|Preferred IUPAC name
3D model (Jmol)
|Molar mass||76.69 g·mol−1|
|Density||1.988 g cm−3|
|Melting point||1,102 °C (2,016 °F; 1,375 K)|
|Main hazards||reacts with water to give silane|
|R-phrases||R23, R24, R25, R34|
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
|what is ?)(|
It can be produced by heating silicon dioxide, SiO2, found in sand, with excess magnesium. The process first forms silicon metal and magnesium oxide, and, if an excess of magnesium is used, the silicide is formed:
- 2 Mg + SiO2 → 2 MgO + Si
If an excess of Mg is present, Mg2Si is formed from the reaction of the remaining magnesium with the silicon:
- 2 Mg + Si → Mg2Si
These reactions proceed exothermically.
Magnesium silicide is used to create aluminium alloys of the 6000 series, containing up to approximately 1.5% Mg2Si. An alloy of this group can be age-hardened to form Guinier-Preston zones and a very fine precipitate, both resulting in increased strength of the alloy.
- Mg2Si + 4 HCl → SiH4 + 2 MgCl2
Mg2Si crystallizes in the antifluorite structure. In the face-centered cubic lattice Si centers occupy the corners and face-centered positions of the unit cell and Mg centers occupy eight tetrahedral sites in the interior of the unit cell. The coordination numbers of Si and Mg are eight and four, respectively.
- P. Ehrlich "Alkaline Earth Metals" in Handbook of Preparative Inorganic Chemistry, 2nd Ed. Edited by G. Brauer, Academic Press, 1963, NY. Vol. 1. p. 920.
- ASM Handbook, 10th Ed., Vol. 1, Properties and Selection: Non-ferrous Alloys and Special Purpose Materials, 1990, ASM International, Materials Park, Ohio.
- A. Kato et al. J. Phys: Condens. Matter 21 (2009) 205801.