Precipitation from Homogeneous Solution
Precipitation from
homogeneous solution is a technique in which a precipitating agent is generated
in a solution of the analyte by a slow chemical reaction. Local reagent
excesses do not occur because the precipitating agent appears gradually and
homogeneously throughout the solution and reacts immediately with the analyte.
As a result, the relative supersaturation is kept low during the entire
precipitation. In general, homogeneously formed precipitates, both colloidal
and crystalline, are better suited for analysis than a solid formed by direct
addition of a precipitating reagent.
e.g.Two precipitates of PbCrO4 are
shown in this photo. The precipitate in the beaker on the left was formed by
pouring quickly a solution 0.1 M Pb(NO3)2 into a solution
of 0.1 M K2CrO4. The precipitate forms rapidly and
consists of very small particles. The precipitate in the beaker on the right
was formed by heating a solution of 0.1 M Pb(NO3)2, 0.1 M
Cr(NO3)3, and 0.1 M KBrO3. Under these
conditions, the slow oxidation of Cr3+ to CrO42– results
in a precipitate that forms slowly and consists of much larger particles. This
latter process is called homogeneous precipitation, which generally results in
a precipitate that is easier to isolate by filtration and that has fewer
impurities.
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