An example of a gravimetric analysis using a precipitate is the determination of chloride (Cl-) in a sample (for example, sea water). In order to perform a gravimetric analysis for chloride, a suitable cation must be found that will form an insoluble precipitate with chloride. The insoluble compound thus formed must be pure and easily filtered. The solubility rules indicate that Ag+, Pb2+, and Hg22+ all form insoluble precipitates with chlorides, so could potentially be used for the gravimetric analysis of chloride ions.
Silver cations (Ag+) would therefore be suitable for determining the percent chloride (%Cl-) in a sample. Silver forms an insoluble precipitate of known composition (AgCl) with chloride ions and it can be formed pure and is easily filtered.
Ag+(aq) + Cl-(aq) ? AgCl(s)
Hence, if you had a sample of sea water (1L) and added an excess of silver (Ag+ 107.87g.mol-1) cations to the solution a precipitate of silver chloride (AgCl 143.32g.mol-1) would form. The AgCl could then be filtered, dried and weighed. Then if the mass of AgCl you weighed was say 60.64g after it was dried, then you would know that you had 0.42 moles of AgCl and hence there must have been 0.42 moles of Cl- in the original sample, in other words the concentration of chloride in the sea water sample would be approximately 15000 mg.L-1.