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Carbides - carbon
KEY POINTS
Carbides are generally formed at high temperatures (> 1500 °C).
Carbides are generally quite stable and exhibit high melting points.
Carbides can be classified as salt-like, interstitial, and covalent..
Salt-like (saline) carbides are composed of the highly electropositive atoms, such as the alkali, alkali earth, and group-III metals, mixed with carbon. Aluminumforms carbides, but other elements from group XIII do not. These materials have isolated carbon centers, often described as "C4-" in the metanides, "C22-" in the acetylides, and "C34-" in the sesquicarbides. Methanides are carbides that decompose in water and generate water; aluminum carbide (Al4C3) and beryllium carbide (Be2C) are examples of this class of carbides. Acetylides are formed from alkali, alkali earth, and lanthanoid metals with the acetylide anion C22-. Lanthanoids also form carbides with the formula M2C3. Metals from group XI also form acetylides, such as copper(I) acetylide and silver acetylide. Carbides of theactinide elements, which have the structure MC2 and M2C3, are also described as salt-like derivatives of C22-. The polyatomic ion C34- is referred to as an allylenide or sesquicarbide and is found in Li4C3 and Mg2C3. The allylenide is linear andisoelectronic with CO2.
In intermediate transition metal carbides, the transition-metal ion is smaller than the critical 135 pm, and the structures are not interstitial but are more complex. Multiple stoichiometries are common. For example, iron forms a number of carbides: Fe3C, Fe7C3 and Fe2C. The best known is cementite, Fe3C, which is present in steels. These carbides are more reactive than the interstitial carbides; for example, the carbides of Cr, Mn, Fe, Co, and Ni are all hydrolyzed by dilute acids and sometimes by water to yield a mixture of hydrogen and hydrocarbons. These compounds share features with both the inert interstitials and the more reactive salt-like carbides.
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