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・ Synthetic catalytic scavenger
・ Synthetic CDO
・ Synthetic chord
・ Synthetic Communications
・ Synthetic control method
・ Synthetic crude
・ Synthetic currency pair
・ Synthetic data
・ Synthetic diamond
・ Synthetic differential geometry
・ Synthetic Dimensions
・ Synthetic division
・ Synthetic Division (album)
・ Synthetic dreads
・ Synthetic ecosystems
Synthetic element
・ Synthetic Entertainment
・ Synthetic environment
・ Synthetic Environment for Analysis and Simulations
・ Synthetic fabric
・ Synthetic fence
・ Synthetic fiber
・ Synthetic file system
・ Synthetic fuel
・ Synthetic fuel commercialization
・ Synthetic Fuels Corporation
・ Synthetic fuels in the United States
・ Synthetic gauge field
・ Synthetic gene database
・ Synthetic Generation


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Synthetic element : ウィキペディア英語版
Synthetic element

In chemistry, a synthetic element is a chemical element that does not occur naturally on Earth, and can only be created artificially. So far, 24 synthetic elements have been created (those with atomic numbers 95–118). All are unstable, decaying with half-lives ranging from 15.6 million years to a few hundred microseconds.
Five other elements were first created artificially and thus considered synthetic, but later discovered to exist naturally (in trace quantities) as well; among them plutonium—first synthesized in 1940—the one best known to laypeople, because of its use in atomic bombs and nuclear reactors.
==Properties==
Synthetic elements are radioactive and decay rapidly into lighter elements—possessing half-lives so short, relative to the age of the Earth (which formed approximately 4.6 billion years ago), that any atoms of these elements that may have existed when the Earth formed have long since decayed. Atoms of synthetic elements only occur on Earth as the product of atomic bombs or 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.
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. 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. Plutonium is an outlier: Its half-life, depending on the isotope, can be as long as 80.8 million years. (The ''principal'' plutonium isotope in use has a half-life of 24,100 years.)

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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