In precipitation methods, the analyte is converted to a sparingly soluble precipitate. This precipitate is then filtered, washed free of impurities, and converted to a product of known composition by suitable heat treatment, and the product is weighed
In volatilization methods, the analyte or its decomposition products are volatilized at a suitable temperature. The volatile product is then collected and weighed, or, alternatively, the mass of the product is determined indirectly from the loss in mass of the sample
Precipitates consisting of large particles are generally desirable for gravimetric work because these particles are easy to filter and wash free of impurities
The particle size of a precipitate is influenced by precipitate solubility, temperature, reactant concentrations, and the rate at which reactants are mixed
Nucleation is a process in which a minimum number of atoms, ions, or molecules join to produce a stable solid. Further precipitation then involves a competition between additional nucleation and growth on existing nuclei (particle growth)
Colloidal precipitates are so small that they tend to pass through the filter paper. The Brownian motion also prevents them from settling out of the solution under gravity
Adsorption is a process in which a substance is held on the surface of a solid. In contrast, absorption involves retention of a substance within the pores of a solid
Homogeneous precipitation is a process in which a precipitate is formed by slow generation of a precipitating reagent homogeneously throughout a solution
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
Gravimetric methods have been developed for most inorganic anions and cations as well as for such neutral species. A variety of organic substances can also be readily determined gravimetrically
Gravimetric methods do not require a calibration or standardization step because the results are calculated directly from the experimental data and molar masses
The calcium in a 200.0-mL sample of a natural water was determined by precipitating the cation as CaC2O4. Calculate the concentration of Ca in water in units of grams per 100 mL of the water