Sunday, 23 October 2016

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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