Scientific research
Rutherfordium is produced, isolated or measured mainly to test atomic, nuclear and periodic trends rather than for bulk commercial use.
Rutherfordium is element 104 (Rf), located in period 7, group 4 and the d block. No macroscopic sample exists, so an ordinary room-temperature phase is not established experimentally. Its calculated electron configuration is [Rn] 5f14 6d2 7s2.
Rutherfordium is a superheavy synthetic element. Only very small numbers of atoms have been produced, so its chemistry is studied through individual decay events and specialised atom-at-a-time experiments rather than bulk samples.
Its position in group 4 and the d block provides a first prediction of its chemistry, but relativistic effects become increasingly important for the heaviest nuclei. Experimental results are therefore essential before extending lighter-group trends too confidently.
Bulk rutherfordium compounds cannot be prepared because only tiny numbers of short-lived atoms are produced. Chemical experiments, when possible, test adsorption, volatility or single-atom reactions and compare the results with lighter elements in the same group.
No macroscopic sample has been produced, so ordinary bulk properties such as density, melting point and boiling point are not established experimentally. Published values for superheavy elements are generally theoretical predictions and should be labelled as such.
In practice, rutherfordium is encountered in scientific research.
Rutherfordium is produced, isolated or measured mainly to test atomic, nuclear and periodic trends rather than for bulk commercial use.
Rutherfordium is in period 7 and group 4. In the neighbourhood shown here, dubnium is immediately to its right in the same period; hafnium is directly above it in the same group. These positions make it possible to compare atomic size, ionisation energy and bonding behaviour with nearby elements.
Values describe the element or neutral atom where applicable. Physical data can depend on allotrope, pressure and measurement conditions.
Rutherfordium is synthetic. It is produced in nuclear-reaction experiments and identified from the decay chains of the atoms created. The quantities involved are far below anything that could form a visible sample.
Rutherfordium has no standard atomic weight. There is no characteristic terrestrial isotopic mixture from which a stable abundance-weighted average can be assigned.
Rutherfordium 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.
Rutherfordium is radioactive. Work with it requires radiological controls appropriate to the isotope, activity, radiation type and chemical form.