Oganesson is IUPAC's name for the transactinide element with the atomic number 118 and element symbol Og. It is also known as eka-radon or element 118, and on the periodic table of the elements it is a p-block element and the last one of the 7th period. Oganesson is currently the only synthetic member of group 18.
Oganesson is a superheavy element with symbol Og and atomic number 118, located at the top right of the periodic table as the heaviest member of group 18 (noble gases). It was first synthesized in 2002 at Los Alamos National Laboratory, United States. It is the heaviest known element and presents properties that, according to theoretical models, could notably depart from the patterns of lighter noble gases due to relativistic effects. Oganesson is produced atom by atom through nuclear reactions, and its known isotopes have extremely short lives, making it impossible to obtain macroscopic samples for direct experimental characterization of its physical and chemical properties.
Og does not react under normal conditions
Although some theoretical models suggest increased reactivity in oganesson due to relativistic effects, no confirmatory experimental chemical assays have been conducted.
Og -> possible formation of theoretical compounds
Certain theoretical calculations predict that oganesson could form compounds with very electronegative elements such as fluorine and oxygen, although this has not yet been experimentally confirmed.
| Compound | Formula | Use or importance |
|---|---|---|
| Oganesson tetrafluoride | OgF4 (theoretical) | Compound predicted by theoretical models; not yet synthesized or characterized experimentally |
| Oganesson hexafluoride | OgF6 (theoretical) | Theoretical compound that could exist under extreme pressure and temperature conditions |
Oganesson has no stable isotopes. Known isotopes are all radioactive with very short half-lives, ranging from 0.69 milliseconds (Og-293-2002) to 0.89 milliseconds (Og-294-2005). The most stable known isotopes include Og-294 (half-life of 0.89 ms) and Og-295. The lighter isotopes, Og-290 to Og-293, have lives of milliseconds or less.
Oganesson is an artificial element that does not occur in nature. It is produced in nuclear physics laboratories through nucleon fusion, generally through the collision of calcium-48 ions with plutonium-244 targets or other heavy targets. Oganesson is not found in the Earth's crust, in the atmosphere nor in any mineral resource.
Oganesson was first synthesized in 2002 at Los Alamos National Laboratory (USA), where a team led by Yuri Oganessian produced an Og-294 atom through the collision of calcium-48 ions with plutonium-244 targets. The synthesis was confirmed in 2006 by a second experiment. In 2016, the International Union of Pure and Applied Chemistry (IUPAC) named the element 'oganesson' in honor of Yuri Oganessian, recognized for his pioneering work in superheavy element synthesis.
Oganesson has no known practical applications. Its study is purely scientific, aimed at expanding the limits of knowledge about atomic structure, relativistic effects and superheavy element chemistry.
No stable oganesson compound is known. Any theoretical compound suggests a high-complexity experiment that would require very advanced experimental technology not yet developed for this element's characterization.
Oganesson has no biological implications, as it is not produced nor used in quantities that could affect living beings. Its isotopes are highly radioactive with millisecond half-lives and radioactivity occurs at atomic scale, so it does not present health risks for humans under normal conditions.
Oganesson is an artificial, highly radioactive element produced in nuclear physics laboratories. Oganesson sample handling is extremely limited and can only be carried out in high-security experimental facilities. Due to its isotopes' short life, oganesson's radiological risk is lower than that of other radioactive elements with longer half-lives, but it requires specialized radiochemical safety protocols.
Oganesson has no environmental impact in nature, as it does not occur naturally. Its production is carried out only in controlled laboratories with specialized safety facilities. Oganesson laboratory waste must be treated in accordance with nuclear safety and radioactivity regulations.
Although oganesson is classified among noble gases, some theoretical calculations predict that it could be solid at room temperature. This possibility is due to intense relativistic effects modifying its electronic structure and interactions between its atoms. A 2020 study estimated a melting point close to 325 kelvin, slightly above usual room temperature. However, a solid sample has not been able to be experimentally observed, so this prediction remains theoretical.
Relativistic effects are modifications of the electronic structure that become important when electrons are subjected to the intense attraction of a nucleus with a very high charge. They alter orbital energies and can change electron distribution, bond formation and the element's physical properties. In oganesson, these effects are especially important to predict its behavior, because conventional chemical models developed for lighter atoms are not sufficient by themselves to describe it accurately.
Oganesson is produced atom by atom in nuclear experiments, and its known isotopes have extremely short lives. This prevents accumulating enough material to perform conventional chemical assays. Researchers identify atoms through their decay chains and resort to quantum physics models to predict its behavior. Studying its chemical bonds or macroscopic properties directly requires experimental techniques that still do not allow characterizing it with the detail usual in other elements.
Studying oganesson allows investigating how matter behaves when nuclei contain extraordinarily high quantities of protons. Scientists compare its electronic and nuclear predictions with those of other superheavy elements to check the limits of current models. These investigations help understand nuclear stability, relativistic effects and the possible properties of still heavier elements. Although oganesson has no known practical applications, its study expands fundamental knowledge about the structure of atoms.
Lighter noble gases usually present very low chemical reactivity, but the same trends are not expected to be maintained exactly in oganesson. Its enormous nuclear charge causes relativistic effects that alter the energy and distribution of outer electrons. Theoretical models predict that these modifications could increase its polarizability and change its chemical behavior compared to radon. Even so, oganesson's chemistry has not been experimentally characterized, so these differences should be considered scientific predictions.
Some theoretical calculations suggest that oganesson could present electronic properties very different from those expected for a conventional noble gas, even semiconductor behavior under certain conditions. These predictions depend on the models used to describe its electrons and interactions between atoms. However, no sample has been obtained that allows directly measuring its electrical conductivity. Therefore, it cannot be experimentally affirmed that oganesson is a conductor, insulator or semiconductor under ambient conditions.
Oganesson is distinguished by being a superheavy element whose behavior could depart considerably from the pattern observed in lighter noble gases. In these latter ones, the external electron configuration usually explains its low reactivity and its tendency to exist as isolated atoms. In oganesson, relativistic effects modify that structure and could alter both its reactivity and its physical properties. These differences make its classification as a noble gas chemically interesting, although its real properties have not yet been confirmed through direct experiments.
Main sources consulted: PubChem, Royal Society of Chemistry, NIST, IUPAC. Last revision: November 2026.