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Magnesium carbonate,MgCO3 (archaic namemagnesia alba), is an inorganic salt that is a colourless or white solid. Severalhydrated andbasic forms of magnesium carbonate also exist asminerals.
The most common magnesium carbonate forms are theanhydrous salt calledmagnesite (MgCO3), and the di, tri, and pentahydrates known as barringtonite (MgCO3·2H2O), nesquehonite (MgCO3·3H2O), and lansfordite (MgCO3·5H2O), respectively.[6] Some basic forms such asartinite (Mg2CO3(OH)2·3H2O),hydromagnesite (Mg5(CO3)4(OH)2·4H2O), anddypingite (Mg5(CO3)4(OH)2·5H2O) also occur asminerals. All of those minerals are colourless or white.
The dihydrate has atriclinic structure, while the trihydrate has amonoclinic structure.
References to "light" and "heavy" magnesium carbonates actually refer to the magnesium hydroxy carbonateshydromagnesite anddypingite, respectively.[7] The "light" form is precipitated from magnesium solutions using alkali carbonate at "normal temperatures" while the "heavy" may be produced from boiling concentrated solutions followed by precipitation to dryness, washing of the precipitate, and drying at 100 C.[8]
If magnesium chloride (or sulfate) is treated with aqueous sodium carbonate, a precipitate of basic magnesium carbonate – ahydrated complex of magnesium carbonate andmagnesium hydroxide – rather than magnesium carbonate itself is formed:
High purity industrial routes include a path throughmagnesium bicarbonate, which can be formed by combining aslurry of magnesium hydroxide andcarbon dioxide at high pressure and moderate temperature.[6] The bicarbonate is then vacuum dried, causing it to lose carbon dioxide and a molecule of water:
At high temperatures MgCO3 decomposes tomagnesium oxide andcarbon dioxide. This process is important in the production of magnesium oxide.[6] This process is calledcalcining:
MgCO3 → MgO + CO2 (ΔH = +118 kJ/mol)
The decomposition temperature is given as 350 °C (662 °F).[10][11]However, calcination to the oxide is generally not considered complete below 900 °C due to interfering readsorption of liberated carbon dioxide.
The hydrates of the salts lose water at different temperatures during decomposition.[12] For example, in the trihydrateMgCO3·3H2O, which molecular formula may be written asMg(HCO3)(OH)·2H2O, the dehydration steps occur at 157 °C and 179 °C as follows:[12]
Mg(HCO3)(OH)·2(H2O) → Mg(HCO3)(OH)·(H2O) + H2O at 157 °C
Because of its low solubility in water andhygroscopic properties,MgCO3 was first added totable salt (NaCl) in 1911 to make it flow more freely. TheMorton Salt company adopted the slogan "When it rains it pours", highlighting that its salt, which containedMgCO3, would not stick together in humid weather.[13]
ClimberJan Hojer blows surpluschalk from his hand. Boulder World Cup 2015
Recent developments in sports chalk manufacturing have explored the differences between naturally mined and laboratory-synthesized forms of magnesium carbonate. Laboratory-produced MgCO₃ is created through controlled precipitation of purified magnesium salts and carbonate compounds, producing higher-purity material with fewer mineral impurities than mined magnesite.[14][15] Manufacturers of specialty grip chalks have reported that such refined magnesium carbonate reduces skin irritation and provides a more consistent moisture-absorption profile during athletic use.[16]
As afood additive, magnesium carbonate is known as E504. Its only known side effect is that it may work as a laxative in high concentrations.[17]
Magnesium carbonate is used intaxidermy for whitening skulls. It can be mixed withhydrogen peroxide to create a paste, which is spread on the skull to give it a white finish.
In addition, high purity magnesium carbonate is used as anantacid and as an additive intable salt to keep it free flowing. Magnesium carbonate can do this because it does not dissolve in water, only in acid, where it willeffervesce (bubble).[19]
^Bénézeth, Pascale; Saldi, Giuseppe D.; Dandurand, Jean-Louis; Schott, Jacques (2011). "Experimental determination of the solubility product of magnesite at 50 to 200 °C".Chemical Geology.286 (1–2):21–31.Bibcode:2011ChGeo.286...21B.doi:10.1016/j.chemgeo.2011.04.016.
^J.R. Partington (1951).General and inorganic chemistry, 2nd ed.
^abAllf, Bradley (21 May 2018)."The Hidden Environmental Cost of Climbing Chalk".Climbing Magazine. Cruz Bay Publishing. Retrieved22 May 2018.In fact, China produces 70 percent of the world's magnesite. Most of that production—both mining and processing—is concentrated in a small corner of Liaoning, a hilly industrial province in northeast China between Beijing and North Korea.
^Allf, Bradley (21 May 2018)."The Hidden Environmental Cost of Climbing Chalk".Climbing Magazine. Cruz Bay Publishing. Retrieved7 November 2025.Most climbing chalks consist of magnesium carbonate (MgCO₃), often derived from mined magnesite deposits in China.
^"The Cold, Dusty Truth About CaCO₃ vs. MgCO₃".Gym Blow Blog. Gym Blow. 13 April 2025. Retrieved7 November 2025.Gym Blow describes its lab-synthesized magnesium carbonate as being produced from purified magnesium salts and carbonate compounds to remove impurities and improve consistency.