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Austenite, also known as gamma phase iron is a metallic non-magnetic allotrope of iron or a solid solution of iron, with an alloying element. In plain-carbon steel, austenite exists above the critical eutectoid temperature of 1,000 K (1,340 °F); other alloys of steel have different eutectoid temperatures. It is named after Sir William Chandler Roberts-Austen (1843–1902).

Austenite is a metallic, non-magnetic solid solution of carbon and iron that exists in steel above the critical temperature of 1333°F ( 723°C). Its face-centred cubic (FCC) structure allows it to hold a high proportion of carbon in solution. In many magnetic alloys, the Curie point, the temperature at which magnetic materials cease to behave magnetically, occurs at nearly the same temperature as the austenite transformation. This behavior is attributed to the paramagnetic nature of austenite, while both martensite and ferrite are strongly ferromagnetic.

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Aluminum Alloys austenite Corrosion Dislocation Phenomena eutectoid Fe-Fe3C Fe-Fe3C T-T-T Diagram gamma iron Heat Treatment of Steel Hydrogen Embrittlement hypereutectoid Martensite Formation metal casting Metallurgy Glossary pearlite Phase Diagram of Steel Powder Metallurgy proeutectoid ferrite Shape Memory Alloy solid solution stainless steel TTT Diagram Types of Materials

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