Concentration, Oxidation and Reduction — Core Principles
Core Principles
Metal extraction from ores begins with Concentration, which removes unwanted impurities (gangue). Methods include hydraulic washing (density difference), magnetic separation (magnetic properties), froth flotation (wetting properties, for sulfide ores), and leaching (chemical dissolution, for Al, Au, Ag).
After concentration, the ore often undergoes Oxidation to convert it into a more reducible form, typically an oxide. This involves Roasting (heating sulfide ores in air to form oxides and ) or Calcination (heating carbonate/hydrated ores in limited air to remove or , forming oxides).
The final major step is Reduction, where the metal oxide is converted to pure metal. Common reduction methods include Smelting (reduction with carbon, often with a flux to form slag), Reduction by other metals (e.
g., aluminium in thermite process), Auto-reduction (self-reduction of partially roasted sulfide ores), and Electrolytic reduction (for highly reactive metals like Al, Na, Mg). Each step is chosen based on the specific ore and metal properties.
Important Differences
vs Calcination
| Aspect | This Topic | Calcination |
|---|---|---|
| Presence of Air/Oxygen | Roasting: Carried out in the presence of excess air or oxygen. | Calcination: Carried out in the absence or limited supply of air/oxygen. |
| Type of Ore Treated | Roasting: Primarily used for sulfide ores (e.g., $ZnS, PbS, Cu_2S$). | Calcination: Primarily used for carbonate ores (e.g., $CaCO_3, MgCO_3$) and hydrated oxide ores (e.g., $Al_2O_3 cdot 2H_2O$). |
| Volatile Products | Roasting: Produces gaseous oxides like $SO_2$ (from sulfur impurities), $As_2O_3$, etc. | Calcination: Produces gaseous oxides like $CO_2$ (from carbonates) or $H_2O$ (from hydrated oxides). |
| Chemical Change | Roasting: Involves oxidation of the ore, often converting sulfide to oxide. | Calcination: Involves thermal decomposition, removing volatile components without necessarily changing the oxidation state of the metal (e.g., $Ca^{2+}$ remains $Ca^{2+}$). |