Synthetic element
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In chemistry, a synthetic element is a chemical element that is too unstable to occur naturally on Earth, and therefore has to be created artificially. So far 30 synthetic elements have been discovered—that is, synthesized. Ten of them are "quasi-synthetic"—meaning that they occur naturally on Earth in trace quantities and generally have to be produced artificially,—and 20 are "fully synthetic"—meaning that they do not occur naturally on Earth at all, and can only be produced artificially. Of all the synthetic elements, plutonium—first synthesized in 1940—is the one best known to lay people, because of its use in atomic bombs and nuclear reactors.
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[edit] Properties
Synthetic elements are radioactive and decay very rapidly into lighter elements—possessing half-lives so short, relative to the age of the Earth (which formed 4.54 billion years ago), that any atoms of these elements that may have existed when the Earth formed have long since decayed. Because of this, atoms of synthetic elements only occur on Earth as the product of experiments that involve nuclear reactors or particle accelerators, via nuclear fusion or neutron absorption.
Atomic mass for natural life is based on weighted average abundance of natural isotopes that occur in the Earth's crust and atmosphere. For synthetic elements, the isotope depends on the means of synthesis, so the concept of natural isotope abundance has no meaning. Therefore, for synthetic elements the total nucleus count (protons plus neutrons) of the most stable isotope, i.e. the isotope with the longest half-life—is listed in brackets as the atomic mass.
(Note: Not all radioactive elements are synthetic. For instance, uranium and thorium have no stable isotopes but occur naturally in the Earth's crust and atmosphere; therefore, neither are synthetic. Unstable elements such as polonium, radium, and radon—which form through the decay of uranium and thorium—are also found in nature, despite their short half-lives.)
[edit] History
| This section requires expansion with: additional examples of elements synthesized over time. |
The first element discovered through synthesis was technetium—its discovery being definitely confirmed in 1936. This discovery filled a gap in the periodic table, and the fact that no stable isotopes of technetium exist explains its natural absence on Earth (and the gap). With the longest-lived isotope of technetium, Tc-98, having a 4.2 million year half-life, no technetium remains from the formation of the Earth. Only minute traces of technetium occur naturally in the Earth's crust—as a spontaneous fission product of uranium-238 or by neutron capture in molybdenum ores—but technetium is present naturally in red giant stars.
[edit] List of synthetic elements
[edit] Quasi-synthetic elements
All elements with atomic numbers 1 through 98, including these, are naturally occurring at least in trace quantities, but are usually produced through synthesis.
| Element name | Chemical Symbol |
Atomic Number |
First definite discovery |
|---|---|---|---|
| Technetium | Tc | 43 | 1936 |
| Promethium | Pm | 61 | 1945 |
| Astatine | At | 85 | 1940 |
| Francium | Fr | 87 | 1939 |
| Neptunium | Np | 93 | 1940 |
| Plutonium | Pu | 94 | 1940 |
| Americium | Am | 95 | 1944 |
| Curium | Cm | 96 | 1944 |
| Berkelium | Bk | 97 | 1949 |
| Californium | Cf | 98 | 1950 |
[edit] Fully synthetic elements
All elements in the following categories do not occur naturally on Earth, and have atomic numbers of 99 and higher.
[edit] Transuranium elements
| Element name | Chemical Symbol |
Atomic Number |
First definite synthesis |
|---|---|---|---|
| Einsteinium | Es | 99 | 1952 |
| Fermium | Fm | 100 | 1952 |
[edit] Transfermium elements
| Element name | Chemical Symbol |
Atomic Number |
First definite synthesis |
|---|---|---|---|
| Mendelevium | Md | 101 | 1955 |
| Nobelium | No | 102 | 1966 |
| Lawrencium | Lr | 103 | 1961 |
[edit] Transactinide elements
| Element name | Chemical Symbol |
Atomic Number |
First definite synthesis |
|---|---|---|---|
| Rutherfordium | Rf | 104 | 1966 (USSR)/ 1969 (USA) * |
| Dubnium | Db | 105 | 1968 (USSR)/ 1970 (USA) * |
| Seaborgium | Sg | 106 | 1974 |
| Bohrium | Bh | 107 | 1981 |
| Hassium | Hs | 108 | 1984 |
| Meitnerium | Mt | 109 | 1982 |
| Darmstadtium | Ds | 110 | 1994 |
| Roentgenium | Rg | 111 | 1994 |
| Copernicium | Cn | 112 | 1996 |
(* The United States and Soviet Union made discoveries of rutherfordium and dubnium independently and were given shared credit by IUPAC/IUPAP in 1992. In 1997, IUPAC decided to give dubnium its current name honoring the city of Dubna where the Russian team made their discoveries since American-chosen names had already been used for many existing synthetic elements, but accepted the name rutherfordium chosen by the American team.)
[edit] Recently observed synthetic elements
Note: Names and symbols for these elements are provisional.
| Element name | Chemical Symbol |
Atomic Number |
First definite synthesis |
|---|---|---|---|
| Ununtrium | Uut | 113 | 2003 |
| Ununquadium | Uuq | 114 | 1999 |
| Ununpentium | Uup | 115 | 2003 |
| Ununhexium | Uuh | 116 | 2000 |
| Ununseptium | Uus | 117 | 2010 |
| Ununoctium | Uuo | 118 | 2002 |