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A carbonate is a salt of , (), characterized by the presence of the carbonate ion, a with the formula . The word "carbonate" may also refer to a , an organic compound containing the carbonate group .

The term is also used as a verb, to describe : the process of raising the concentrations of carbonate and ions in water to produce and other carbonated beverageseither by the addition of gas under pressure or by dissolving carbonate or bicarbonate salts into the water.

In and , the term "carbonate" can refer both to carbonate minerals and (which is made of chiefly carbonate minerals), and both are dominated by the carbonate ion, . Carbonate minerals are extremely varied and ubiquitous in chemically precipitated . The most common are or calcium carbonate, , the chief constituent of (as well as the main component of shells and skeletons); dolomite, a calcium-magnesium carbonate ; and , or iron(II) carbonate, , an important . ("soda" or "natron"), , and potassium carbonate ("potash"), , have been used since antiquity for cleaning and preservation, as well as for the manufacture of . Carbonates are widely used in industry, such as in iron smelting, as a raw material for and lime manufacture, in the composition of , and more. New applications of alkali metal carbonates include: thermal energy storage, catalysis and electrolyte both in fuel cell technology as well as in electrosynthesis of in aqueous media.Anodic generation of hydrogen peroxide in continuous flow, DOI: 10.1039/D2GC02575B (Paper) Green Chem., 2022, 24, 7931–7940


Structure and bonding
The carbonate ion is the simplest . It consists of one atom surrounded by three atoms, in a arrangement, with D3h molecular symmetry. It has a molecular mass of 60.01  and carries a total of −2. It is the of the ion, , which is the conjugate base of , .

The of the carbonate ion has two (long) single bonds to negative oxygen atoms, and one short double bond to a neutral oxygen atom.

This structure is incompatible with the observed symmetry of the ion, which implies that the three bonds are the same length and that the three oxygen atoms are equivalent. As in the case of the ion, the symmetry can be achieved by a resonance among three structures:

This resonance can be summarized by a model with fractional bonds and charges:


Chemical properties
Metal carbonates generally decompose on heating, liberating carbon dioxide and leaving behind an oxide of the metal. This process is called , after calx, the Latin name of quicklime or , CaO, which is obtained by roasting limestone in a :
As illustrated by its affinity for , carbonate is a ligand for many metal cations. Transition metal carbonate and bicarbonate complexes feature metal ions covalently bonded to carbonate in a variety of bonding modes.

Lithium, , potassium, rubidium, caesium, and ammonium carbonates are water-soluble salts, but carbonates of 2+ and 3+ ions are often poorly soluble in water. Of the insoluble metal carbonates, is important because, in the form of , it accumulates in and impedes flow through pipes. is rich in this material, giving rise to the need for infrastructural .

Acidification of carbonates generally liberates :

Thus, scale can be removed with acid.

In solution the equilibrium between carbonate, bicarbonate, carbon dioxide and carbonic acid is sensitive to pH, temperature, and pressure. Although di- and trivalent carbonates have low solubility, bicarbonate salts are far more soluble. This difference is related to the disparate of solids composed of mono- vs dianions, as well as mono- vs dications.

In , carbonate, bicarbonate, carbon dioxide, and carbonic acid participate in a dynamic equilibrium. In strongly basic conditions, the carbonate ion predominates, while in weakly basic conditions, the ion is prevalent. In more acid conditions, aqueous , , is the main form, which, with water, , is in equilibrium with carbonic acidthe equilibrium lies strongly towards carbon dioxide. Thus is basic, sodium bicarbonate is weakly basic, while carbon dioxide itself is a weak acid.


Organic carbonates
In organic chemistry a carbonate can also refer to a within a larger molecule that contains a carbon atom bound to three oxygen atoms, one of which is double bonded. These compounds are also known as organocarbonates or carbonate esters, and have the general formula , or . Important organocarbonates include dimethyl carbonate, the cyclic compounds ethylene carbonate and propylene carbonate, and the phosgene replacement, .


Buffer
Three reversible reactions control the pH balance of blood and act as a to stabilise it in the range 7.37–7.43:

Exhaled depletes , which in turn consumes , causing the equilibrium of the first reaction to try to restore the level of carbonic acid by reacting bicarbonate with a hydrogen ion, an example of Le Châtelier's principle. The result is to make the blood more alkaline (raise pH). By the same principle, when the pH is too high, the kidneys excrete bicarbonate () into urine as urea via the (or Krebs–Henseleit ornithine cycle). By removing the bicarbonate, more is generated from carbonic acid (), which comes from produced by cellular respiration.

(2025). 9781292094939, Pearson.

Crucially, a similar buffer operates in the oceans. It is a major factor in climate change and the long-term carbon cycle, due to the large number of marine organisms (especially coral) which are made of calcium carbonate. Increased solubility of carbonate through increased temperatures results in lower production of marine and increased concentration of atmospheric carbon dioxide. This, in turn, increases Earth temperature. The amount of available is on a geological scale and substantial quantities may eventually be redissolved into the sea and released to the atmosphere, increasing levels even more.


Carbonate salts
  • Carbonate overview:


Presence outside Earth
It is generally thought that the presence of carbonates in rock is strong evidence for the presence of liquid water. Recent observations of the NGC 6302 show evidence for carbonates in space,Kemper, F., Molster, F.J., Jager, C. and Waters, L.B.F.M. (2001) The mineral composition and spatial distribution of the dust ejecta of NGC 6302. Astronomy & Astrophysics 394, 679–690. where aqueous alteration similar to that on Earth is unlikely. Other minerals have been proposed which would fit the observations.

Small amounts of carbonate deposits have been found on Mars via spectral imaging and Martian meteorites also contain small amounts. Groundwater may have existed at and .


See also


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