| Atomic
Number: |
104 |
| Atomic
Symbol: |
Rf
|
| Atomic
Weight: |
261 |
| Electron
Configuration: |
[Rn]7s25f146d2 |
In 1964, workers at the Joint Nuclear Research
Institute at Dubna (U.S.S.R.) bombarded plutonium with accelerated
113 to 115 MeV neon ions. By measuring fission tracks in
a special glass with a microscope, they detected an isotope
that decays by spontaneous fission. They
suggested that this isotope, which had a half-life of 0.3
+/- 0.1 s might be 260-104, produced by the following reaction:
242Pu + 22Ne -->104 +4n.
Element
104, the first transactinide element, is expected to have
chemical properties similar to those of hafnium. It would,
for example, form a relatively volatile compound with
chlorine (a tetrachloride).
The
Soviet scientists have performed experiments aimed at
chemical identification, and have attempted to show that
the 0.3-s activity is more volatile than that of the relatively
nonvolatile actinide trichlorides. This experiment does
not fulfill the test of chemically separating
the new element from all others, but it provides important
evidence for evaluation.
New
data, reportedly issued by Soviet scientists, have reduced
the half-life of the isotope they worked with from 0.3
to 0.15 s. The Dubna scientists suggest the name kurchatovium
and symbol Ku for element 104, in honor of Igor Vasilevich
Kurchatov (1903-1960), former Head
of Soviet Nuclear Research.
Isotopes
In
1969 Ghiorso, Nurmia, Harris, K.A.Y. Eskola, and P.L.
Eskola of the University of California at Berkeley reported
that they had positively identified two, and possibly
three, isotopes of Element 104. The group indicated that,
after repeated attempts, they produced isotope 260-104
reported by the Dubna groups in 1964.
The
discoveries at Berkeley were made by bombarding a target
of 249Cf with 12C nuclei of 71 MeV, and 13C nuclei of
69 MeV. The combination of 12C with 249Cf followed by
instant emission of four neutrons produced Element 257-104.
This isotope has a half-life of 4 to 5 s, decaying by
emitting an alpha particle into 253No, with a half-life
of 105 s.
The
same reaction, except with the emission of three neutrons,
was thought to have produced 258-104 with a half-life
of about 1/100 s.
Element
259-104 is formed by the merging of a 13C nuclei with
249Cf, followed by emission of three neutrons. This isotope
has a half-life of 3 to 4 s, and decays by emitting an
alpha particle into 255No, which has a half-life of 185
s.
Thousands
of atoms of 257-104 and 259-104 have ben detected. The
Berkeley group believes their identification of 258-104
is correct, but attaches less confidence to this work
than to their work on 257-104 and 259-104.
The
claims for discovery and the naming of Element 104 are
still in question. The Berkeley group proposes for the
new element the name rutherfordium (symbol Rf), in honor
of Ernest R. Rutherford, a New Zealand physicist. Meanwhile,
the International Union of Pure and Applied Physics has
proposed using the neutral temporary name, unnilquadium.