Plutonium-242

Source: Wikipedia, the free encyclopedia.
Plutonium-242, 242Pu
General
Decay mode
Decay energy (MeV)
Isotopes of plutonium
Complete table of nuclides
Actinides[1] by decay chain Half-life
range (a)
Fission products of 235U by yield[2]
4n
4n + 1
4n + 2
4n + 3
4.5–7% 0.04–1.25% <0.001%
228
Ra
4–6 a
155
Euþ
244
Cmƒ
241Puƒ
250
Cf
227
Ac
10–29 a
90Sr 85Kr
113m
Cdþ
232Uƒ 238Puƒ
243
Cmƒ
29–97 a
137
Cs
151
Smþ
121m
Sn
248Bk[3]
249
Cfƒ
242m
Amƒ
141–351 a

No fission products have a half-life
in the range of 100 a–210 ka ...

241Amƒ
251Cfƒ[4]
430–900 a
226Ra
247
Bk
1.3–1.6 ka
240Pu
229
Th
246
Cmƒ
243
Amƒ
4.7–7.4 ka
245
Cmƒ
250
Cm
8.3–8.5 ka
239Puƒ 24.1 ka
230
Th
231
Pa
32–76 ka
236
Npƒ
233Uƒ 234U 150–250 ka 99Tc
126
Sn
248
Cm
242Pu 327–375 ka 79Se
1.53 Ma
93
Zr
237
Npƒ
2.1–6.5 Ma
135
Cs
107
Pd
236U
247
Cmƒ
15–24 Ma 129I
244Pu 80 Ma

... nor beyond 15.7 Ma[5]

232Th 238U 235Uƒ№ 0.7–14.1 Ga
(thermal neutron capture cross section greater than 3k barns)

Plutonium-242 (242Pu or Pu-242) is one of the isotopes of plutonium, the second longest-lived, with a half-life of 375,000 years. The half-life of 242Pu is about 15 times that of 239Pu; so 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

cross section
is also low.

In the nuclear fuel cycle

Transmutation flow in LWR

Plutonium-242 is produced by successive

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

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 mainly decays into

uranium series. Plutonium-242 decays via spontaneous fission in about 5.5 × 10−4% of cases[7]
.

References

  1. ^ 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 nuclides have half-lives of at least four years (the longest-lived nuclide 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.
  2. thermal neutron fission of uranium-235, e.g. in a typical nuclear reactor
    .
  3. .
    "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 [years]. No growth of Cf248 was detected, and a lower limit for the β half-life can be set at about 104 [years]. No alpha activity attributable to the new isomer has been detected; the alpha half-life is probably greater than 300 [years]."
  4. sea of instability
    ".
  5. ^ Excluding those "classically stable" nuclides with half-lives significantly in excess of 232Th; e.g., while 113mCd has a half-life of only fourteen years, that of 113Cd is eight quadrillion years.
  6. ^ "PLUTONIUM ISOTOPIC RESULTS OF KNOWN SAMPLES USING THE SNAP GAMMA SPECTROSCOPY ANALYSIS CODE AND THE ROBWIN SPECTRUM FITTING ROUTINE" (PDF). Archived from the original (PDF) on 2017-08-13. Retrieved 2013-03-15.
  7. ^ Chart of all nuclei which includes half life and mode of decay