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Magnesite MgCO

Magnesium oxide. The natural minerals, i.e., magnesite (MgCO ), brucite [Mg(OH)9], etc., after being crushed to predetermined size, are calcined at temperatures varying from 1055 to 2000 K, depending upon whether a caustic or a dead-burned produc t (periclase) is being... [Pg.1207]

Carbonates Aragonite CaCOs, calcite CaCOs, cerussite PbCOs, magnesite MgCOs, strontianite SrCOs, witherite BaCOs... [Pg.7]

Figsch V., Bunanova E. Synthesis of spinel-magnesia ceramics from finely milled mixtures of magnesite MgCOs and gibbsite Al(OH)j. In Book of Abstract I Int. Conf. INCOME, Kosice, 23-26 March,1993... [Pg.138]

Magnesium Brines, seawater magnesite [MgCOs] A1 alloys die casting... [Pg.4697]

Magnesium has a high chemical reactivity, and for this reason it is never found in nature in its free state but rather in compounds—as chloride in seawater and in salt deposits such as carnallite (MgCl2 KCl - 6H2O) and as carbonates in the ores dolomite (MgCOs CaCOs) and magnesite (MgCOs), etc. [Pg.520]

Chlorination of magnesia (MgO) or magnesite (MgCOs) in the presence of carbon or carbon monoxide... [Pg.521]

Magnesium oxide (MgO, magnesia) occurs naturally as the mineral periclase, a metamorphic mineral formed by the breakdown of dolomite, CaMg(C03)2, and other magnesium minerals. Occurrences of periclase are rare and are of no commercial importance. The principal commercial sources of MgO are magnesite (MgCOs) and magnesium hydroxide [Mg(OH)2]. [Pg.352]

See other pages where Magnesite MgCO is mentioned: [Pg.164]    [Pg.109]    [Pg.368]    [Pg.369]    [Pg.511]    [Pg.518]    [Pg.518]    [Pg.530]    [Pg.299]    [Pg.134]    [Pg.57]    [Pg.62]    [Pg.32]    [Pg.58]    [Pg.500]    [Pg.3490]    [Pg.394]    [Pg.427]    [Pg.484]    [Pg.698]    [Pg.46]    [Pg.206]    [Pg.218]    [Pg.194]    [Pg.218]    [Pg.5]    [Pg.135]    [Pg.539]    [Pg.60]    [Pg.215]    [Pg.549]    [Pg.777]    [Pg.785]    [Pg.769]    [Pg.777]    [Pg.17]    [Pg.168]    [Pg.218]    [Pg.479]    [Pg.26]   
See also in sourсe #XX -- [ Pg.3 , Pg.26 , Pg.352 ]

See also in sourсe #XX -- [ Pg.3 , Pg.26 , Pg.352 ]



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