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Chemistry · Ch 13 — General Principles and Processes of Isolation of Elements

Occurrence of Metals

13.1

Occurrence of Metals

Metals almost never sit around waiting to be picked up in their pure, shiny form. Only a handful of unreactive elements — carbon, sulphur, gold, and the noble gases — are found "free" in nature. Everything else is locked up in compounds inside the earth's crust, and the first job of metallurgy is figuring out which compound to dig for.

Abundance sets the stage

Metals differ enormously in how common they are:

  • Aluminium is the most abundant metal in the crust, and in fact the third most abundant element overall — roughly 8.3% by weight. It shows up as a major component of igneous minerals such as mica and clays. Even gemstones borrow it: ruby and sapphire are really impure Al2O3Al_2O_3, coloured by traces of Cr and Co respectively.
  • Iron is the second most abundant metal. Its chemistry is unusually versatile, which is why it ends up in so many compounds and so many everyday uses — and biology depends on it too (haemoglobin being the obvious example).

From mineral to ore

A mineral is simply a naturally occurring chemical substance found in the crust and won by mining. Any given metal is usually locked up in several different minerals, but only a few of them are actually worth mining — rich enough, or accessible enough, to be commercially sensible. A mineral that clears that bar is called an ore. So every ore is a mineral, but not every mineral is an ore.

Table 6.1 lists the principal ores of the four metals this chapter keeps coming back to:

MetalOresComposition
AluminiumBauxiteAlOx(OH)3−2xAlO_x(OH)_{3-2x} [0<x<10 < x < 1]
Kaolinite (a clay)[Al2(OH)4Si2O5][Al_2(OH)_4Si_2O_5]
IronHaematiteFe2O3Fe_2O_3
MagnetiteFe3O4Fe_3O_4
SideriteFeCO3FeCO_3
Iron pyritesFeS2FeS_2
CopperCopper pyritesCuFeS2CuFeS_2
MalachiteCuCO3.Cu(OH)2CuCO_3.Cu(OH)_2
CupriteCu2OCu_2O
Copper glanceCu2SCu_2S
ZincZinc blende / SphaleriteZnSZnS
CalamineZnCO3ZnCO_3
ZinciteZnOZnO

Why one ore is chosen over another

Having several candidate ores for the same metal means a choice has to be made, and that choice is driven by what's chemically feasible and commercially viable:

  • Aluminium is extracted almost exclusively from bauxite — it's abundant and the extraction route built around it (Section 6.2.4) works cleanly.
  • Iron is usually pulled from its oxide ores. They're plentiful, and — just as importantly — they don't release polluting gases the way iron pyrites does when it's roasted (roasting FeS2FeS_2 generates SO2SO_2).
  • Copper and zinc can be sourced from any of the ores in the table above, and the choice comes down to local availability and cost.

Metallurgy as an overall process

The complete scientific and industrial sequence used to pull a metal out of its ore is called metallurgy. It draws on several branches of chemistry at once, but almost every metal's extraction follows the same broad script:

  1. Concentration of the ore — stripping away the unwanted rocky material.
  2. Isolation of the metal from the concentrated ore (usually a reduction step).
  3. Purification (refining) of the isolated metal.

An ore is essentially never pure — it comes mixed with earthy, commercially worthless material called gangue, and separating gangue from the valuable mineral is where the story begins.


The sections that follow walk through this script in order: first the physical tricks used to concentrate an ore, then the thermodynamic and electrochemical reasoning behind converting the concentrate into metal.

Table 6.1Principal Ores of Some Important Metals
MetalOresComposition
AluminiumBauxiteAlOx(OH)3-2x [where 0 < x < 1]
Kaolinite (a form of clay)[Al2(OH)4Si2O5]
IronHaematiteFe2O3
MagnetiteFe3O4
SideriteFeCO3
Iron pyritesFeS2
CopperCopper pyritesCuFeS2
MalachiteCuCO3.Cu(OH)2
CupriteCu2O
Copper glanceCu2S
ZincZinc blende or SphaleriteZnS
CalamineZnCO3
ZinciteZnO