Rutherfordium is the transactinide (superheavy) element with atomic number 104, synthesized in the 1960s by teams at the Joint Institute for Nuclear Research in Dubna, USSR, and at Berkeley, U.S., by bombarding lead and plutonium targets with heavy ions. All of its isotopes have half-lives within the minute scale, it does not occur in nature, and it can only be produced atom by atom in heavy-ion accelerators. It has no industrial or civilian uses and is studied only to test whether the chemistry of superheavy elements follows the periodic law.
Rutherfordium compounds such as rutherfordium tetrachloride (RfCl4) have only been briefly measured in single-atom gas-phase and solution-phase chemistry experiments, to test whether it behaves like hafnium and zirconium; they have never been prepared or weighed in macroscopic quantities and have no practical application.