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Element 103 · actinide

Lawrencium (Lr)


In 2015 a team at the Japan Atomic Energy Agency in Tokai measured how hard it is to pull one electron off an atom of lawrencium, and got 4.96 electronvolts. That is a startlingly small number for a metal at the bottom of the actinide series. It is smaller than any other actinide, smaller than any lanthanide, and close to the value for the alkali metals — the elements that give their outer electron away most readily of anything in chemistry. Among all the elements, only the group 1 metals, and francium in particular, hold their outermost electron more loosely.

It was also the first ionisation potential ever measured for an element beyond fermium, and it was done on atoms arriving one at a time from an accelerator, each surviving about twenty-seven seconds.

Two claims, one shared credit

Element 103's discovery is one of the messier entries in the record, and the mess is unusually symmetrical.

Berkeley got there first, in 1961, using the newly commissioned heavy-ion linear accelerator to fire boron at a californium target. Albert Ghiorso, Torbjørn Sikkeland, Almon Larsh and Robert Latimer reported an alpha emitter with a half-life of about eight seconds and assigned it to lawrencium-257. The trouble is that the isotope they described does not appear to be the one they made; later work put the observed activity at lawrencium-258, and the decay energy they reported did not hold up.

Dubna produced element 103 in 1965, from americium under an oxygen beam, and identified lawrencium-256 by chemically fingerprinting its decay daughter. That assignment stood better, but it was not unambiguous either.

When the IUPAC/IUPAP Transfermium Working Group reviewed the file in 1992, it found neither claim individually sufficient and recommended that the credit be shared between the two laboratories. Berkeley kept the naming right in practice, and the name honours Ernest Lawrence, whose invention of the cyclotron underwrote the entire enterprise and who had died three years before the element was made.

The symbol has changed once. Berkeley proposed Lw; IUPAC replaced it with Lr in 1963. Dubna, for its part, had wanted element 103 called rutherfordium — a name that would eventually attach itself to a different square on the table entirely.

Reading an atom's structure from how it ionises

The 2015 measurement, led by T. K. Sato and published in Nature, worked by exploiting a property of hot metal surfaces: an atom landing on one will be released as a positive ion if its ionisation potential is low enough, and as a neutral atom if it is not. Scan the surface temperature, count how many lawrencium atoms come off charged, and the crossover tells you the ionisation energy.

The result did more than fill in a number. The conventional configuration assigned to lawrencium, and the one still carried on most reference tables, ends in a 6d electron, following the pattern set by lutetium above it. A 6d electron would be held more tightly than 4.96 eV. A 7p electron would not — and relativistic calculations had for years predicted that in lawrencium the 7p₁/₂ orbital drops below 6d, because relativistic effects contract and stabilise orbitals with electron density near the nucleus.

The measured value matched the 7p prediction almost exactly. That is worth stating carefully: the ionisation potential is a measurement, and the ground-state configuration inferred from it is an inference supported by calculation, not something anyone has observed directly. But it is a strong inference, and it means lawrencium is the first element where the actinide series' expected electron filling visibly breaks.

Where element 103 belongs

Lawrencium is at the centre of one of the last genuinely unsettled arguments about the shape of the periodic table: what goes in group 3, underneath scandium and yttrium.

Two rival arrangements have been in print for decades, and element 103 is in one of them and not the other. Either it caps the actinide row, or it steps sideways into group 3 alongside lutetium and leaves the f-block to begin an element earlier. Textbooks and wall charts differ, and chemists hold the question with some heat.

What lawrencium contributes to the argument is its electronic structure, which is why the ionisation measurement matters beyond the number itself. An IUPAC project convened to settle the membership of group 3 issued a provisional report in 2021 favouring the arrangement that includes element 103, on the principle that each block should be completed before the next begins. The matter is not closed. What is unusual is that a synthetic element known from a few thousand atoms should have any bearing at all on how the whole table is drawn.

What its chemistry is, and what it is not

Lawrencium in solution is trivalent and nothing else. Unlike nobelium immediately below it in atomic number, it shows no tendency toward a +2 state, and the reason is the same electron count read the other way: lawrencium already has a filled 5f¹⁴ shell in its ground state, so the outer electron sits outside it and is easy to remove without disturbing anything. Experiments in the 1980s, tracking a few atoms through solvent extraction, confirmed it behaves as a tripositive ion of about the size predicted.

The isotopes are short. Lawrencium-266, identified in 2014 as a decay product of heavier nuclei, lasts about eleven hours and is by a wide margin the most durable; lawrencium-262 lasts under four hours, and the isotopes that most experiments actually use are gone within seconds. No metallic lawrencium exists, no compound has been isolated, and the melting point quoted for it is an extrapolation from its neighbours rather than anything anyone has watched happen.

Isotopes of Lawrencium

No isotope of Lawrencium has a measurable natural abundance, and only one has a relative atomic mass on record.

Isotopes of Lawrencium with relative atomic mass and natural abundance
IsotopeRelative atomic massNatural abundance
262Lr262.10961(22#)none

103

Lr

Lawrencium

actinide

Standard atomic weight
[262]the mass number of the longest-lived isotope; this element has no stable one
Group / period / block
3 · 7 · d
Electron configuration
[Rn] 7s2 5f14 6d1
Electrons per shell
2, 8, 18, 32, 32, 8, 3
State at 20 °C
solid
Melting point
1900 K · 1627 °C
Boiling point
not known
Density
not known
Electronegativity
1.3 (Pauling)
First ionisation energy
not known
Common oxidation states
+3
Discovery
1961 · credited to Lawrence Berkeley National Laboratory

Hazard facts

  • Radioactive Every isotope is unstable, so the element emits ionising radiation as it decays.

These are properties of the element, stated as facts. Nothing on this site describes how to handle or work with any substance.

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