Carbothermic reaction

\( \require{mhchem} \)

Carbothermic reactions involve the reduction of substances, often metal oxides (O^2-), using carbon (C) as the reducing agent. The reduction is usually conducted in the electric arc furnace or reverberatory furnace, depending on the metal ore. These chemical reactions are usually conducted at temperatures of several hundred degrees Celsius. Such processes are applied for production of the elemental forms of many elements. The ability of metals to participate in carbothermic reactions can be predicted from Ellingham diagrams.^[1]

Carbothermal reactions produce carbon monoxide (CO) and sometimes carbon dioxide (CO₂). The facility of these conversions is attributable to the entropy of reaction: two solids, the metal oxide (and flux) and carbon, are converted to a new solid (metal) and a gas (CO_x), the latter having high entropy.

.
Applications

A prominent example is that of iron ore smelting. Many reactions are involved, but the simplified equation is usually shown as:

2Fe₂O₃ + 3C → 4Fe + 3CO₂

On a more modest scale, about 1 million tons of elemental phosphorus is produced annually by carbothermic reactions.^[2] Calcium phosphate (phosphate rock) is heated to 1,200–1,500 °C with sand, which is mostly SiO
₂, and coke (impure carbon) to produce P
₄. The chemical equation for this process when starting with fluoroapatite, a common phosphate mineral, is:

4Ca₅(PO₄)₃F + 18SiO₂ + 30C → 3P₄ + 30CO + 18CaSiO₃ + 2CaF₂

Of historic interest is the Leblanc process. A key step in this process is the reduction of sodium sulfate with coal:^[3]

Na₂SO₄ + 2 C → Na₂S + 2 CO₂

The Na₂S is then treated with calcium carbonate to give sodium carbonate, a commodity chemical.

Recently, development of the 'MagSonic' carbothermic magnesium process has restarted interest in its chemistry:^[4]

MgO + C ↔ Mg + CO

The reaction is readily reversible from its product vapors, and requires rapid cooling to prevent back-reaction.

Silicon

Metallurgical grade silicon may also be obtained by carbothermic reaction. The overall reaction is following:^[5]

SiO₂ + C ↔ Si + CO₂

The actual reaction given is more complex than it seems and includes several steps.^[5]

Variations

Sometimes carbothermic reactions are coupled to other conversions. One example is the chloride process for separating titanium from ilmenite, the main ore of titanium. In this process, a mixture of carbon and the crushed ore is heated at 1000 °C under flowing chlorine gas, giving titanium tetrachloride:

2FeTiO₃ + 7Cl₂ + 6C → 2TiCl₄ + 2FeCl₃ + 6CO

For some metals, carbothermic reactions do not afford the metal, but instead give the metal carbide. This behavior is observed for titanium, hence the use of the chloride process. Carbides also form upon high temperature treatment of Cr₂O₃ with carbon. For this reason, aluminium is employed as the reducing agent.

References

Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8. "Figure 8.19 Ellingham diagram for the free energy of formation of metallic oxides" p. 308
Diskowski, Herbert; Hofmann, Thomas (2005). "Phosphorus". Ullmann's Encyclopedia of Industrial Chemistry. Weinheim: Wiley-VCH. doi:10.1002/14356007.a19_505. ISBN 9783527306732.
Christian Thieme (2000). "Sodium Carbonates". Ullmann's Encyclopedia of Industrial Chemistry. Weinheim: Wiley-VCH. doi:10.1002/14356007.a24_299. ISBN 978-3527306732.
Prentice, Leon; Nagle, Michael (2012). "Carbothermal Production of Magnesium: CSIRO's MagSonic Process". In Mathaudhu (ed.). Magnesium Technology 2012. Cham: Springer. doi:10.1007/978-3-319-48203-3_6. ISBN 9783319482033.
Lee, J. G.; Miller, P. D.; Cutler, I. B. (1977), Wood, John; Lindqvist, Oliver; Helgesson, Claes; Vannerberg, Nils-Gösta (eds.), "Carbothermal Reduction of Silica", Reactivity of Solids, Boston, MA: Springer US, pp. 707–711, doi:10.1007/978-1-4684-2340-2_102, ISBN 978-1-4684-2342-6, retrieved 2023-06-04

Chemistry Encyclopedia

World

Index

Hellenica World - Scientific Library

Retrieved from "http://en.wikipedia.org/"
All text is available under the terms of the GNU Free Documentation License