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The 20 pages that link to Magnetic anisotropy, each with the reason it gives.

• Magnetic susceptibilityRelated: Anisotropic materials require susceptibility to be represented by a direction-dependent tensor.

• FerromagnetismRelated: Anisotropy selects favored magnetization directions and affects domain stability.

• Magnetic hysteresisRelated: Anisotropy shapes the energy barriers that influence hysteresis and switching fields.

• Curie temperatureRelated: It influences domain structure and magnetic behavior below the ordering threshold.

• Magnetic domainRelated: It favors particular domain orientations, called easy axes.

• AntiferromagnetismRelated: Anisotropy can select the directions along which ordered moments point.

• SuperparamagnetismRelated: It sets the energy barrier that thermal fluctuations must overcome.

• Permanent magnetRelated: Strong anisotropy helps keep a magnetization direction stable.

• Rare-earth magnetRelated: Strong directional preference helps rare-earth magnets resist demagnetization.

• TerbiumRelated: Terbium’s strong anisotropy contributes to its usefulness in magnetostrictive alloys.

• DysprosiumRelated: Dysprosium’s anisotropy helps magnets resist demagnetization as temperature rises.

• Magnetoresistive random-access memoryRelated: It helps keep each junction’s stored magnetic state stable without power.

• 4f electronRelated: The orbital character of 4f states can produce strong direction-dependent magnetism.

• MaghemiteRelated: Anisotropy influences how maghemite particles reverse their magnetization.

• Thermoremanent magnetizationRelated: Preferred magnetic directions help stabilize the remanence after cooling.

• SamariumRelated: Strong anisotropy helps samarium–cobalt magnets resist demagnetization.

• Hopkinson effectRelated: Its weakening with temperature can make magnetization respond more readily to small fields.

• Louis NéelRelated: Anisotropy helps determine the stability and arrangement of magnetic domains.

• Magnetic systemsRelated: Anisotropy selects preferred orientations for magnetic moments in a material.

• Rock magnetismRelated: Anisotropy can bias remanence directions and complicate paleomagnetic readings.