Chemistry:Brucite

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Short description: Magnesium hydroxide mineral
Brucite
Brucite-231242.jpg
General
CategoryOxide mineral
Formula
(repeating unit)
Mg(OH)2
Strunz classification4.FE.05
Crystal systemTrigonal
Crystal classHexagonal crystal family (3m)
H-M symbol: (3 2/m)
Space groupP3m1
Unit cella = 3.142(1) Å, c = 4.766(2) Å; Z = 1
Identification
ColorWhite, pale green, blue, gray; honey-yellow to brownish red
Crystal habitTabular crystals; platy or foliated masses and rosettes – fibrous to massive
CleavagePerfect on {0001}
FractureIrregular
TenacitySectile
Mohs scale hardness2.5 to 3
|re|er}}Vitreous to pearly
StreakWhite
DiaphaneityTransparent
Specific gravity2.39 to 2.40
Optical propertiesUniaxial (+)
Refractive indexnω = 1.56–1.59
nε = 1.58–1.60
Birefringence0.02
Other characteristicsPyroelectric
References[1][2][3]

Brucite is the mineral form of magnesium hydroxide, with the chemical formula Mg(OH)2. It is a common alteration product of periclase in marble; a low-temperature hydrothermal vein mineral in metamorphosed limestones and chlorite schists; and formed during serpentinization of dunites. Brucite is often found in association with serpentine, calcite, aragonite, dolomite, magnesite, hydromagnesite, artinite, talc and chrysotile.

It adopts a layered CdI2-like structure with hydrogen-bonds between the layers.[5]

Discovery

Brucite was first described in 1824 by François Sulpice Beudant[6] and named for the discoverer, American mineralogist, Archibald Bruce (1777–1818). A fibrous variety of brucite is called nemalite. It occurs in fibers or laths, usually elongated along [1010], but sometimes [1120] crystalline directions.

Occurrence

A notable location in the US is Wood's Chrome Mine, Cedar Hill Quarry, Lancaster County, Pennsylvania. Yellow, white and blue brucite with a botryoidal habit was discovered in Qila Saifullah District of Province Baluchistan, Pakistan. In a later discovery, brucite also occurred in the Bela Ophiolite of Wadh, Khuzdar District, Province Baluchistan, Pakistan. Brucite has also occurred from South Africa, Italy, Russia, Canada, and other localities as well, but the most notable discoveries are the US, Russian and Pakistani examples.[citation needed]

Industrial applications

Synthetic brucite is mainly consumed as a precursor to magnesia (MgO), a useful refractory and thermal insulator. It finds some use as a flame retardant because it thermally decomposes to release water in a similar way to aluminium hydroxide (Al(OH)
3
) and mixtures of huntite (Mg
3
Ca(CO
3
)
4
) and hydromagnesite (Mg
5
(CO
3
)
4
(OH)
2
 · 4H2O
).[7][8] It also constitutes a significant source of magnesium for industry. Although generally deemed safe, brucite can be contaminated with naturally occurring asbestos fibers.[9]

Magnesium attack of cement and concrete

When cement or concrete are exposed to Mg2+, the neoformation of brucite, an expansive material, may induce mechanical stress in the hardened cement paste or may clog the porous network creating a buffering effect[clarification needed] and delaying the alteration/transformation of the C-S-H phase (the "glue" phase in the hardened cement paste) into M-S-H phase (a non-cohesive mineral phase). The exact magnitude of impact that brucite has on cement paste is still debatable. Prolonged contact between sea water or brines and concrete may induce durability issues for regularly immersed concrete components or structures.

The use of dolomite as aggregate in concrete can also cause magnesium attack and should be avoided.[10]

Gallery

See also

References

  1. Brucite on Mindat.org
  2. Handbook of Mineralogy
  3. Brucite on Webmineral
  4. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode2021MinM...85..291W. https://www.cambridge.org/core/journals/mineralogical-magazine/article/imacnmnc-approved-mineral-symbols/62311F45ED37831D78603C6E6B25EE0A. 
  5. Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8. 
  6. "Blog | GeoRarities" (in en). 2021-01-13. https://georarities.com/blog/. 
  7. Hollingbery, LA; Hull TR (2010). "The Thermal Decomposition of Huntite and Hydromagnesite - A Review". Thermochimica Acta 509 (1–2): 1–11. doi:10.1016/j.tca.2010.06.012. http://clok.uclan.ac.uk/1139/. 
  8. Hollingbery, LA; Hull TR (2010). "The Fire Retardant Behaviour of Huntite and Hydromagnesite - A Review". Polymer Degradation and Stability 95 (12): 2213–2225. doi:10.1016/j.polymdegradstab.2010.08.019. http://clok.uclan.ac.uk/1432. 
  9. Malferrari, Daniele; Di Guisseppe, Dario; Scognamiglio, Valentina; Gualtieri, Alessandro F. (2021). "Commercial brucite, a worldwide used raw material deemed safe, can be contaminated by asbestos". Periodico di Mineralogia 90 (3): 317–324. doi:10.13133/2239-1002/17384. https://rosa.uniroma1.it/rosa04/periodico_di_mineralogia/article/view/17384. 
  10. Lee, Hyomin; Cody, Robert D.; Cody, Anita M.; Spry, Paul G. (1 May 2002). "Observations on brucite formation and the role of brucite in Iowa highway concrete deterioration". Environmental and Engineering Geoscience 8 (2): 137–145. doi:10.2113/gseegeosci.8.2.137. ISSN 1078-7275. Bibcode2002EEGeo...8..137L. https://doi.org/10.2113/gseegeosci.8.2.137. 

Further reading