History
In June 1974, members of the Joint Institute for Nuclear Research in Dubna,
U.S.S.R., reported their discovery of Element 106, which they reported to have
synthesized. Glenn Seaborg was part of this group, and the element was named in
his honor. Seaborgium is often still referred to as Element 106 because the
international committee in charge of names changed the rules. They decided
retroactively it couldn't be named after a living person.
In September 1974, workers of the Lawrence Berkeley and Livermore
Laboratories also claimed creation Element 106 "without any scientific doubt."
The LBL and LLL Group used the Super HILAC to accelerate 18O ions onto a 249Cf
target.
Element 106 was created by the reaction 249Cf(18O, 4N)263X, which decayed by
alpha emission to rutherfordium, and
then by alpha emission to nobelium, which in
turn further decayed by alpha between daughter and granddaughter. The element so
identified had alpha energies of 9.06 and 9.25 MeV with a half-life of 0.9 +/-
0.2 s.
At Dubna, 280-MeV ions of 54Cr from the 310-cm cyclotron were used to strike
targets of 206Pb, 207Pb, and 208Pb, in separate runs. Foils exposed to a
rotating target disc were used to detect spontaneous fission activities. The
foils were etched and examined microscopically to detect the number of fission
tracks and the half-life of the fission activity.
Page Source: Los Alamos National Laboratory
Last Updated: 12/19/97, CST Information Services Team
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