IPA: /ˌfɛrɪˈmæɡnɪˌtɪzəm/
KK: /fɛrɪˈmæɡnɪtɪzəm/
A type of magnetism where materials have unequal magnetic moments that do not completely cancel each other out, resulting in some overall magnetization even at low temperatures.
Ferrimagnetism is observed in certain materials like magnetite, where the magnetic moments of the atoms are unequal.
Ferrimagnetism → It is formed from "ferri-" (from Latin "ferrum", meaning iron) and "magnetism" (from Greek "magnetis", meaning of Magnesia, a region known for its magnetic properties). The term describes a type of magnetism that occurs in materials that have unequal magnetic moments, typically involving iron.
Think of 'iron' ('ferri-') and 'magnetism' together to remember that 'ferrimagnetism' refers to a magnetic property related to iron.
No commonly confused words.