Og 118
Oganesson was first synthesized in 2002 by a collaborative team of Russian and American scientists at the Joint Institute for Nuclear Research (JINR) in Dubna, Russia, and Lawrence Livermore National Laboratory in California, USA. The name 'Oganesson' honors the Russian physicist Yuri Oganessian, who contributed significantly to the discovery of superheavy elements. The element was created by bombarding californium-249 with calcium-48 ions, resulting in the formation of oganesson. The official recognition of oganesson as a chemical element by the International Union of Pure and Applied Chemistry (IUPAC) took place in 2016, following extensive validation of its synthesis.
Oganesson does not occur naturally and is a highly unstable synthetic element. Its production requires sophisticated equipment and techniques for nuclear reactions. The element has been created only in minute quantities (on the order of just a few atoms) in laboratories, and there has been no successful isolation of oganesson in any pure form. Due to its short half-life, oganesson tends to decay rapidly into lighter elements, which contributes to the challenge of studying its properties and behavior.
Currently, there are no known biological roles for oganesson. As a synthetic and highly unstable element, it has not been found in nature, and the extremely brief existence of each atom produced makes biological experiments impractical. Researchers speculate that, if it were stable, oganesson might exhibit unique chemical behavior due to relativistic effects. However, as of now, it remains an element of interest primarily for academic research in nuclear physics and chemistry rather than for potential biological applications.
Oganesson is expected to possess unique physical and chemical properties that may differ significantly from its lighter counterparts in group 18 of the periodic table. While detailed studies are limited due to its instability, theoretical calculations suggest that oganesson could have a relatively high atomic mass, a distinct electronic structure, and possibly exhibit metallic character rather than the typical inertness expected from noble gases. Its predicted boiling and melting points are also anticipated to be higher than those of other noble gases. However, because of the scarcity of oganesson and its rapid decay, empirical data to support these theoretical predictions remains minimal.
Due to its synthetic nature, tremendous instability, and the challenges associated with its production, oganesson currently has no practical applications. Its primary significance lies in the realm of scientific research, particularly regarding studies of superheavy elements, atomic structure, and behavior under relativistic conditions. As scientists continue to explore the nuclear landscape, the study of oganesson may provide insights into the forces that govern the stability of atomic nuclei and advance knowledge in theoretical chemistry.