The Principles of Chemistry, Volume IIMendeleyev, Dmitry Ivanovich
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The Principles of Chemistry, Volume II
Mendeleyev, Dmitry Ivanovich
Argon; Chemistry; Periodic law
The Deville method for the preparation of metallic aluminium is
based on the decomposition of the above-mentioned compound of
sodium and aluminium chlorides by metallic sodium. The compound is
obtained by passing the vapour of aluminium chloride (evolved from
a mixture of alumina, extracted from bauxite or cryolite, with
charcoal ignited in a stream of chlorine) over red-hot salt, when
the compound AlNaCl_{4}, is itself volatilised, and may in this
manner be obtained pure. A mixture of this compound with salt and
fluor spar, or with cryolite, is heated with a certain excess of
sodium, cut into small lumps. On a large scale this operation is
carried on in special furnaces with a small access of air and at a
high temperature. The decomposition takes place chiefly according
to the equation NaAlCl_{4} + 3Na = 4NaCl + Al. Neither charcoal
nor zinc will reduce the oxygen compounds of aluminium; even
sodium and potassium do not act on alumina. Moreover, metallic
aluminium, like magnesium, is able to reduce even the metals of
the alkalis from their oxygen compounds. This is connected with
the fact that the atom of oxygen evolves more heat in combining
with Al (and Mg) than it does in combining with other metals;
whilst on the other hand, chlorine (and the other halogens) evolve
more heat in combining with the metals of the alkalis.[36 tri]
[36 tri] In addition to the data given in Chapters XI., XIII., and
in Chapter XV., Note 19, the following are the amounts of heat in
thousands of units, evolved in the formation of the oxides and
chlorides from the metals taken in gram-atomic quantities:
Na_{2}O 100; MgO 140*; 1/3Al_{2}O_{3} 120*;
1/3Fe_{2}O_{3} 63*;
Na_{2}Cl_{2} 195; MgCl_{2} 151; 1/3Al_{2}Cl_{6} 107;
1/3Fe_{2}Cl_{6} 64.
The asterisks following the oxides of Mg, Al and Fe call attention
to the fact that the existing data refer to the formation of the
hydrates of these metals, from which the heat of formation of the
anhydrous oxides may easily be assumed, because the heat of
hydration (for example, MgO + H_{2}O) has not yet been determined.
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