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Isotopes of neptunium
Artificial nuclides with atomic number of 93 but with different mass numbers

Neptunium (93Np) is usually considered an artificial element, although trace quantities are found in nature, so a standard atomic weight cannot be given. Like all trace or artificial elements, it has no stable isotopes. The first isotope to be synthesized and identified was 239Np in 1940, produced by bombarding 238U with neutrons to produce 239U, which then underwent beta decay to 239Np.

Trace quantities are found in nature from neutron capture reactions by uranium atoms, a fact not discovered until 1951.

Twenty-five neptunium radioisotopes have been characterized, with the most stable being 237Np with a half-life of 2.14 million years, 236Np with a half-life of 154,000 years, and 235Np with a half-life of 396.1 days. All of the remaining radioactive isotopes have half-lives that are less than 4.5 days, and the majority of these have half-lives that are less than 50 minutes. This element also has five meta states, with the most stable being 236mNp (t1/2 22.5 hours).

The isotopes of neptunium range from 219Np to 244Np, though the intermediate isotope 221Np has not yet been observed. The primary decay mode before the most stable isotope, 237Np, is electron capture (with a good deal of alpha emission), and the primary mode after is beta emission. The primary decay products before 237Np are isotopes of uranium and protactinium, and the primary products after are isotopes of plutonium. Neptunium is the heaviest element for which the location of the proton drip line is known; the lightest bound isotope is 220Np.

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List of isotopes

Nuclide3ZNIsotopic mass (Da)45Half-life6Decaymode78Daughterisotope9Spin andparity101112Isotopicabundance
Excitation energy13
219Np1493126219.031602(99)570(450) μsα215Pa9/2−#
220Np1593127220.032716(33)25+14−7 μsα216Pa1−#
222Np93129222.033575(41)480(190) nsα218Pa1−#
223Np93130223.032913(89)2.5(8) μsα219Pa(9/2−)
224Np1693131224.034388(31)38+26−11 μsα (83%)220m1Pa2−#
α (17%)220m2Pa
225Np93132225.033943(98)6.5(35) msα221Pa9/2−#
226Np93133226.03523(11)35(10) msα222Pa
227Np93134227.034975(83)510(60) msα223Pa5/2+#
228Np93135228.03631(11)#61.4(14) sEC (59%)228U4+#
α (41%)224Pa
β+, SF (0.0126%)(various)
229Np93136229.03629(11)4.00(18) minα (68%)225Pa5/2+#
β+ (32%)229U
230Np93137230.037828(59)4.6(3) minβ+ (>97%)230U4+#
α (<3%)226Pa
231Np93138231.038244(55)48.8(2) minβ+ (98%)231U5/2+#
α (2%)227Pa
232Np93139232.04011(11)#14.7(3) minβ+232U(5−)
233Np93140233.040739(55)36.2(1) minβ+233U5/2+#
α (0.0007%)229Pa
234Np93141234.0428932(90)4.4(1) dβ+234U(0+)
234mNp17~9 minIT234Np5+
EC234U
235Np93142235.0440615(15)396.1(12) dEC235U5/2+
α (0.00260%)231Pa
236Np1893143236.046568(54)1.53(5)×105 yEC (86.3%)236U(6−)
β− (13.5%)236Pu
α (0.16%)232Pa
236mNp1960(50) keV22.5(4) hEC (50%)236U(1−)
β− (50%)236Pu
237Np93144237.0481716(12)2.144(7)×106 yα233Pa5/2+Trace20
SF (<2×10−10%)(various)
CD (<4×10−12%)207Tl30Mg
237mNp945.20(10) keV710(40) nsIT237Np13/2−
238Np93145238.0509446(12)2.099(2) dβ−238Pu2+
238mNp2300(200)# keV112(39) nsSF(various)
239Np93146239.0529375(14)2.356(3) dβ−239Pu5/2+Trace21
240Np93147240.056164(18)61.9(2) minβ−240Pu(5+)Trace22
240mNp2318(14) keV7.22(2) minβ− (99.88%)240Pu(1+)
IT (0.12%)240Np
241Np93148241.058349(33)2413.9(2) minβ−241Pu(5/2+)
242Np93149242.061738(87)252.2(2) minβ−242Pu(1+)
242mNp2650(50)# keV5.5(1) minβ−242Pu(6+)
243Np93150243.064204(34)#1.85(15) minβ−243Pu5/2+#
244Np93151244.06789(11)#2.29(16) minβ−244Pu7−#
This table header & footer:
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Actinides vs fission products

Actinides and fission products by half-life
  • v
  • t
  • e
Actinides27 by decay chainHalf-life range (a)Fission products of 235U by yield28
4n4n + 14n + 24n + 34.5–7%0.04–1.25%<0.001%
228Ra№4–6 a155Euþ
248Bk29> 9 a
244Cmƒ241Puƒ250Cf227Ac№10–29 a90Sr85Kr113mCdþ
232238Puƒ243Cmƒ29–97 a137Cs151Smþ121mSn
249Cfƒ242mAmƒ141–351 a

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

241Amƒ251Cfƒ30430–900 a
226Ra№247Bk1.3–1.6 ka
240Pu229Th246Cmƒ243Amƒ4.7–7.4 ka
245Cmƒ250Cm8.3–8.5 ka
239Puƒ24.1 ka
230Th№231Pa№32–76 ka
236Npƒ233234U№150–250 ka99Tc₡126Sn
248Cm242Pu327–375 ka79Se₡
1.33 Ma135Cs₡
237Npƒ1.61–6.5 Ma93Zr107Pd
236U247Cmƒ15–24 Ma129I₡
244Pu80 Ma

... nor beyond 15.7 Ma31

232Th№238U№235Uƒ№0.7–14.1 Ga

Notable isotopes

Neptunium-235

Neptunium-235 has 142 neutrons and a half-life of 396.1 days. This isotope decays by:

This isotope of neptunium has a weight of 235.044 063 3 u.

Neptunium-236

Neptunium-236 has 143 neutrons and a half-life of 154,000 years. It can decay by the following methods:

  • Electron capture: the decay energy is 0.93 MeV and the decay product is uranium-236. This usually decays (with a half-life of 23 million years) to thorium-232.
  • Beta emission: the decay energy is 0.48 MeV and the decay product is plutonium-236. This usually decays (half-life 2.8 years) to uranium-232, which usually decays (half-life 69 years) to thorium-228, which decays in a few years to lead-208.
  • Alpha emission: the decay energy is 5.007 MeV and the decay product is protactinium-232. This decays with a half-life of 1.3 days to uranium-232.

This particular isotope of neptunium has a mass of 236.04657 u. It is a fissile material; it has an estimated critical mass of 6.79 kg (15.0 lb),32 though precise experimental data is not available.33

236Np is produced in small quantities via the (n,2n) and (γ,n) capture reactions of 237Np,34 however, it is nearly impossible to separate in any significant quantities from its parent 237Np.35 It is for this reason that despite its low critical mass and high neutron cross section, it has not been researched extensively as a nuclear fuel in weapons or reactors.36 Nevertheless, 236Np has been considered for use in mass spectrometry and as a radioactive tracer, because it decays predominantly by beta emission with a long half-life.37 Several alternative production routes for this isotope have been investigated, namely those that reduce isotopic separation from 237Np or the isomer 236mNp. The most favorable reactions to accumulate 236Np were shown to be proton and deuteron irradiation of uranium-238.38

Neptunium-237

237Np decays via the neptunium series, which terminates with thallium-205, which is stable, unlike most other actinides, which decay to stable isotopes of lead.

In 2002, 237Np was shown to be capable of sustaining a chain reaction with fast neutrons, as in a nuclear weapon, with a critical mass of around 60 kg.39 However, it has a low probability of fission on bombardment with thermal neutrons, which makes it unsuitable as a fuel for light water nuclear power plants (as opposed to fast reactor or accelerator-driven systems, for example).

Inventory in spent nuclear fuel

237Np is the only neptunium isotope produced in significant quantity in the nuclear fuel cycle, both by successive neutron capture by uranium-235 (which fissions most but not all of the time) and uranium-236, or (n,2n) reactions where a fast neutron occasionally knocks a neutron loose from uranium-238 or isotopes of plutonium. Over the long term, 237Np also forms in spent nuclear fuel as the decay product of americium-241.

237Np is considered to be one of the most mobile radionuclides at the site of the Yucca Mountain nuclear waste repository (Nevada) where oxidizing conditions prevail in the unsaturated zone of the volcanic tuff above the water table.

Raw material for 238Pu production

Main articles: Plutonium-238 and Radioisotope thermoelectric generator

When exposed to neutron bombardment 237Np can capture a neutron, undergo beta decay, and become 238Pu, this product being useful as a thermal energy source in a radioisotope thermoelectric generator (RTG or RITEG) for the production of electricity and heat. The first type of thermoelectric generator SNAP (Systems for Nuclear Auxiliary Power) was developed and used by NASA in the 1960's and during the Apollo missions to power the instruments left on the Moon surface by the astronauts. Thermoelectric generators were also embarked on board of deep space probes such as for the Pioneer 10 and 11 missions, the Voyager program, the Cassini–Huygens mission, and New Horizons. They also deliver electrical and thermal power to the Mars Science Laboratory (Curiosity rover) and Mars 2020 mission (Perseverance rover) both exploring the cold surface of Mars. Curiosity and Perseverance rovers are both equipped with the last version of multi-mission RTG, a more efficient and standardized system dubbed MMRTG.

These applications are economically practical where photovoltaic power sources are weak or inconsistent due to probes being too far from the sun or rovers facing climate events that may obstruct sunlight for long periods (like Martian dust storms). Space probes and rovers also make use of the heat output of the generator to keep their instruments and internals warm.40

Shortage of 237Np stockpiles

The long half-life (T1/2 ~ 88 years) of 238Pu and the absence of γ-radiation that could interfere with the operation of on-board electronic components, or irradiate people, makes it the radionuclide of choice for electric thermogenerators.

237Np is therefore a key radionuclide for the production of 238Pu, which is essential for deep space probes requiring a reliable and long-lasting source of energy without maintenance.

Stockpiles of 238Pu built up in the United States since the Manhattan Project, thanks to the Hanford nuclear complex (operating in Washington State from 1943 to 1977) and the development of atomic weapons, are now almost exhausted. The extraction and purification of sufficient new quantities of 237Np from irradiated nuclear fuels is therefore necessary for the resumption of 238Pu production in order to replenish the stocks needed for space exploration by robotic probes.

Neptunium-239

Neptunium-239 has 146 neutrons and a half-life of 2.356 days. It is produced via β− decay of the short-lived uranium-239, and undergoes another β− decay to plutonium-239. This is the primary route for making plutonium, as 239U can be made by neutron capture in uranium-238.41

Uranium-237 and neptunium-239 are regarded as the leading hazardous radioisotopes in the first hour-to-week period following nuclear fallout from a nuclear detonation, with 239Np dominating "the spectrum for several days".4243

References

  1. Peppard, D. F.; Mason, G. W.; Gray, P. R.; Mech, J. F. (1952). "Occurrence of the (4n + 1) series in nature" (PDF). Journal of the American Chemical Society. 74 (23): 6081–6084. doi:10.1021/ja01143a074. https://digital.library.unt.edu/ark:/67531/metadc172698/m2/1/high_res_d/metadc172698.pdf

  2. Zhang, Z. Y.; Gan, Z. G.; Yang, H. B.; et al. (2019). "New isotope 220Np: Probing the robustness of the N = 126 shell closure in neptunium". Physical Review Letters. 122 (19): 192503. Bibcode:2019PhRvL.122s2503Z. doi:10.1103/PhysRevLett.122.192503. PMID 31144958. S2CID 169038981. /wiki/Physical_Review_Letters

  3. mNp – Excited nuclear isomer. /wiki/Nuclear_isomer

  4. ( ) – Uncertainty (1σ) is given in concise form in parentheses after the corresponding last digits.

  5. # – Atomic mass marked #: value and uncertainty derived not from purely experimental data, but at least partly from trends from the Mass Surface (TMS).

  6. 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. https://www-nds.iaea.org/amdc/ame2020/NUBASE2020.pdf

  7. 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. https://www-nds.iaea.org/amdc/ame2020/NUBASE2020.pdf

  8. Modes of decay: EC:Electron captureCD:Cluster decayIT:Isomeric transitionSF:Spontaneous fission /wiki/Electron_capture

  9. Bold italics symbol as daughter – Daughter product is nearly stable.

  10. 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. https://www-nds.iaea.org/amdc/ame2020/NUBASE2020.pdf

  11. ( ) spin value – Indicates spin with weak assignment arguments.

  12. # – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).

  13. # – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).

  14. Heaviest known nucleus, as of 2025[update], that is beyond the proton drip line.[4] https://en.wikipedia.org/w/index.php?title=Isotopes_of_neptunium&action=edit

  15. Zhang, Z. Y.; Gan, Z. G.; Yang, H. B.; et al. (2019). "New isotope 220Np: Probing the robustness of the N = 126 shell closure in neptunium". Physical Review Letters. 122 (19): 192503. Bibcode:2019PhRvL.122s2503Z. doi:10.1103/PhysRevLett.122.192503. PMID 31144958. S2CID 169038981. /wiki/Physical_Review_Letters

  16. Huang, T. H.; et al. (2018). "Identification of the new isotope 224Np" (pdf). Physical Review C. 98 (4): 044302. Bibcode:2018PhRvC..98d4302H. doi:10.1103/PhysRevC.98.044302. S2CID 125251822. https://www.researchgate.net/publication/328038265

  17. Asai, M.; Suekawa, Y.; Higashi, M.; et al. (2020). Discovery of 234 Np isomer and its decay properties (PDF) (Report) (in Japanese). http://www.radiochem.org/jnrs-abst/pdf/64-501.pdf

  18. Fissile nuclide /wiki/Fissile

  19. Order of ground state and isomer is uncertain.

  20. Produced by neutron capture in uranium ore /wiki/Neutron_capture

  21. Produced by neutron capture in uranium ore /wiki/Neutron_capture

  22. Intermediate decay product of 244Pu /wiki/Plutonium-244

  23. Order of ground state and isomer is uncertain.

  24. Niwase, T.; Watanabe, Y. X.; Hirayama, Y.; et al. (2023). "Discovery of New Isotope 241U and Systematic High-Precision Atomic Mass Measurements of Neutron-Rich Pa-Pu Nuclei Produced via Multinucleon Transfer Reactions" (PDF). Physical Review Letters. 130 (13): 132502-1 – 132502-6. doi:10.1103/PhysRevLett.130.132502. PMID 37067317. S2CID 257976576. https://eprints.whiterose.ac.uk/197980/1/PhysRevLett.130.132502.pdf

  25. Niwase, T.; Watanabe, Y. X.; Hirayama, Y.; et al. (2023). "Discovery of New Isotope 241U and Systematic High-Precision Atomic Mass Measurements of Neutron-Rich Pa-Pu Nuclei Produced via Multinucleon Transfer Reactions" (PDF). Physical Review Letters. 130 (13): 132502-1 – 132502-6. doi:10.1103/PhysRevLett.130.132502. PMID 37067317. S2CID 257976576. https://eprints.whiterose.ac.uk/197980/1/PhysRevLett.130.132502.pdf

  26. Order of ground state and isomer is uncertain.

  27. 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. /wiki/Polonium

  28. Specifically from thermal neutron fission of uranium-235, e.g. in a typical nuclear reactor. /wiki/Thermal_neutron

  29. Milsted, J.; Friedman, A. M.; Stevens, C. M. (1965). "The alpha half-life of berkelium-247; a new long-lived isomer of berkelium-248". Nuclear Physics. 71 (2): 299. Bibcode:1965NucPh..71..299M. doi:10.1016/0029-5582(65)90719-4."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]." /wiki/Bibcode_(identifier)

  30. This is the heaviest nuclide with a half-life of at least four years before the "sea of instability". /wiki/Sea_of_instability

  31. 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. /wiki/Primordial_nuclide

  32. Final Report, Evaluation of nuclear criticality safety data and limits for actinides in transport (PDF) (Report). Republic of France, Institut de Radioprotection et de Sûreté Nucléaire, Département de Prévention et d'étude des Accidents. Archived from the original (PDF) on 2011-05-19. https://web.archive.org/web/20110519171204/http://ec.europa.eu/energy/nuclear/transport/doc/irsn_sect03_146.pdf

  33. Reed, B. C. (2017). "An examination of the potential fission-bomb weaponizability of nuclides other than 235U and 239Pu". American Journal of Physics. 85: 38–44. doi:10.1119/1.4966630. /wiki/Doi_(identifier)

  34. Analysis of the Reuse of Uranium Recovered from the Reprocessing of Commercial LWR Spent Fuel, United States Department of Energy, Oak Ridge National Laboratory. http://info.ornl.gov/sites/publications/files/Pub14204.pdf

  35. **Jukka Lehto; Xiaolin Hou (2011). "15.15: Neptunium". Chemistry and Analysis of Radionuclides (1st ed.). John Wiley & Sons. 231. ISBN 978-3527633029. 978-3527633029

  36. Reed, B. C. (2017). "An examination of the potential fission-bomb weaponizability of nuclides other than 235U and 239Pu". American Journal of Physics. 85: 38–44. doi:10.1119/1.4966630. /wiki/Doi_(identifier)

  37. Jerome, S.M.; Ivanov, P.; Larijani, C.; Parker, D.J.; Regan, P.H. (2014). "The production of Neptunium-236g". Journal of Environmental Radioactivity. 138: 315–322. doi:10.1016/j.jenvrad.2014.02.029. PMID 24731718. /wiki/Journal_of_Environmental_Radioactivity

  38. Jerome, S.M.; Ivanov, P.; Larijani, C.; Parker, D.J.; Regan, P.H. (2014). "The production of Neptunium-236g". Journal of Environmental Radioactivity. 138: 315–322. doi:10.1016/j.jenvrad.2014.02.029. PMID 24731718. /wiki/Journal_of_Environmental_Radioactivity

  39. P. Weiss (26 October 2002). "Neptunium Nukes? Little-studied metal goes critical". Science News. 162 (17): 259. doi:10.2307/4014034. JSTOR 4014034. Archived from the original on 26 May 2024. Retrieved 7 November 2013. https://archive.today/20240526102438/https://www.webcitation.org/6Cw9Vnt0Q?url=http://www.sciencenews.org/view/generic/id/3246/title/Neptunium_Nukes%3F_Little-studied_metal_goes_critical

  40. Witze, Alexandra (2014-11-27). "Nuclear power: Desperately seeking plutonium". Nature. 515 (7528): 484–486. Bibcode:2014Natur.515..484W. doi:10.1038/515484a. PMID 25428482. https://doi.org/10.1038%2F515484a

  41. "Periodic Table Of Elements: LANL - Neptunium". Los Alamos National Laboratory. Retrieved 2013-10-13. http://periodic.lanl.gov/93.shtml

  42. [Film Badge Dosimetry in Atmospheric Nuclear Tests, By Committee on Film Badge Dosimetry in Atmospheric Nuclear Tests, Commission on Engineering and Technical Systems, Division on Engineering and Physical Sciences, National Research Council. pg24-35]

  43. Bounding Analysis of Effects of Fractionation of Radionuclides in Fallout on Estimation of Doses to Atomic Veterans DTRA-TR-07-5. 2007 http://www.dtra.mil/Portals/61/Documents/NTPR/4-Rad_Exp_Rpts/30_DTRA-TR-07-5_Fractionation_Report.pdf