Lawrencium

    group 3 · period 7 · d-block · actinide

    Identity

    Name and symbol
    Lawrencium, Lr
    Atomic number
    103 protons
    Position
    group 3 · period 7 · d-block · actinide
    CAS number
    22537-19-5

    Atomic structure

    Atomic mass
    262 u
    Electron configuration
    1s² 2s² 2p⁶ 3s² 3p⁶ 4s² 3d¹⁰ 4p⁶ 5s² 4d¹⁰ 5p⁶ 6s² 4f¹⁴ 5d¹⁰ 6p⁶ 7s² 5f¹⁴ 7p¹
    [Rn] 7s²⁵f¹⁴⁶d¹
    Electrons per shell
    2, 8, 18, 32, 32, 8, 3
    Valence electrons
    3 ns and (n-1)d
    nuclidehalf-lifedecay
    266Lr22 hSF=100%
    264Lr10 h [Estimated]α ?; SF ?
    265Lr10 h [Estimated]α ?; SF ?
    263Lr5 h [Estimated]α ?
    no stable isotope; the longest-lived nuclides

    Physical properties

    State at room temperature
    Solid
    Melting point
    1,900 K (1,626.85 °C)
    Boiling point
    not in sources
    Density
    not in sources
    Appearance
    silvery (predicted)
    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
    +3
    Electronegativity
    not in sources
    Ionisation energy
    4.96 eV
    1st 470 kJ/mol
    Electron affinity
    not in sources
    Atomic radius
    not in sources
    Ionic radius
    not in sources
    Reactivity
    The last actinide, known only from experiments on a few thousand atoms; it is trivalent in solution, Lr3+ about as stable as Lu3+, and every attempt to reduce it to Lr2+ or Lr+ in water has failed.
    with water
    Not known for the metal; in water lawrencium exists as the Lr3+ ion, ionic radius about 88 pm, eluting near erbium from cation-exchange columns.
    with oxygen, air
    Not known.
    with acids
    In acid solution extracts and elutes with the trivalent actinides, not with the divalent or tetravalent ones.
    with halogens
    Reacts with chlorine to a product that is most likely LrCl3, with volatility similar to the chlorides of curium, fermium and nobelium and much lower than rutherfordium chloride (1969 experiment).
    Typical compounds
    not in sources

    Occurrence, production and use

    Crustal abundance
    Not Applicable
    Oceanic abundance
    Not Applicable
    Occurrence and sources
    • synthetic only californium bombarded with boron
    Extraction, production
    not in sources
    Uses

    Since only tiny amounts of lawrencium have ever been produced, there are currently no uses for it outside of basic scientific research.

    Safety, toxicity
    not in sources

    Discovery and name

    Discovered by
    Lawrence Berkeley National Laboratory and Joint Institute for Nuclear Research
    Discovered
    1961 to 1971
    First isolated
    not in sources
    Named by
    not in sources
    Origin of the name
    after Ernest Lawrence

    Lawrencium does not occur naturally in the Earth’s crust. Credit for the first synthesis of this element in 1971 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 (Fig. IUPAC.103.1). The element is named for Ernest O. Lawrence (Fig. IUPAC.103.2), who developed the cyclotron. The chemical symbol for lawrencium was originally proposed as Lw. At the IUPAC General Assembly in 1963, lawrencium was officially accepted by IUPAC, but the symbol was changed to Lr because the Commission on Inorganic Nomenclature determined that the letter ‘w’ presented a problem in languages other than English [636], [640], [641], [642]. There are no known isotopic applications for lawrencium outside of scientific research.

    Lawrencium behaves differently from dipositive nobelium and more like the tripositive elements earlier in the actinide series.

    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.