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Engineering applications are to be found in diverse areas such as analysis of electrical networks, conduction of heat in solids, solution of partial differential equations by finite difference finite element methods.
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This phenomenon is termed ionic substitution, or solid solution.
Substitutional solid solution is the most common variety.
The least common type of solid solution is omission solid solution, in which a crystal contains one or more atomic sites that are not completely filled.
The alkali (Or-Ab) series exhibits complete solid solution at high temperatures but only incomplete solid solution at low temperatures; substitution of potassium for sodium is involved.
The aragonite group displays more limited solid solution than the calcite group.
The second major type of ionic substitution is interstitial solid solution, or interstitial substitution.
Only a mineral that displays no solid solution may therefore be considered a phase.
This provides a way to tailor the properties of the solid solution for specific applications.
Ferrosilite, silicate mineral (Fe2Si2O6) and iron-rich end member of the orthopyroxene solid solution series.
Simple cationic or anionic substitutions are the most basic types of substitutional solid solution.
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