
1.22
Most of the substances we encounter are either chemical com-
pounds or mixtures. The difference between the two is that a compound
is formed when there is a chemical join at the surfaces of two or more
different atoms, whilst in a mixture only mechanical 'entangling' occurs
between discrete particles of the two substances. For example, the pow-
dered element sulphur can be mixed with iron filings and easily separated
again by means of a magnet, but if the mixture is gently heated a vigorous
chemical reaction proceeds and a compound called iron sulphide is formed.
This is different in appearance from either of the parent elements and its
decomposition into the parent elements, sulphur and iron, is now more
difficult and can be accomplished only be chemical means.
1.23 Chemical elements can be represented by a symbol which is usu-
ally an abbreviation of either the English or Latin name, eg O stands
for oxygen whilst Fe stands for 'ferrum', the Latin equivalent of iron'.
Ordinarily, a symbol written thus refers to a single atom of the element,
whilst two atoms (constituting what in this instance we call a molecule)
would be indicated so: O2.
1.24 Table 1.1 includes some of the more important elements we are
likely to encounter in a study of metallurgy. The term 'relative atomic
mass',
(formerly 'atomic weight'), mentioned in this table must not be con-
fused with the relative density of the element. The latter value will depend
upon how closely the atoms, whether small or large, are packed together.
Since atoms are very small particles (the mass of the hydrogen atom is
1.673 x 10~
27
kg), it would be inconvenient to use such small values in
everyday chemical calculations. Consequently, since the hydrogen atom
was known to be the smallest, its relative mass was taken as unity and the
relative masses of the atoms of other elements calculated as multiples of
this.
Thus relative atomic mass became
mass of one atom of the element
mass of one atom of hydrogen
Later it was found more useful to adjust the relative atomic mass of oxygen
(by far the most common element) to exactly 16.0000. On this basis the
relative atomic mass of hydrogen became 1.008 instead of
1.0000.
More
recently chemists and physicists have agreed to relate atomic masses to
that of the carbon isotope (C = 12.0000). (See paragraph
1.90.)
1.25 The most common metallic element in the Earth's crust is alu-
minium (Table 1.2) but as a commercially usable metal it is not the cheap-
est. This is because clay, the most abundant mineral containing aluminium,
is very difficult—and therefore costly—to decompose chemically. There-
fore our aluminium supply comes from the mineral bauxite (originally
mined near the village of Les Baux, in France), which is a relatively scarce
ore.
It will be seen from the table that apart from iron most of the useful
metallic elements account for only a very small proportion of the Earth's
crust. Fortunately they occur in relatively concentrated deposits which
makes their mining and extraction economically possible.
In passing it is interesting to note that in the Universe as a whole hydro-