How are new elements discovered?
Several experimental
techniques have been used to make new chemical elements.
Some of these include
i)
heavy ion transfer reactions,
ii) cold or hot fusion evaporation
reactions,
iii) neutron capture reactions,
Iv) light-ion charged particle induced
reactions, and
V) even nuclear explosions.
These techniques each
have advantages and disadvantages making them suitable for studying nuclei in
certain regions.
The types of nuclear
reactions that have been successfully used to produce new elements in the last
decade are cold fusion reactions and hot fusion reactions.
Cold fusion
reactions use beam and target nuclei that are closer to each other in mass in
order to produce a compound nucleus (the complete fusion of one target nucleus
with one beam nucleus) with generally lower excitation energy that typically
requires evaporation of one or no neutrons. This generates fewer neutron-rich
isotopes of an element that have higher survival probabilities with respect to
fission, but have lower fusion probabilities. An example of this type of
reaction is70Zn + 208Pb
→ 277112
+ 1n with a cross-section of ~1 picobarn.
Because the 112
isotope ultimately decays by α emission to known nuclei [namely isotopes of elements
102 (No) and 104 (Rf)], identification of this element is straightforward. Hot
fusion reactions use more asymmetric beam and target nuclei, produce a compound
nucleus with generally higher excitation energy that typically requires
evaporation of three to five neutrons, generate more neutron-rich isotopes of
an element, have lower survival probabilities with respect to fission, but have
higher fusion probabilities.
An example of this type of reaction is 48Ca
+ 244Pu
→ 288114
+ 4n with a cross-section of ~1 pb. Because of the neutron-richness of this
isotope of element 114, it never subsequently decays to any known isotope, and
thus its identification is more problematic. Cold fusion reactions have been
successful in producing elements 104—112 and hot fusion reactions have recently
provided evidence for elements 113—118.
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