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Calcium sulfide
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Calcium sulfide is the chemical compound with the formula . This white material crystallizes in cubes like rock salt. CaS has been studied as a component in a process that would recycle , a product of flue-gas desulfurization. Like many salts containing ions, CaS typically has an odour of , which results from small amount of this gas formed by hydrolysis of the salt.

In terms of its atomic structure, CaS crystallizes in the same motif as indicating that the bonding in this material is highly . The high melting point is also consistent with its description as an ionic solid. In the crystal, each ion is surrounded by an of six Ca2+ ions, and complementarily, each Ca2+ ion surrounded by six S2− ions.


Production
CaS is produced by carbothermic reduction of , which entails the conversion of carbon, usually as charcoal, to :
CaSO4 + 2 C → CaS + 2 CO2
and can react further:
3 CaSO4 + CaS → 4 + 4

In the second reaction the (+6 ) oxidizes the (−2 oxidation state) to (+4 oxidation state), while it is being reduced to sulfur dioxide itself (+4 oxidation state).

CaS is also a byproduct in the , a once major industrial process for producing sodium carbonate. In that process sodium sulfide reacts with calcium carbonate:

Na2S + CaCO3 → CaS + Na2CO3
Millions of tons of this calcium sulfide byproduct was discarded, causing extensive pollution and controversy.

Milk of lime, Ca(OH)2, reacts with elemental sulfur to give a "", which has been used as an . The active ingredient is probably a calcium , not CaS.Holleman, A. F.; Wiberg, E. "Inorganic Chemistry" Academic Press: San Diego, 2001. .


Reactivity and uses
Calcium sulfide decomposes upon contact with water, including moist air, giving a mixture of Ca(SH)2, Ca(OH)2, and Ca(SH)(OH).
CaS + H2O → Ca(SH)(OH)
Ca(SH)(OH) + H2O → Ca(OH)2 + H2S

It reacts with such as hydrochloric acid to release toxic gas.

CaS + 2 HCl → CaCl2 + H2S

Calcium sulfide is , and will glow a blood red for up to an hour after a light source is removed.

As a noxious byproduct of the , it can be converted to calcium carbonate and , the latter of which can be used as a sulfur source for the lead chamber process to produce the necessary for the Leblanc process:


Natural occurrence
is the name for mineralogical form of CaS. It is a rare component of some meteorites and has scientific importance in solar nebula research. Burning of coal dumps can also produce the compound.


See also
  • Glossary of meteoritics

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