Primary and Secondary Structures - Meteorites
New England Meteoritical Services

 

Decomposing Cohenite

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Meteorite, Nantan, IAB iron 
 
Cohenite is a naturally occurring iron carbide mineral (Fe?C) that forms as a primary phase in iron-nickel alloys, specifically from taenite (a high-nickel Fe-Ni phase) and austenite, during cooling. It crystallizes over a temperature range of approximately 675°C to 610°C, provided the alloy contains 6-8% nickel. Above 8% nickel, cohenite formation is inhibited. The carbon required for its formation is sourced from the surrounding matrix, reacting with taenite to produce this mineral.

The temperature window for cohenite formation-spanning 675°C to 610°C-varies slightly depending on the Ni/Fe ratio of the alloy. Below 610°C, cohenite ceases to form, and graphite begins to take its place. By this point, phases such as taenite, cohenite, and kamacite (a low-nickel Fe-Ni phase) have stabilized, while other minerals, like schreibersite ((Fe,Ni)?P), start to nucleate. Schreibersite can begin forming at temperatures as high as 850°C and continues down to around 400°C, when nucleation processes generally stop.

Temperature is a critical factor in both the formation and breakdown of cohenite. As the alloy cools below 610°C, cohenite becomes unstable and decomposes into its constituent elements-iron (Fe), nickel (Ni), and carbon (C)-with the carbon often precipitating as graphite within the matrix. This decomposition occurs through a process of resolution and graphite nucleation, with its rate influenced by the nickel content, the temperature, and the time available before the material cools past 610°C.

In iron meteorites, where cohenite is almost exclusively found, this decomposition continues below 610°C. The unique conditions of slow cooling in space allow cohenite to form and persist, though its instability at lower temperatures leads to its eventual breakdown into Fe, Ni, and graphite.


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Figure 1. Scale bar 1.2 mm.

Meteorite, Nantan, IAB
 
Decomposing cohenite surrounding kamacite.
 
 
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Figure 1. Scale bar 1.2 mm.

Meteorite, Nantan, IAB
 
Decomposing cohenite
 
 
 
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