Scientific research
Lawrencium is produced, isolated or measured mainly to test atomic, nuclear and periodic trends rather than for bulk commercial use.
Lawrencium is element 103 (Lr), located in period 7, group 3 and the d block. At room temperature its reference phase is solid. Its electron configuration is [Rn] 5f14 7s2 7p1.
The d subshell participates in the chemistry of lawrencium. Transition metals can use electrons of similar energies in bonding, which is why variable oxidation states, coordination compounds and catalytic behaviour are common across the d block.
Its electron configuration, [Rn] 5f14 7s2 7p1, should be read together with the oxidation state of the compound: removing electrons changes which d orbitals are occupied and can alter colour, magnetism, bonding and reactivity.
For lawrencium, important chemical forms include metals and alloys, oxides, halides and coordination compounds. Variable oxidation states are common because s and d electrons have similar energies, and ligands around the metal ion can strongly alter colour, magnetism and reactivity.
The reference phase at room temperature is solid. The melting point is 1 900 K (1 627 °C). Where a phase-transition value is not listed, the behaviour may be poorly defined under ordinary pressure, depend strongly on allotrope, or lack a reliable reference value. Pressure, purity and crystal structure can shift measured physical properties.
In practice, lawrencium is encountered in scientific research.
Lawrencium is produced, isolated or measured mainly to test atomic, nuclear and periodic trends rather than for bulk commercial use.
Lawrencium is in period 7. In the f-block sequence shown here, it appears between nobelium and rutherfordium. This sequence allows a direct comparison with the neighbouring f-block elements.
Values describe the element or neutral atom where applicable. Physical data can depend on allotrope, pressure and measurement conditions.
The discovery of lawrencium is associated with Lawrence Berkeley National Laboratory. Recognition of the element, isolation of a pure sample and assignment of its modern atomic number did not necessarily occur at the same time.
Lawrencium has no standard atomic weight. There is no characteristic terrestrial isotopic mixture from which a stable abundance-weighted average can be assigned.
Lawrencium has no stable isotope. Its isotopes are radioactive, and their half-lives and decay modes become important whenever the element is measured, handled or used.
Lawrencium is radioactive. Work with it requires radiological controls appropriate to the isotope, activity, radiation type and chemical form.