Oganesson

    group 18 · period 7 · p-block · unknown, predicted to be noble gas

    Identity

    Name and symbol
    Oganesson, Og
    Atomic number
    118 protons
    Position
    group 18 · period 7 · p-block · unknown, predicted to be noble gas
    CAS number
    54144-19-3

    Atomic structure

    Atomic mass
    294 u
    Electron configuration
    1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹⁴ 5d¹⁰ 6p⁶ 7s² 5f¹⁴ 6d¹⁰ 7p⁶
    [Rn] 7s² 7p⁶ 5f¹⁴ 6d¹⁰(predicted)
    Electrons per shell
    2, 8, 18, 32, 32, 18, 8
    Valence electrons
    8 outer shell
    nuclidehalf-lifedecay
    295Og680 msα≈100%
    293Og1 ms [Estimated]α ?
    294Og0.7 msα≈100%; SF ?
    no stable isotope; the longest-lived nuclides

    Physical properties

    State at room temperature
    Expected to be a Gas
    Melting point
    not in sources
    Boiling point
    350 K (76.85 °C)
    Density
    not in sources
    Appearance
    metallic (predicted)
    Thermal conductivity
    not in sources
    Electrical resistivity
    not in sources
    Electrical conductivity
    not in sources
    Crystal structure
    face-centered cubic
    Molar heat capacity
    not in sources

    Chemical properties

    Oxidation states
    -1, 0, +1,+2,+4, +6 ​(predicted)
    Electronegativity
    not in sources
    Ionisation energy
    not in sources
    Electron affinity
    not in sources
    Atomic radius
    not in sources
    Ionic radius
    not in sources
    Reactivity
    The heaviest known element, closing period 7 under radon; only a few atoms with sub-millisecond half-lives have been made, so no chemical experiment has been possible and its properties, including whether it behaves as a noble gas at all, are calculated only.
    with water
    Not known; no experiment has been reported.
    with oxygen, air
    Not known; no experiment has been reported.
    with acids
    Not known; no experiment has been reported.
    with halogens
    Not known; no experiment has been reported.
    Typical compounds
    not in sources

    Occurrence, production and use

    Crustal abundance
    Not Applicable
    Oceanic abundance
    Not Applicable
    Occurrence and sources
    • synthetic only californium-249 bombarded with calcium-48 ions at Dubna
    Extraction, production
    not in sources
    Uses

    Since only a few atoms of oganesson have ever been produced, it currently has no uses outside of basic scientific research.

    Safety, toxicity
    not in sources

    Discovery and name

    Discovered by
    Joint Institute for Nuclear Research and Lawrence Livermore National Laboratory
    Discovered
    2002
    First isolated
    not in sources
    Named by
    not in sources
    Origin of the name
    after Yuri Oganessian

    Oganesson does not occur naturally in the Earth’s crust. The name oganesson and symbol Og are the accepted ones for element 118. The name is in line with the tradition of honoring a scientist and recognizes Prof. Yuri Oganessian (Fig. IUPAC.118.1; born 1933) for his pioneering contribution to trans-actinoid element research. His many achievements include the discovery of super-heavy elements and significant advances in the nuclear physics of super-heavy nuclei, including experimental evidence for the “island of stability.”

    In 2005, experiments were performed in Dubna’s U-400 cyclotron, where 48Ca bombarded a spinning target of 249Cf at nearly 3×104 km/s to produce oganesson. With the success of creating oganesson, scientists from Livermore and Joint Institute for Nuclear Research (JINR) are starting experiments to create element 120 by bombarding a 244Pu target with a beam of 58Fe [680], [681], [682], [683]. Oganesson has no known isotopic applications aside from scientific research.

    Conventions

    Valence electrons are counted by the usual convention: the outer shell for s- and p-block elements, ns and (n-1)d for the d-block, ns, (n-1)d and (n-2)f for the f-block. Lanthanides and actinides are placed in the f-block with no group number. Electrical conductivity is the reciprocal of the printed resistivity. Ionic radii are Shannon effective radii, six-coordinate unless noted. Where a field reads “not in sources” the value was not found; it is a gap, not a zero. Regulatory limits are the published values and change often, so check the standard in force at your site and the numbers written into your own permit before you design to them.

    Data

    Element records, isotopes, radii and the descriptive text come from PubChem (NCBI), the Los Alamos National Laboratory periodic table, IUPAC CIAAW and the IAEA Atomic Mass Data Center. Appearance, thermal conductivity, electrical resistivity, crystal structure, discovery and the origin of each name come from Wikipedia and Periodic-Table-JSON, used under CC BY-SA 4.0. Hazard classifications come from the ECHA C&L inventory via PubChem. Ionic radii follow R. D. Shannon (1976). The water chapters cite their own sources at the foot of each entry, and are written to the level of Snoeyink and Jenkins, Stumm and Morgan, MWH's Water Treatment and Metcalf and Eddy.