Rutherfordium

    group 4 · period 7 · d-block · transition metal

    Identity

    Name and symbol
    Rutherfordium, Rf
    Atomic number
    104 protons
    Position
    group 4 · period 7 · d-block · transition metal
    CAS number
    53850-36-5

    Atomic structure

    Atomic mass
    263 u
    Electron configuration
    1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹⁴ 5d¹⁰ 6p⁶ 7s² 5f¹⁴ 6d²
    [Rn] 7s²⁵f¹⁴⁶d²
    Electrons per shell
    2, 8, 18, 32, 32, 10, 2
    Valence electrons
    4 ns and (n-1)d
    nuclidehalf-lifedecay
    266Rf4 h [Estimated]α ?; SF ?
    267Rf2.5 hSF=100%
    264Rf1 h [Estimated]α ?
    268Rf1 h [Estimated]α ?; SF ?
    no stable isotope; the longest-lived nuclides

    Physical properties

    State at room temperature
    Solid
    Melting point
    2,400 K (2,126.85 °C)
    Boiling point
    5,800 K (5,526.85 °C)
    Density
    not in sources
    Appearance
    not in sources
    Thermal conductivity
    not in sources
    Electrical resistivity
    not in sources
    Electrical conductivity
    not in sources
    Crystal structure
    hexagonal close-packed
    Molar heat capacity
    not in sources

    Chemical properties

    Oxidation states
    +4
    Electronegativity
    not in sources
    Ionisation energy
    6.02 eV
    1st 580 kJ/mol
    Electron affinity
    not in sources
    Atomic radius
    not in sources
    Ionic radius
    not in sources
    Reactivity
    The first transactinide, made a few atoms at a time; single-atom gas-phase and aqueous experiments show it behaves as a group 4 metal like hafnium, with +4 the only established state, so bulk reactivity cannot be measured.
    with water
    Not known for the element; in basic solution rutherfordium coprecipitates as a hydroxide, probably Rf(OH)4 (2021 experiment).
    with oxygen, air
    Not known; the stable refractory oxide RfO2 is predicted by analogy with zirconium and hafnium but has not been made.
    with acids
    In hydrochloric and hydrofluoric acid single atoms of Rf4+ form hexahalide complexes: RfX4++6ClXRfClX6X2\ce{Rf^4+ + 6 Cl^- -> RfCl6^2-}, and the analogous RfF6^2-, with a weaker fluoride and sulfate affinity than hafnium.
    with halogens
    Single atoms react with chlorine and bromine to the volatile tetrahalides RfCl4 and RfBr4, and an oxychloride RfOCl2, RfCl4 being more volatile than HfCl4.
    Typical compounds
    • RfCl₄ rutherfordium tetrachloride detected in single-atom gas thermochromatography
    • RfBr₄ rutherfordium tetrabromide detected in single-atom gas-phase experiments

    Occurrence, production and use

    Crustal abundance
    Not Applicable
    Oceanic abundance
    Not Applicable
    Occurrence and sources
    • synthetic only californium-249 bombarded with carbon-12 nuclei
    Extraction, production
    not in sources
    Uses

    Due to the small amounts produced and its short half-life, there are currently no uses for rutherfordium outside of basic scientific research.

    Safety, toxicity
    not in sources

    Discovery and name

    Discovered by
    Joint Institute for Nuclear Research and Lawrence Berkeley National Laboratory
    Discovered
    1969
    First isolated
    not in sources
    Named by
    not in sources
    Origin of the name
    after Ernest Rutherford

    Rutherfordium does not occur naturally in the Earth’s crust. Credit for the first synthesis of this element is given jointly to Albert Ghiorso and his team at the University of California in Berkeley and Georgi Flerov and his team at the Joint Institute for Nuclear Research (JINR) in Dubna, Russia. The element is named for Ernest Rutherford (Fig. IUPAC.104.1), who won the Nobel Prize for developing the theory of radioactive transformations [645].

    Rutherfordium is of interest in particle physics research, but it has no commercial applications. 261Rf was one of the decay products used to confirm the synthesis of copernicium in a particle accelerator experiment [634].

    Rutherfordium named after Ernest Rutherford.

    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.