Inorganic chemistry

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Inorganic chemistry is a subdiscipline of chemistry involving the scientific study of the properties and reactions of all chemical elements and chemical compounds other than the vast number of organic compounds (compounds containing at least one carbon-hydrogen chemical bond).[1][2]

There are a number of subdivisions of inorganic chemistry such as the four subdivisions of the American Chemical Society's Division of Inorganic Chemistry, namely organometallic chemistry, bioinorganic chemistry, solid-state chemistry and nanoscience.[3]

Inorganic chemistry is closely related to other disciplines such as materials science, earth science, mineralogy, geology and crystallography.

Distinctions between inorganic and organic chemistry

The distinction or boundary between inorganic chemistry and organic chemistry is not very well defined. In general, the above definition of inorganic chemistry seemingly excludes carbon compounds but it does not exclude elemental carbon itself. Hence, carbon oxides, carbon sulfides, cyanides and cyanates, metallic carbides and carbonates are included as inorganic compounds.[4]

As another example of the ill-defined distinction between inorganic and organic chemistry, oxalic acid (H2C204) is commonly considered to be an organic compound even though it does not contain a carbon-hydrogen bond.

Types of inorganic compounds

Inorganic chemistry encompasses a very complicated variety of substances which the distinguished American chemist, F. Albert Cotton (1930 − 2007), grouped into these four classes:[5]

The chemical elements: These have a variety of structure and properties and include:

Ionic compounds: These are always solids at reference conditions of 0 °C temperature and 101.325 kPa absolute pressure and include:

Molecular compounds: These may be solids, liquids or gases and include:

Inorganic polymers and superconductors: These include numerous and varied inorganic polymers and superconductors. One example of an inorganic polymer has the chemical formula of YBa2Cu3O7.

Typical inorganic chemical reactions




Analysis and characterization of inorganic compounds

The number of known chemical elements that occur naturally on Earth is 94 and the number of diverse inorganic chemical compounds derived by combinations of those elements is virtually innumerable. The characterization of those compounds includes the measurement of chemical and physical properties such as boiling points, melting points, density, solubility, refractive index and the pH and electrical conductivity of solutions.

The techniques of qualitative and quantitative analytical chemistry can provide the composition of a chemical compound in terms of its constituent chemical elements and can thus determine the chemical formula of a compound.

Modern laboratory equipment and techniques can provide many more details for characterizing chemical compounds. Some of the more commonly used modern techniques are:

References

  1. Inorganic Chemistry: A Study Guide From the website of the University of Waterloo, Canada
  2. Christopher G. Morris (Editor) (1992). Academic Press Dictionary of Science and Technology, 1st Edition. Academic Press. ISBN 0-12-200400-0. 
  3. Division of Inorganic Chemistry, 2010 Officers From the website of the American Chemical Society
  4. Note: For example, carbon monoxide (CO), carbon dioxide (CO2), carbon disulfide (CS2), sodium cyanide (NaCN), potassium cyanate (KOCN), silicon carbide (SiC) and calcium carbonate (CaCO3)
  5. F. Albert Cotton, Geoffrey Wilkinson and Paul L. Gaus (1995). Basic Inorganic Chemistry, 3rd Edition. John Wiley. ISBN 0-471-50532-3.  First published in 1976 with Professor F. Albert Cotton of Texas A and M University as the main author.
  6. Note: Allotropes are molecules having different molecular structures. This differs from isotopes which are elements having different atomic structures (i.e., the same number of protons but different numbers of neutrons in the atomic nucleus.
  7. Note: Network solids are chemical compounds with the atoms being bonded by covalent bonds in a continuous network. Thus, there are no individual molecules in a network solid and the entire solid may be considered to be a macromolecule. Diamond is an example of a network solid with a continuous network of carbon atoms. Another example is graphite, which consists of continuous two dimensional layers of carbon atoms covalently bonded within each layer and with other bond types holding the layers together.