
This is the most important ferrous salt. It is also called green vitriol. We also call it as copperas because it is a by product of the hydrometallurgy of copper. In the laboratory it is prepared: (i)By dissolving iron in dil. H2SO4filtering, evaporating and crystallizing.
Fe + H2SO4 → FeSO4+ H2
(ii)From Kipp’s waste: Kipp’s waste (or residue) contains FeSO4along with free H2SO4. The waste is heated with a small quantity of scrap iron which reacts with excess of H2S to give FeSO4and nascent hydrogen. This nascent hydrogen reduces any ferric iron, if present, to ferrous state. On allowing the hot solution to stand, crystals of FeSO4.7H2O separate out. On a large scale it is obtained by the slow oxidation of iron pyrites in the presence of air and moisture. The pyrites are exposed to air in big heaps and the following reaction takes place.
2FeS2 + 2H2O + 7O2 → 2FeSO4+ 2H2SO4
The free H2SO4is removed by the addition of scrap iron, which also reduces any ferric sulphate formed. On crystallization we get green coloured crystals containing seven molecules of water of crystallization. These crystals are monoclinic and are isomorphous with MgSO4.7H2O. Ferrous sulphate containing 6, 5, 3, 2, 1 molecules and no water of crystallization is also known.
