Isotopes of plutonium

Isotopes of plutonium (94Pu)
Main isotopes[1] Decay
abun­dance half-life (t1/2) mode pro­duct
236Pu synth 2.858 y α 232U
SF
238Pu trace 87.7 y[2] α 234U
SF
239Pu trace 2.411×104 y α 235U
SF
240Pu trace 6.561×103 y α 236U
SF
241Pu synth 14.329 y β 241Am
α 237U
SF
242Pu synth 3.75×105 y α 238U
SF
244Pu trace 8.13×107 y α 240U
SF

Plutonium (94Pu) is an artificial element, except for trace quantities resulting from neutron capture by uranium, and thus a standard atomic weight cannot be given.[note 1] Like all artificial elements, it has no stable isotopes. It was synthesized before being found in nature, with the first isotope synthesized being 238Pu in 1940. Twenty-two plutonium radioisotopes have been characterized. The most stable are 244Pu with a half-life of 80.8 million years; 242Pu with a half-life of 373,300 years; and 239Pu with a half-life of 24,110 years; and 240Pu with a half-life of 6,560 years. This element also has eight meta states; all have half-lives of less than one second.

The known isotopes of plutonium range from 226Pu to 247Pu. The primary decay modes before the most stable isotope, 244Pu, are spontaneous fission and alpha decay; the primary mode after is beta emission. The primary decay products before 244Pu are isotopes of uranium and neptunium (not considering fission products), and the primary decay products after are isotopes of americium.

  1. ^ Kondev, F. G.; Wang, M.; Huang, W. J.; Naimi, S.; Audi, G. (2021). "The NUBASE2020 evaluation of nuclear properties" (PDF). Chinese Physics C. 45 (3): 030001. doi:10.1088/1674-1137/abddae.
  2. ^ Magurno & Pearlstein 1981, pp. 835 ff.
  3. ^ Wu, Yang; Dai, Xiongxin; Christl, Marcus; Synal, Hans-Arno; Xing, Shan; Hou, Shaochun (17 June 2021). "Ultrasensitive Analytical Method for Direct Search of Primordial 244 Pu in Bastnaesite". ACS Earth and Space Chemistry. 5 (6): 1316–1324. doi:10.1021/acsearthspacechem.0c00288.


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