Plutonium-242
Actinides and fission products by half-life
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Actinides[1] by decay chain | Half-life range (y) |
Fission products of 235U by yield[2] | ||||||
4n | 4n+1 | 4n+2 | 4n+3 | |||||
4.5–7% | 0.04–1.25% | <0.001% | ||||||
228Ra№ | 4–6 | † | 155Euþ | |||||
244Cm | 241Puƒ | 250Cf | 227Ac№ | 10–29 | 90Sr | 85Kr | 113mCdþ | |
232Uƒ | 238Pu№ | 243Cmƒ | 29–97 | 137Cs | 151Smþ | 121mSn | ||
248Bk[3] | 249Cfƒ | 242mAmƒ | 141–351 |
No fission products |
||||
241Amƒ | 251Cfƒ[4] | 430–900 | ||||||
226Ra№ | 247Bk | 1.3 k – 1.6 k | ||||||
240Pu | 229Th№ | 246Cm | 243Amƒ | 4.7 k – 7.4 k | ||||
245Cmƒ | 250Cm | 8.3 k – 8.5 k | ||||||
239Puƒ№ | 24.1 k | |||||||
230Th№ | 231Pa№ | 32 k – 76 k | ||||||
236Npƒ | 233Uƒ№ | 234U№ | 150 k – 250 k | ‡ | 99Tc₡ | 126Sn | ||
248Cm | 242Pu | 327 k – 375 k | 79Se₡ | |||||
1.53 M | 93Zr | |||||||
237Np№ | 2.1 M – 6.5 M | 135Cs₡ | 107Pd | |||||
236U№ | 247Cmƒ | 15 M – 24 M | 129I₡ | |||||
244Pu№ | 80 M |
... nor beyond 15.7 M years[5] |
||||||
232Th№ | 238U№ | 235Uƒ№ | 0.7 G – 14.1 G | |||||
Legend for superscript symbols |
Plutonium-242 is one of the isotopes of plutonium, the second longest-lived, with a half-life of 373,300 years. 242Pu's halflife is about 15 times as long as Pu-239's halflife; therefore, it is one-fifteenth as radioactive and not one of the larger contributors to nuclear waste radioactivity. 242Pu's gamma ray emissions are also weaker than those of the other isotopes.[6]
It is not fissile (though it is fissionable by fast neutrons) and its neutron capture cross section is also low.
In the nuclear fuel cycle
Plutonium-242 is produced by successive neutron capture on 239Pu, 240Pu, and 241Pu. The odd-mass isotopes 239Pu and 241Pu have about a 3/4 chance of undergoing fission on capture of a thermal neutron and about a 1/4 chance of retaining the neutron and becoming the following isotope. The proportion of 242Pu is low at low burnup but increases nonlinearly.
Plutonium-242 has a particularly low cross section for thermal neutron capture; and it takes four neutron absorptions to become another fissile isotope (either curium-245 or plutonium-241) and undergo fission. Even then, there is a chance either of those two fissile isotopes will fail to fission but instead absorb the fourth neutron, becoming curium-246 (on the way to even heavier actinides like californium, which is a neutron emitter by spontaneous fission and difficult to handle) or becoming 242Pu again; so the mean number of neutrons absorbed before fission is even higher than 4. Therefore Pu-242 is particularly unsuited to recycling in a thermal reactor and would be better used in a fast reactor where it can be fissioned directly. However, 242Pu's low cross section means that relatively little of it will be transmuted during one cycle in a thermal reactor.
Decay
Plutonium-242 primarily decays into uranium-238 via alpha decay, before continuing along the Uranium series. Plutonium-242 will occasionally decay via spontaneous fission with a rate of 5.5 × 10−4%.[7]
References
- ↑ Plus radium (element 88). While actually a sub-actinide, it immediately precedes actinium (89) and follows a three-element gap of instability after polonium (84) where no isotopes have half-lives of at least four years (the longest-lived isotope in the gap is radon-222 with a half life of less than four days). Radium's longest lived isotope, at 1,600 years, thus merits the element's inclusion here.
- ↑ Specifically from thermal neutron fission of U-235, e.g. in a typical nuclear reactor.
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
"The isotopic analyses disclosed a species of mass 248 in constant abundance in three samples analysed over a period of about 10 months. This was ascribed to an isomer of Bk248 with a half-life greater than 9 y. No growth of Cf248 was detected, and a lower limit for the β− half-life can be set at about 104 y. No alpha activity attributable to the new isomer has been detected; the alpha half-life is probably greater than 300 y." - ↑ This is the heaviest isotope with a half-life of at least four years before the "Sea of Instability".
- ↑ Excluding those "classically stable" isotopes with half-lives significantly in excess of 232Th; e.g., while 113mCd has a half-life of only fourteen years, that of 113Cd is nearly eight quadrillion years.
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Chart of all nuclei which includes half life and mode of decay
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