| 1. | The uniaxial anisotropy is mainly determined by the first two terms.
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| 2. | In the widely used Stoner Wohlfarth model, the anisotropy is uniaxial.
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| 3. | A crystal with only one optic axis is called a uniaxial crystal.
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| 4. | Unlike uniaxial minerals, biaxial crystals have 2 optic axes.
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| 5. | Fluoborite is uniaxial, just like all other hexagonal minerals.
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| 6. | Stress versus strain data should be obtained in both uniaxial and biaxial forms.
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| 7. | Whereas cryptohalite belongs to the isotropic optical class, bararite is uniaxial negative.
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| 8. | In an optical spectrum changbaiite is uniaxial positive and it can be biaxial.
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| 9. | This applies to a particle with uniaxial magnetocrystalline anisotropy.
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| 10. | Many models of magnetization represent the anisotropy as uniaxial and ignore higher order terms.
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