Analyte is converted to a sparingly solubleprecipitate
Precipitate is filtered, washed free of impurities, and converted to a product of known composition by suitable heat treatment
The product is weighed
Volatilization methods
Analyte or its decomposition products are volatilized at a suitable temperature
The volatile product is then collected and weighed, or the mass of the product is determined indirectly from the loss in mass of the sample
Properties of an ideal precipitating reagent
Readily filtered and washed free of contaminants
Sufficiently low solubility so that no significant loss of the solid occurs during filtration and washing
Unreactive with constituents of the atmosphere
Of known composition after it is dried or, if necessary, ignited
Particle size and filterability of precipitates
Large particles are generally desirable as they are easy to filter and wash free of impurities
Colloidal particles show no tendency to settle from solution and are not easily filtered
Particles of a crystalline suspension tend to settle spontaneously and are readily filtered
Factors affecting particle size
Precipitatesolubility
Temperature
Reactantconcentrations
Rate at which reactants are mixed
Relative supersaturation
Q is the concentration of the solute at any instant and S is its equilibrium solubility
When (Q - S)/S is large, the precipitate tends to be colloidal
When (Q - S)/S is small, a crystalline solid is more likely
Formation of precipitates
1. Nucleation: a process in which a minimum number of atoms, ions, or molecules join together to produce a stable solid
2. Particle growth: further precipitation then involves a competition between additional nucleation and growth on existing nuclei
Controlling particle size for crystalline precipitates
Elevate the temperature to increase the solubility of the precipitate, dilute solutions, and slow addition of the precipitating agent with good stirring
Larger particles can also be obtained by pH control, provided the solubility of the precipitate depends on pH
Digestion of crystalline precipitates (without stirring) for some time after formation frequently yields a purer, more filterable product
Controlling particle size for colloidal precipitates
Coagulate, or agglomerate, the individual particles to give a filterable, amorphous mass that will settle out of solution
Adsorption is a process in which a substance is held on the surface of a solid
Coagulation of a colloidal suspension can often be brought about by a short period of heating, particularly if accompanied by stirring
An even more effective way to coagulate a colloid is to increase the electrolyte concentration of the solution
Peptization is a process by which a coagulated colloid returns to its dispersed state
Coprecipitation
A process in which normally soluble compounds are carried out of solution by a precipitate
Types of coprecipitation
Surfaceadsorption
Mixed-crystalformation
Occlusion
Mechanicalentrapment
Surface adsorption
A common source of coprecipitation that is likely to cause significant contamination of precipitates with large specific surface areas, coagulated colloids
Coagulation of a colloid does not significantly decrease the amount of adsorption
The net effect is the carrying down of an otherwise soluble compound as a surface contaminant
Minimizing adsorbed impurities on colloids
Digestion: a process in which a precipitate is heated without stirring for an hour or more
Reprecipitation: a drastic but effective way to minimize the effects of adsorption
Mixed-crystal formation
One of the ions in the crystallattice of a solid is replaced by an ion of another element
The extent of mixed-crystal contamination is governed by the law of mass action and increases as the ratio of contaminant to analyte concentration increases
Occlusion and mechanical entrapment
Occlusion is a type of coprecipitation in which a compound is trapped within a pocket formed during rapid crystal growth
Mechanical entrapment occurs when crystals lie close together during growth
Both are at a minimum when the rate of precipitate formation is low, under conditions of low supersaturation
Digestion is often remarkably helpful in reducing these types of coprecipitation
Homogeneous precipitation
A process in which a precipitate is formed by slow generation of a precipitating reagent homogeneously throughout a solution
Homogeneously formed precipitates, both colloidal and crystalline, are better suited for analysis than a solid formed by direct addition of a precipitating reagent
Drying and ignition of precipitates
After filtration, a gravimetric precipitate is heated until its mass becomes constant
Some precipitates are also ignited to decompose the solid and form a compound of known composition, called the weighing form
Calculating results from gravimetric data
The results are generally computed from the mass of sample and the mass of a product of known composition
Calculating results from gravimetric data
Determination of Calcium in NaturalWaters
Determination of SodiumHydrogenCarbonate content of antacid tablets
Calculating results from gravimetric data - example 1
1. Step 1: Determine the mass of CaO
2. Step 2: Calculate the number of moles of Ca in the sample
3. Step 3: Calculate the concentration of Ca in the water per 100 mL
Calculating results from gravimetric data - example 2
1. Step 1: Calculate the number of moles of Fe2O3
2. Step 2: Calculate the number of moles of Fe present
3. Step 3: Calculate the %Fe present
4. Step 4: Calculate the %Fe3O4
Applications of gravimetric methods
Inorganicanions and cations
Organic substances
Do not require calibration or standardization
Inorganic precipitating agents
Form slightly solublesalts or hydrousoxides with the analyte
Not very selective
Organic precipitating agents
Coordination compounds: form slightly solublenonionic products
Ionic compounds: form products in which the bonding between the inorganicspecies and the reagent is largelyionic