| Display title | Magnetocrystalline anisotropy |
| Default sort key | Magnetocrystalline Anisotropy |
| Page length (in bytes) | 21,118 |
| Namespace ID | 0 |
| Page ID | 235396 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
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| Counted as a content page | Yes |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
| Move | Allow all users (infinite) |
| Page creator | imported>SpringEdit |
| Date of page creation | 05:35, 9 March 2024 |
| Latest editor | imported>SpringEdit |
| Date of latest edit | 05:35, 9 March 2024 |
| Total number of edits | 1 |
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Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | In physics, a ferromagnetic material is said to have magnetocrystalline anisotropy if it takes more energy to magnetize it in certain directions than in others. These directions are usually related to the principal axes of its crystal lattice. It is a special case of magnetic anisotropy. In other words... |
