Any substance consisting of two or more different types of
atoms (
chemical elements) in a fixed
stoichiometric proportion can be termed a
chemical compound; the concept is most readily understood when considering pure
chemical substances. It follows from their being composed of fixed proportions of two or more types of atoms that chemical compounds can be converted, via
chemical reaction, into compounds or substances each having fewer atoms. A
chemical formula is a way of expressing information about the proportions of atoms that constitute a particular chemical compound, using
chemical symbols for the chemical elements, and
subscripts to indicate the number of atoms involved. For example,
water is composed of two
hydrogen atoms bonded to one
oxygen atom: the chemical formula is H2O. In the case of
non-stoichiometric compounds, the proportions may be reproducible with regard to their preparation, and give fixed proportions of their component elements, but proportions that are not integral [e.g., for
palladium hydride, PdHx (0.02 2, or the
polyatomic molecule S8, etc.). Many
chemical compounds have a unique numerical identifier assigned by the
Chemical Abstracts Service (CAS): its
CAS number. There is varying and sometimes inconsistent nomenclature differentiating substances, which include truly non-stoichiometric examples, from chemical compounds, which require the fixed ratios. Many solid chemical substances—for example many
silicate minerals—are chemical substances, but do not have simple formulae reflecting chemical bonding of elements to one another in fixed ratios; even so, these
crystalline substances are often called "
non-stoichiometric compounds". It may be argued that they are related to, rather than being chemical compounds, insofar as the variability in their compositions is often due to either the presence of foreign elements trapped within the crystal structure of an otherwise known true
chemical compound, or due to perturbations in structure relative to the known compound that arise because of an excess or deficit of the constituent elements at places in its structure; such non-stoichiometric substances form most of the
crust and
mantle of the Earth. Other compounds regarded as chemically identical may have varying amounts of heavy or light
isotopes of the constituent elements, which changes the ratio of elements by mass slightly. == Types ==