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The coefficient of thermal expansion of nickel/iron alloys is plotted here against the nickel percentage (on a mass basis) in the alloy. The sharp minimum occurs at the Invar ratio of 36%.
Invar®, also known generically 36FeNi, is a nickel steel alloy 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. Like other nickel/iron compositions, Invar is a solid solution; that is, it is a single-phase alloy—similar to a dilution of common table salt mixed into water.
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 0.62–0.65 ppm/°C. Some formulations display negative thermal expansion (NTE) characteristics. It is used in precision instruments (clocks, physics laboratory devices, seismic creep gauges, shadow-mask frames,Nickel Institute: Nickel & Its Uses 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:[citation needed] this company originates from Aciéries d’Imphy (a small city near Nevers, France) where the alloy was initially industrialised after its invention.
There are variations of the original Invar material that have slightly different coefficient of thermal expansion such as:
A detailed explanation of Invar’s spuriously low CTE has proven elusive for physcists. 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. Scientists had once proposed that Invar’s behavior 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. K. Lagarec, D.G. Rancourt, S.K. Bose, B. Sanyal, and R.A. Dunlap. Observation of a composition-controlled high-moment/low-moment transition in the face centered cubic Fe-Ni system: Invar effect is an expansion, not a contraction. Journal of Magnetism and Magnetic Materials 236 (2001) 107-130. 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. D.G. Rancourt and M.-Z. Dang. Relation between anomalous magneto-volume behaviour and magnetic frustration in Invar alloys. Physical Review B 54 (1996) 12225-12231.
INVAR means invariable. It means that it will not react to thermal expansion.
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