A carbonate is a salt or ester of carbonic acid, H2CO3, containing the carbonate ion [CO3]2-. A solution of carbon dioxide in water reacts with a base to form a carbonate.
Carbonates are common rock-forming minerals, occurring as calcite and limestone (both calcium carbonate, CaCO3), siderite (FeCaCO3), magnesite (MgCO3), dolomite (CaMg(CO3)2), and ankerite (Ca(Fe,Mg,Mn)(CO3)2).
The bicarbonates (hydrogen carbonates) contain the [HCO3]- ion and important salts include NaHCO3 and Ca(HCO3)2.
The carbonates of the alkali metals and alkaline earth metals are stable (the latter insoluble). Most other metal carbonates are precipitated as basic carbonates, e.g. 2PbCO3·Pb(OH)2. All carbonates except the alkali metal carbonates lose carbon dioxide on strong heating.
Carbonate esters are important solvents.
Related categories INORGANIC CHEMISTRY
GEOLOGY AND PLANETARY SCIENCE
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