Allotropy
Property of some chemical elements to exist in two or more different forms

Allotropy or allotropism (from Ancient Greek ἄλλος (allos) 'other' and τρόπος (tropos) 'manner, form') is the property of some chemical elements to exist in two or more different forms, in the same physical state, known as allotropes of the elements. Allotropes are different structural modifications of an element: the atoms of the element are bonded together in different manners. For example, the allotropes of carbon include diamond (the carbon atoms are bonded together to form a cubic lattice of tetrahedra), graphite (the carbon atoms are bonded together in sheets of a hexagonal lattice), graphene (single sheets of graphite), and fullerenes (the carbon atoms are bonded together in spherical, tubular, or ellipsoidal formations).
The term allotropy is used for elements only, not for compounds. The more general term, used for any compound, is polymorphism, although its use is usually restricted to solid materials such as crystals. Allotropy refers only to different forms of an element within the same physical phase (the state of matter, i.e. plasmas, gases, liquids, or solids). The differences between these states of matter would not alone constitute examples of allotropy. Allotropes of chemical elements are frequently referred to as polymorphs or as phases of the element.
For some elements, allotropes have different molecular formulae or different crystalline structures, as well as a difference in physical phase; for example, two allotropes of oxygen (dioxygen, O2, and ozone, O3) can both exist in the solid, liquid and gaseous states. Other elements do not maintain distinct allotropes in different physical phases; for example, phosphorus has numerous solid allotropes, which all revert to the same P4 form when melted to the liquid state.
| Feature | Isomerism (Isomers) | Allotropy (Allotropes) | Polymorphism (Polymorphs) |
|---|---|---|---|
| Core Concept | Molecules with identical molecular formulas but distinct structural arrangements or spatial orientations. | Distinct structural modifications of a single element within the same physical state. | The capacity of a solid compound or element to manifest in multiple distinct crystal lattices. |
| Scope of Applicability | Compounds and molecules (organic and inorganic). | Elements exclusively. | Crystalline solids (elements, ionic salts, or molecular solids). |
| Structural Variation | Variations in chemical bonding, atom connectivity, or three-dimensional spatial geometry. | Variations in bonding patterns, molecular formulas, or crystal structures of an element. | Variations in the packing arrangements or space groups of atoms or molecules in a solid. |
| Chemical Properties | Significant variances in reactivity and functionality (e.g., ethanol versus dimethyl ether). | Marked divergence in chemical reactivity (e.g., the inertness of diamond versus the reactivity of graphite). | Identity in liquid or gaseous phases; minor variations in solid-state surface reactivity. |
| Physical Properties | Variances in boiling points, melting points, and densities. | Radical divergence in characteristics (e.g., the transparency and hardness of diamond versus the opacity and softness of graphite). | Distinct variations in solubility, hardness, density, and melting points. |
| Physical State | Gas, liquid, and solid phases. | Predominantly solid phases, with occurrences in liquid and gas phases (e.g., dioxygen versus ozone gas). | Crystalline solids exclusively. |
| Primary Mechanism | Alternative modes of atomic linkage, functional group placement, or molecular rotation. | Alternative modes of homonuclear bonding and molecular aggregation. | Thermodynamic variations in temperature and pressure during the process of crystallization. |
| Examples |
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01History
The concept of allotropy was originally proposed in 1840 by the Swedish scientist Baron Jöns Jakob Berzelius (Swedish: [jœ̌ns ˈjɑ̂ːkɔb bæˈʂěːlɪɵs]; 1779-1848). The term is derived from Greek άλλοτροπἱα (allotropia) 'variability, changeableness'. After the acceptance of Avogadro's hypothesis in 1860, it was understood that elements could exist as polyatomic molecules, and two allotropes of oxygen were recognized as O2 and O3. In the early 20th century, it was recognized that other cases such as carbon were due to differences in crystal structure.
By 1912, Ostwald noted that the allotropy of elements is just a special case of the phenomenon of polymorphism known for compounds, and proposed that the terms allotrope and allotropy be abandoned and replaced by polymorph and polymorphism. Although many other chemists have repeated this advice, IUPAC and most chemistry texts still favour the usage of allotrope and allotropy for elements only.

02Differences in properties of an element's allotropes
Allotropes are different structural forms of the same element and can exhibit quite different physical properties and chemical behaviours. The change between allotropic forms is triggered by the same forces that affect other structures, i.e., pressure, light, and temperature. Therefore, the stability of the particular allotropes depends on particular conditions. For instance, iron changes from a body-centered cubic structure (ferrite) to a face-centered cubic structure (austenite) above 906 °C, and tin undergoes a modification known as tin pest from a metallic form to a semimetallic form below 13.2 °C (55.8 °F). As an example of allotropes having different chemical behaviour, ozone (O3) is a much stronger oxidizing agent than dioxygen (O2).
03List of allotropes
Typically, elements capable of variable coordination number and/or oxidation states tend to exhibit greater numbers of allotropic forms. Another contributing factor is the ability of an element to catenate.
Examples of allotropes include:
Non-metals
| Element | Allotropes |
|---|---|
| Carbon |
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| Nitrogen |
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| Phosphorus |
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| Oxygen |
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| Sulfur |
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| Selenium |
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| Spin isomers of hydrogen |
These nuclear spin isomers have sometimes been described as allotropes, notably by the committee which awarded the 1932 Nobel prize to Werner Heisenberg for quantum mechanics and singled out the "allotropic forms of hydrogen" as its most notable application. |
Metalloids
| Element | Allotropes |
|---|---|
| Boron |
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| Silicon |
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| Germanium |
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| Arsenic |
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| Antimony |
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| Tellurium |
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Metals
Among the metallic elements that occur in nature in significant quantities (56 up to U, without Tc and Pm), almost half (27) are allotropic at ambient pressure: Li, Be, Na, Ca, Ti, Mn, Fe, Co, Sr, Y, Zr, Sn, La, Ce, Pr, Nd, Sm, Gd, Tb, Dy, Yb, Hf, Tl, Th, Pa and U. Some phase transitions between allotropic forms of technologically relevant metals are those of Ti at 882 °C, Fe at 912 °C and 1,394 °C, Co at 422 °C, Zr at 863 °C, Sn at 13 °C and U at 668 °C and 776 °C.
| Element | Phase name(s) | Space group | Pearson symbol | Structure type | Description |
|---|---|---|---|---|---|
| Lithium | α-Li | R3m | hR9 | α-Sm | Forms below 70 K. |
| β-Li | Im3m | cI2 | W | Stable at room temperature and pressure. | |
| Fm3m | cF4 | Cu | Forms above 7GPa | ||
| R3m | hR1 | α-Hg | An intermediate phase formed ~40GPa. | ||
| I43d | cI16 | Forms above 40GPa. | |||
| oC88 | Forms between 60 and 70 GPa. | ||||
| oC40 | Forms between 70 and 95 GPa. | ||||
| oC24 | Forms above 95 GPa. | ||||
| Beryllium | α-Be | P63/mmc | hP2 | Mg | Stable at room temperature and pressure. |
| β-Be | Im3m | cI2 | W | Forms above 1255 °C. | |
| Sodium | α-Na | R3m | hR9 | α-Sm | Forms below 20 K. |
| β-Na | Im3m | cI2 | W | Stable at room temperature and pressure. | |
| Fm3m | cF4 | Cu | Forms at room temperature above 65 GPa. | ||
| I43d | cI16 | Forms at room temperature, 108GPa. | |||
| Pnma | oP8 | MnP | Forms at room temperature, 119GPa. | ||
| tI19* | A host-guest structure that forms above between 125 and 180 GPa. | ||||
| hP4 | Forms above 180 GPa. | ||||
| Magnesium | P63/mmc | hP2 | Mg | Stable at room temperature and pressure. | |
| Im3m | cI2 | W | Forms above 50 GPa. | ||
| Aluminium | α-Al | Fm3m | cF4 | Cu | Stable at room temperature and pressure. |
| β-Al | P63/mmc | hP2 | Mg | Forms above 20.5 GPa. | |
| Potassium | Im3m | cI2 | W | Stable at room temperature and pressure. | |
| Fm3m | cF4 | Cu | Forms above 11.7 GPa. | ||
| I4/mcm | tI19* | A host-guest structure that forms at about 20 GPa. | |||
| P63/mmc | hP4 | NiAs | Forms above 25 GPa. | ||
| Pnma | oP8 | MnP | Forms above 58GPa. | ||
| I41/amd | tI4 | Forms above 112 GPa. | |||
| Cmca | oC16 | Formas above 112 GPa. | |||
| Iron | α-Fe, ferrite | Im3m | cI2 | Body-centered cubic | Stable at room temperature and pressure. Ferromagnetic at T<770 °C, paramagnetic from T=770-912 °C. |
| γ-iron, austenite | Fm3m | cF4 | Face-centered cubic | Stable from 912 to 1,394 °C. | |
| δ-iron | Im3m | cI2 | Body-centered cubic | Stable from 1,394, 1,538 °C, same structure as α-Fe. | |
| ε-iron, Hexaferrum | P63/mmc | hP2 | Hexagonal close-packed | Stable at high pressures. | |
| Cobalt | α-Cobalt | hexagonal-close packed | Forms below 450 °C. | ||
| β-Cobalt | face centered cubic | Forms above 450 °C. | |||
| ε-Cobalt | P4132 | primitive cubic | Forms from thermal decomposition of [Co2CO8]. Nanoallotrope. | ||
| Rubidium | α-Rb | Im3m | cI2 | W | Stable at room temperature and pressure. |
| cF4 | Forms above 7 GPa. | ||||
| oC52 | Forms above 13 GPa. | ||||
| tI19* | Forms above 17 GPa. | ||||
| tI4 | Forms above 20 GPa. | ||||
| oC16 | Forms above 48 GPa. | ||||
| Tin | α-tin, gray tin, tin pest | Fd3m | cF8 | d-C | Stable below 13.2 °C. |
| β-tin, white tin | I41/amd | tI4 | β-Sn | Stable at room temperature and pressure. | |
| γ-tin, rhombic tin | I4/mmm | tI2 | In | Forms above 10 GPa. | |
| γ'-Sn | Immm | oI2 | MoPt2 | Forms above 30 GPa. | |
| σ-Sn, γ"-Sn | Im3m | cI2 | W | Forms above 41 GPa. Forms at very high pressure. | |
| δ-Sn | P63/mmc | hP2 | Mg | Forms above 157 GPa. | |
| Stanene | |||||
| Polonium | α-Polonium | simple cubic | |||
| β-Polonium | rhombohedral |
Most stable structure under standard conditions.
Structures stable below room temperature.
Structures stable above room temperature.
Structures stable above atmospheric pressure.
Lanthanides and actinides
- Cerium, samarium, dysprosium and ytterbium have three allotropes.
- Praseodymium, neodymium, gadolinium and terbium have two allotropes.
- Plutonium has six distinct solid allotropes under "normal" pressures. Their densities vary within a ratio of some 4:3, which vastly complicates all kinds of work with the metal (particularly casting, machining, and storage). A seventh plutonium allotrope exists at very high pressures. The transuranium metals Np, Am, and Cm are also allotropic.
- Promethium, americium, berkelium and californium have three allotropes each.

04Nanoallotropes
In 2017, the concept of nanoallotropy was proposed. Nanoallotropes, or allotropes of nanomaterials, are nanoporous materials that have the same chemical composition (e.g., Au), but differ in their architecture at the nanoscale (that is, on a scale 10 to 100 times the dimensions of individual atoms). Such nanoallotropes may help create ultra-small electronic devices and find other industrial applications. The different nanoscale architectures translate into different properties, as was demonstrated for surface-enhanced Raman scattering performed on several different nanoallotropes of gold. A two-step method for generating nanoallotropes was also created.
Sources and credits
This article is adapted from the Wikipedia article “Allotropy”, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.
Images, from Wikimedia Commons:
- Diamond and graphite.jpg by User:Itub, CC BY-SA 3.0
- Jöns Jacob Berzelius.png by Olof Johan Södermark (1790-1848). Print Artist: Charles W. Sharpe, d. 1875(76). Per [2], Public domain
- Actinide phases.svg by James L. Smith, LANL., Public domain
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