Calcination reactions usually take place at or above the thermal decomposition temperature (for decomposition and volatilization reactions) or the transition temperature (for
phase transitions). This temperature is usually defined as the temperature at which the standard
Gibbs free energy for a particular calcination reaction is equal to zero.
Limestone calcination In limestone calcination, a decomposition process that occurs at 900 to 1050°C, the chemical reaction is The standard Gibbs free energy of reaction in [J/mol] is approximated as Δ
G°
r ≈ 177,100 J/mol − 158 J/(mol*K) *
T. The standard free energy of reaction is 0 in this case when the temperature,
T, is equal to 1121K, or 848 °C.
Oxidation In some cases, calcination of a metal results in
oxidation of the metal to produce a
metal oxide. In his essay "
Formal response to the question, why Tin and Lead increase in weight when they are calcined" (1630),
Jean Rey notes that "having placed two pounds six ounces of fine English tin in an iron vessel and heated it strongly on an open furnace for the space of six hours with continual agitation and without adding anything to it, he recovered two pounds thirteen ounces of a white calx". He claimed "That this increase in weight comes from the air, which in the vessel has been rendered denser, heavier, and in some measure adhesive, by the vehement and long-continued heat of the furnace: which air mixes with the calx (frequent agitation aiding) and becomes attached to its most minute particles: not otherwise than water makes heavier sand which you throw into it and agitate, by moistening it and adhering to the smallest of its grains", presumably the metal gained weight as it was being oxidized. At room temperature, tin is quite resistant to the impact of air or water, as a thin oxide film forms on the surface of the metal. In air, tin starts to oxidize at a temperature of over 150 °C: Sn + O2 → SnO2.
Antoine Lavoisier explored this experiment with similar results time later. ==Alchemy==