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Transuranium element

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In chemistry, transuranium elements (also known as transuranic elements) are the chemical elements with atomic numbers greater than 92 (the atomic number of uranium). None of these elements are stable; they decay radioactively into other elements.

Overview

Periodic table with elements colored according to the half-life of their most stable isotope.
  Stable elements;
  Radioactive elements with very long-lived isotopes. Their half-lives of over four million years confer them very small, if not negligible radioactivities;
  Radioactive elements that may present low health hazards. Their most stable isotopes have half-lives between 800 and 34.000 years. Because of this, they usually have some commercial applications;
  Radioactive elements that are known to pose high safety risks. Their most stable isotopes have half-lifes between one day and 103 years. Their radioactivities confers them little potential for commercial uses;
  Highly radioactive elements. Their most stable isotopes have half-lifes between one day and several minutes. They pose severe health risks. Few of them receive uses outside basic research;
  Extremely radioactive elements. Very little is known about these elements due to their extreme instability and radioactivity.

Of the elements with atomic numbers 1 to 92, all but four (technetium, promethium, astatine, and francium) occur in easily detectable quantities on Earth, having stable, or very long half-life isotopes, or are created as common products of the decay of uranium.

All of the elements with higher atomic numbers, however, have been first discovered in the laboratory, other than neptunium and plutonium. They are all radioactive, with a half-life much shorter than the age of the Earth, so any atoms of these elements, if they ever were present at the Earth's formation, have long since decayed. Trace amounts of neptunium and plutonium form in some uranium-rich rock, and small amounts are produced during atmospheric tests of atomic weapons. The Np and Pu generated are from neutron capture in uranium ore with two subsequent beta decays (238U239U239Np239Pu).

Those that can be found on Earth now are artificially generated synthetic elements, via nuclear reactors or particle accelerators. The half lives of these elements show a general trend of decreasing with atomic number. There are exceptions, however, including dubnium and several isotopes of curium. Further anomalous elements in this series have been predicted by Glenn T. Seaborg, and are categorised as the “island of stability.”

Heavy transuranic elements are difficult and expensive to produce, and their prices go up rapidly with atomic number. As of 2008, weapons-grade plutonium cost around $4,000/gram (or roughly 150 times more than gold),[1] and californium cost $60,000/gram.[2] Due to production difficulties, none of the elements beyond californium have industrial applications or were ever produced in macroscopic quantities.

Transuranic elements that have not been discovered, or have been discovered but are not yet officially named, use IUPAC's systematic element names. The naming of transuranic elements is a source of controversy.

Discovery and naming of transuranium elements

The majority of the transuranium elements were produced by three groups:

List of the transuranic elements

*The existence of these elements has been confirmed, however the names and symbols given are provisional as no names for the elements have been agreed on.

Super-heavy atoms

Position of the super-heavy elements in the periodic table.

Super-heavy atoms, (super heavy elements, commonly abbreviated SHE), are the transactinide elements beginning with rutherfordium (atomic number 104).[citation needed] They have only been made artificially, and currently serve no useful purpose because their short half-lives cause them to decay after a few minutes to just a few milliseconds, which also makes them extremely hard to study.[3][4]

Super-heavy atoms have all been created during the latter half of the 20th century and are continually being created during the 21st century as technology advances. They are created through the bombardment of elements in a particle accelerator, for example the nuclear fusion of californium-249 and carbon-12 creates rutherfordium. These elements are created in quantities on the atomic scale and no method of mass creation has been found.[3]

See also

References

  1. ^ "Price of Plutonium". The Physics Factbook.
  2. ^ Rodger C. Martin and Steven E. Kos. "Applications and Availability of Californium-252 Neutron Sources for Waste Characterization" (pdf).
  3. ^ a b Heenen, P. H.; Nazarewicz, W. (2002). "Quest for superheavy nuclei". Europhysics News. 33: 5. doi:10.1051/epn:2002102.
  4. ^ Greenwood, N. N. (1997). "Recent developments concerning the discovery of elements 100-111". Pure and Applied Chemistry. 69: 179. doi:10.1351/pac199769010179.

Further reading