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Invar, also called FeNi, is a special class of metal alloy known as an intermetallic compound and is 64% iron (by weight) and 36% nickel. Invar is notable for its uniquely low coefficient of thermal expansion (CTE or α). It was invented in 1896 by Swiss scientist Charles Edouard Guillaume. He received the Nobel Prize in Physics in 1920 for this discovery, which shows the importance of this alloy in scientific instruments.
Additional recommended knowledge
Common grades of Invar have an α (20–100 °C) of about 1.2 × 10–6 K–1 (1.2 ppm/°C). However, extra-pure grades (<0.1% Co) can readily produce values as low as 0.65 ppm/°C. Some formulations have negative thermal expansion, NTE) it is used in precision instruments (clocks, physics laboratory devices, seismic creep gauges, shadow-mask frames, valves in motors, antimagnetic watches, etc.) However, it has a propensity to creep.
Although Invar is today a widely used material in many industries and applications, this is a particular trademark of a French company named Imphy Alloys: this company originates from Aciéries d’Imphy (a small city near Nevers, France) where the alloy was initially industrialised after its invention. The generic reference for Invar® is FeNi36.
There are variations of the original Invar material that have slightly different coefficient of thermal expansion such as:
Source of thermal properties
Physicists consider true ideal Invar to be an intermetallic compound with molar ratio of Fe65Ni35 that has the face centered cubic crystal structure, since this laboratory alloy has all the essential properties of the commercial varieties. The Invar problem of physics has been to discover the microscopic mechanism that gives Invar its exceptional thermal properties. It was established early on that Invar behaviour is directly related to and dependent upon the alloy's ferromagnetism however the exact mechanism has been the subject of much research and debate, including several international conferences on the subject. The dominant theories of Invar were recently critically reviewed.
All the iron-rich face centered cubic Fe-Ni alloys show Invar anomalies in their measured thermal and magnetic properties, that evolve continuously in intensity with varying alloy composition. Recently it was advanced that Invar behaviour was a direct consequence of a high-magnetic-moment to low-magnetic-moment transition occurring in the face centered cubic Fe-Ni series (and that gives rise to the mineral antitaenite), however this has now been shown to be incorrect. Instead, it appears that the low-moment/high-moment transition is preceded by a high-magnetic-moment frustrated ferromagnetic state in which the Fe-Fe magnetic exchange bonds have a large magneto-volume effect of the right sign and magnitude to create the observed thermal expansion anomaly.
4. Beranger, G., Duffaut, F., Morlet, J., Tiers, Jean-Francois, A Hundred Years after the Discovery of Invar®…The Iron-Nickel Alloys, Intercept Limited, Andover, UK, 1996.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Invar". A list of authors is available in Wikipedia.|