Carbonate
A carbonate is a salt of carbonic acid (HCO), characterized by the presence of the carbonate ion, a polyatomic ion with the formula of . The name may also refer to a carbonate ester, an organic compound containing the carbonate group C(=O)(O–). The term is also used as a verb, to describe carbonation: the process of raising the concentrations of carbonate and bicarbonate ions in water to produce carbonated water and other carbonated beverageseither by the addition of carbon dioxide gas under pressure, or by dissolving carbonate or bicarbonate salts into the water. In geology and mineralogy, the term "carbonate  can refer both to carbonate minerals and carbonate rock (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 sedimentary rock. The most common are calcite or calcium carbonate, CaCO, the chief constituent of limestone (as well as the main component of mollusc shells and coral skeletons); dolomite, a calcium-magnesium carbonate CaMg(CO); and siderite, or iron(II) carbonate, FeCO, an important iron ore. Sodium carbonate (soda" or "natron") and potassium carbonate ("potash") have been used since antiquity for cleaning and preservation, as well as for  the manufacture of glass. Carbonates are widely used in industry, such as in iron smelting, as a raw material for Portland cement and lime manufacture, in the composition of ceramic glazes, and more. Structure and bonding. The carbonate ion is the simplest oxocarbon anion. It consists of one carbon atom surrounded by three oxygen atoms, in a trigonal planar arrangement, with "D" molecular symmetry. It has a molecular mass of 60.01 g/mol and carries a total formal charge of −2. It is the conjugate base of the hydrogencarbonate (bicarbonate) ion, , which is the conjugate base of , carbonic acid. The  Lewis structure 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 isoelectronic nitrate ion, the symmetry can be achieved by a resonance among three structures: This resonance can be summarized by a model with fractional bonds and delocalized charges: Chemical properties. Metal carbonates generally decompose on heating, liberating carbon dioxide from  the long term carbon cycle to the short term carbon cycle and leaving behind an oxide of the metal. This process is called calcination, after "calx", the Latin name of quicklime or calcium oxide, CaO, which is obtained by roasting limestone in a lime kiln. A carbonate salt forms when a positively charged ion, , , or , associates with the negatively charged oxygen atoms of the ion by forming electrostatic attractions with them, forming an ionic compound: Most carbonate salts are insoluble in water at standard temperature and pressure, with solubility constants of less than . Exceptions include lithium, sodium, potassium, rubidium, caesium , and ammonium carbonates, as well as many uranium carbonates. In aqueous solution, carbonate, bicarbonate, carbon dioxide, and carbonic acid exist together in a dynamic equilibrium. In strongly basic conditions, the carbonate ion predominates, while in weakly basic conditions, the bicarbonate ion is prevalent. In more acid conditions, aqueous carbon dioxide, CO(aq), is the main form, which, with water, HO, is in equilibrium with carbonic acidthe equilibrium lies strongly towards carbon dioxide. Thus sodium carbonate is basic, sodium bicarbonate is weakly basic, while carbon dioxide itself is a weak acid. Carbonated water is formed by dissolving CO in water under pressure . When the partial pressure of CO is reduced, for example when a can of soda is opened, the equilibrium for each of the forms of carbonate (carbonate, bicarbonate, carbon dioxide, and carbonic acid) shifts until the concentration of CO in the solution is equal to the solubility of CO at that temperature and pressure. In living systems an enzyme, carbonic anhydrase, speeds the interconversion of CO and carbonic acid. Although the carbonate salts of most metals are insoluble in water, the same is not true of the bicarbonate salts. In solution this equilibrium between carbonate, bicarbonate, carbon dioxide and carbonic  acid changes constantly to the changing temperature and pressure conditions. In the case of metal ions with insoluble carbonates, such as CaCO, formation of insoluble compounds results. This is an explanation for the buildup of scale inside pipes caused by hard water. Carbonate in the inorganic nomenclature. Systematic additive IUPAC name for carbonate anion is trioxidocarbonate(2−). Similarly, cyanide anion CN is named nitridocarbonate(1−). However, following the same logic for carbonate(4−) (orthocarbonic acid), by similitude to silicate(4−) (orthosilicic acid), in the systematic additive nomenclature makes no sense as this species has never been identified under normal conditions of temperature and pressure . Orthocarbonic acid is energetically much less stable than orthosilicic acid and cannot exist under normal conditions because of the energetically unfavorable orbital configuration of a single central carbon atom bound to four oxygen atoms. Organic carbonates. In organic chemistry a carbonate can also refer to a functional group 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 ROCOOR′, or RR′CO. Important organocarbonates include dimethyl carbonate, the cyclic compounds ethylene carbonate and propylene carbonate , and the phosgene replacement, triphosgene. Buffer. It works as a buffer in the blood as follows: when pH is low, the concentration of hydrogen ions is too high, so one exhales CO. This will cause the equation to shift left, essentially decreasing the concentration of H ions, causing a more basic pH. When pH is too high, the concentration of hydrogen ions in the blood is too low, so the kidneys excrete bicarbonate (). This causes the equation to shift right, essentially increasing the concentration of hydrogen ions, causing a more acidic pH. Three important reversible reactions control the above pH  balance: Exhaled CO(g) depletes CO(aq), which in turn consumes HCO, causing the aforementioned shift left in the first reaction by Le Châtelier's principle. By the same principle, when the pH is too high, the kidneys excrete bicarbonate () into urine as urea via the urea cycle (or Krebs–Henseleit ornithine cycle). By removing the bicarbonate, more H is generated from carbonic acid (HCO), which comes from CO(g) produced by cellular respiration. Crucially, this same 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 formed of calcium carbonate. Increased solubility of carbonate through increased temperatures results in lower production of marine calcite and increased concentration of atmospheric carbon dioxide. This, in turn, increases Earth temperature. The tonnage of is on a geological scale and may all be redissolved into the sea and released to the atmosphere, increasing CO levels even more. 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 planetary nebula NGC 6302 show evidence for carbonates in space, where  aqueous alteration similar to that on Earth is unlikely. Other minerals have been proposed which would fit the observations. Until recently carbonate deposits have not been found on Mars via remote sensing or in situ missions, even though Martian meteorites contain small amounts. Groundwater may have existed at Gusev and Meridiani Planum.