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 covalent 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.

Classification 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

There is no universally accepted list of the typical, important inorganic reactions. Although there are numerous available sources (books, journal and Internet websites) that include such lists, they all differ to some extent from each other. The inorganic reaction types listed and explained below were drawn from many of the available sources:[5][8][9][10][11]

Synthesis reaction: (also referred to as combination or composition reaction)

This is a reaction in which two or more reactants combine to form a single product, where each reactant is a chemical element or compound and the reaction product consist of the two reactants. Examples include:

2Na + Cl2 → 2NaCl
CO2 + H2O → H2CO3
H2 + S → H2S

Decomposition reaction: (may be thermal, electrolytic or catalytic decomposition reaction)

This is a reaction in which a chemical compound is separated into elements or simpler compounds. It is often defined as being the opposite of a synthesis reaction. Examples include:

  • hydrogen peroxide → water + oxygen     (Hydrogen peroxide spontaneously decomposes into water and gaseous oxygen.)
2H2O2 → 2H2O + O2
CaCO3 + heat → CaO + CO2

Single displacement reaction: (also referred to as substitution or single replacement reaction)

This is a reaction characterized by one element being displaced from a compound by another element. Examples include:

Cu + 2HCl → CuCl2 + H2
Zn + CuSO4 → Cu + ZnSO4

Metathesis reaction: (also referred to as exchange or double displacement or double replacement reaction)

This is a reaction in which two compounds exchange bonds or ions to form new, different compounds. Examples include:

Na2SO4 + BaCl2 → BaSO4 + 2NaCl
AgNO3 + HCl → HNO3 + AgCl

Precipitation reaction: (a specific type of metathesis referred to as aqueous metathesis)

This is a reaction that occurs when two inorganic salt solutions, as in the example below, react to form a solution containing a soluble product and another product that is insoluble and precipitates out of the solution:

CaCl2 (aq) + 2AgNO3 (aq) → Ca(NO3)2 (aq) + 2AgCl (s)

Neutralization reaction: (another specific type of metathesis that is sometimes referred to as an acid-base reaction)

This is a reaction in which an acid and a base react to form a salt. Water is also produced in neutralizations with Arrhenius acids, which dissociate in aqueous solution to form hydrogen ions (H +), and Arrhenius bases, which form hydroxide ions (OH). However, water is not produced in all neutralizations as is the case with ammonia. Examples include:

HNO3 + NaOH → NaNO3 + H2O
HCl + NH3 → NH4Cl

Redox reaction: (also referred to as oxidation-reduction reaction)

This is a reaction in which the oxidation numbers of atoms are changed. Examples include:

H2 + F2 → 2HF

    Hydrogen is oxidized by its oxidation number increasing from zero to +1. Fluorine is reduced by its oxidation number decreasing from zero to -1.

Fe + CuSO4 → FeSO4 + Cu

    Iron is oxidized by its oxidation number increasing from zero to +2. Copper is reduced by its oxidation number decreasing from +2 to zero.

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:


  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. 5.0 5.1 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.
  8. P.A. Cox (2004). Inorganic Chemistry, 2nd Edition. Taylor & Francis. ISBN 1-85996-289-0. 
  9. Types of Equations From the website of the Virginia Polytechnic Institute and State University (Virginia Tech). A list of many similar, excellent chemistry articles are available here.
  10. Types of Inorganic Chemical Reactions By Dr. Anne Marie Helmenstine on the website of Chemistry.
  11. Types of Chemical Reactions By Dr. Anne Marie Helmenstine on the website of Chemistry.