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Brucite is the form of magnesium hydroxide, with the chemical formula ()2. It is a common alteration product of in ; a low-temperature vein mineral in metamorphosed and ; and formed during of . Brucite is often found in association with , , , dolomite, , , , and .

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


Discovery
Brucite was first described in 1824 by François Sulpice Beudant 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 .


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 of Wadh, , 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.


Industrial applications
Synthetic brucite is mainly consumed as a precursor to (MgO), a useful and thermal insulator. It finds some use as a because it thermally decomposes to release water in a similar way to aluminium hydroxide () and mixtures of () and (). It also constitutes a significant source of magnesium for industry. Although generally deemed safe, brucite can be contaminated with naturally occurring fibers.


Degradation of cement and concrete
When or are exposed to and ions simultaneously present in , the precipitation of the poorly brucite contributes to enhance the formation of in the sulfate attack :

The precipitation of insoluble helps to considerably drive the chemical equilibrium of the reaction to the right. It exacerbates the sulfate attack resulting in the formation of and (an expansive phase) responsible for the mechanical stress in the hardened cement paste. However, brucite, a phase with a small (), may contribute to clogging the porous network in the hardened cement paste, hindering the diffusion of these harmful reactive species in the cement matrix. This can delay the decalcification of the C-S-H phase (the "glue" phase in the hardened cement paste responsible for the cohesion in concrete) and its transformation into an M-S-H phase.

The exact mechanism of brucite degradation of hardened cement paste remains a matter of debate. If brucite had a high molar volume, it could be de facto considered a swelling phase (like , or highly hydrated minerals), but this does not appear to be the case. It is unclear if it causes expansion or not, and how. If it replaces another phase locally (topo chemical replacement), in cases where its molar volume is smaller than that of the phase it replaces, no expansion is expected; rather, a decrease in is anticipated. However, if it crystallizes in a large number of tiny crystals growing between existing ones, even with a small molar volume, it could exert a considerable crystallization pressure in the cement matrix, resulting in tensile stress, expansion and cracking.

Anyway, prolonged contact between , or naturally rich Mg-, and concrete may induce durability issues for regularly immersed concrete structures, and their components, especially if they also contain (pitting corrosion caused by ions).

The use of dolomite as aggregate in concrete made with a cement with a too high alkali content can also cause brucite precipitation, driving the dedolomitization reaction, as observed in the alkali-aggregate reaction.

Consequently, the use of dolomite is prohibited as aggregate for concrete.

== Gallery ==


See also


Further reading
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