2009
DOI: 10.1134/s1063783409060158
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Hydrostatic pressure and hexagonal magnetic anisotropy of hematite

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Cited by 2 publications
(8 citation statements)
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“…In [4], this discrepancy is explained by the residual after growth mechanical stresses in a sample. In [8], we sug gested a mechanism explaining the increase in the effective hexagonal magnetic anisotropy constant in the case when the crystal is not perfect. The residual mechanical stresses arising in the process of fast cool ing after the synthesis [9] were simulated by a hypo thetic hydrostatic pressure.…”
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confidence: 81%
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“…In [4], this discrepancy is explained by the residual after growth mechanical stresses in a sample. In [8], we sug gested a mechanism explaining the increase in the effective hexagonal magnetic anisotropy constant in the case when the crystal is not perfect. The residual mechanical stresses arising in the process of fast cool ing after the synthesis [9] were simulated by a hypo thetic hydrostatic pressure.…”
mentioning
confidence: 81%
“…The hydrostatic pressure P contributes to the effective uniaxial anisotropy constant in the form a -μP (a is the uniaxial crystalline anisotropy constant and μ is a constant, see below). In turn, this constant determines the contribution Δe to the effective hexagonal anisot ropy of the crystal [8]: Δe = d 2 /4(a -μP) (d is the fourth order magnetic anisotropy constant). The model constructed in [8] led to rather a high hydro static pressure (~10 10 dyn/cm 2 ).…”
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confidence: 99%
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