169出版社
AMER PHYSICAL SOC
DOI: 10.1103/PhysRevLett.85.5166
关键词
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We show that the observed transition from rock salt to orthorhombic P-nma symmetry in CrN can be understood in terms of stress anisotropy. Using Local spin density functional theory, we find that the imbalance between stress stored in spin-paired and spin-unpaired Cr nearest neighbors causes the rock-salt structure to be unstable against distortions and justifies the observed antiferromagnetic ordering. This stress has a purely magnetic origin and may be important in any system where the coupling between spin ordering and structure is strong.
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