An iron–nickel alloy or nickel–iron alloy, abbreviated FeNi or NiFe, is a group of consisting primarily of the chemical element nickel (Ni) and iron (Fe). It is the main constituent of the "iron" and . In chemistry, the acronym NiFe refers to an iron–nickel Catalysis or component involved in various chemical reactions, or the reactions themselves; in geology, it refers to the main constituents of telluric (including Earth's).
Some metallurgy of iron–nickel are called nickel steel or stainless steel. Depending on the intended use of the alloy, these are usually fortified with small amounts of other metals, such as chromium, cobalt, molybdenum, and titanium.
Nickel–iron alloys occur naturally on Earth's surface as telluric iron or meteoric iron.
In steel metallurgy, nickel is alloyed with iron since 1888 (date of Schneider et Cie's patent on nickel steel based on Jean Werth's research) to produce maraging steel and some . Other technological uses include Invar and Mu-metal.
FeNi |
NiFe to NiFe |
about 5.5% nickel |
36% nickel |
36% nickel |
FeNi |
15–25% nickel |
5–30% nickel |
77% nickel |
various |
4–8% nickel |
NiFe |
0.05%–4% nickel |
FeNi |
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