Iron oxides Nonstoichiometry is pervasive for
metal oxides, especially when the metal is not in its highest
oxidation state. For example, although
wüstite (
ferrous oxide) has an ideal (
stoichiometric) formula , the actual stoichiometry is closer to . The non-stoichiometry reflect the ease of oxidation of {{chem2|Fe^{2+} }} to {{chem2|Fe^{3+} }} effectively replacing a small portion of {{chem2|Fe^{2+} }} with two thirds their number of {{chem2|Fe^{3+} }}. Thus for every three "missing" {{chem2|Fe^{2+} }} ions, the crystal contains two {{chem2|Fe^{3+} }} ions to balance the charge. The composition of a non-stoichiometric compound usually varies in a continuous manner over a narrow range. Thus, the formula for wüstite is written as {{chem2|Fe_{1−
x}O}}, where
x is a small number (0.05 in the previous example) representing the deviation from the "ideal" formula. Nonstoichiometry is especially important in solid, three-dimensional polymers that can tolerate mistakes. To some extent, entropy drives all solids to be non-stoichiometric. But for practical purposes, the term describes materials where the non-stoichiometry is measurable, usually at least 1% of the ideal composition.
Iron sulfides , with formula {{chem2|Fe_{1−
x}S}} (
x = 0 to 0.2) The monosulfides of the transition metals are often nonstoichiometric. Best known perhaps is nominally iron(II) sulfide (the mineral
pyrrhotite) with a composition {{chem2|Fe_{1−
x}S}} (
x = 0 to 0.2). The rare stoichiometric
endmember is known as the mineral
troilite. Pyrrhotite is remarkable in that it has numerous
polytypes, i.e. crystalline forms differing in symmetry (
monoclinic or
hexagonal) and composition (, , and others). These materials are always iron-deficient owing to the presence of lattice defects, namely iron vacancies. Despite those defects, the composition is usually expressed as a ratio of large numbers and the crystals symmetry is relatively high. This means the iron vacancies are not randomly scattered over the crystal, but form certain regular configurations. Those vacancies strongly affect the magnetic properties of pyrrhotite: the magnetism increases with the concentration of vacancies and is absent for the stoichiometric .
Palladium hydrides Palladium hydride is a nonstoichiometric material of the approximate composition {{chem2|PdH_{
x} }} (0.02 <
x < 0.58). This solid conducts hydrogen by virtue of the mobility of the hydrogen atoms within the solid.
Tungsten oxides It is sometimes difficult to determine if a material is non-stoichiometric or if the formula is best represented by large numbers. The oxides of tungsten illustrate this situation. Starting from the idealized material
tungsten trioxide, one can generate a series of related materials that are slightly deficient in oxygen. These oxygen-deficient species can be described as {{chem2|WO_{3−
x} }}, but in fact they are stoichiometric species with large unit cells with the formulas {{chem2|W_{
n}O_{3
n−2} }}, where
n = 20, 24, 25, 40. Thus, the last species can be described with the stoichiometric formula , whereas the non-stoichiometric description implies a more random distribution of oxide vacancies.
Other cases At high temperatures (1000 °C),
titanium sulfides present a series of non-stoichiometric compounds. The non-stoichiometric phases exhibit useful properties vis-à-vis their ability to bind
caesium and
thallium ions. ==Applications==