Actinide
Neptunium is a chemical element; it has symbol Np and atomic number 93. A radioactive actinide metal, neptunium is the first transuranic element. It is named after Neptune, the planet beyond Uranus in the Solar System, which uranium is named after. A neptunium atom has 93 protons and 93 electrons, of which seven are valence electrons. Neptunium metal is silvery and tarnishes when exposed to air. The element occurs in three allotropic forms and it normally exhibits five oxidation states, ranging from +3 to +7. Like all actinides, it is radioactive, poisonous, pyrophoric, and capable of accumulating in bones, which makes the handling of neptunium dangerous.
Although many false claims of its discovery were made over the years, the element was first synthesized by Edwin McMillan and Philip H. Abelson at the Berkeley Radiation Laboratory in 1940. Since then, most neptunium has been and still is produced by neutron irradiation of uranium in nuclear reactors. The vast majority is generated as a by-product in conventional nuclear power reactors. While neptunium itself has no commercial uses at present, it is used as a precursor for the formation of plutonium-238, which is in turn used in radioisotope thermal generators to provide electricity for spacecraft. Neptunium has also been used in detectors of high-energy neutrons.
The longest-lived isotope of neptunium, neptunium-237, is a by-product of nuclear reactors and plutonium production. …
When the first periodic table of the elements was published by Dmitri Mendeleev in the early 1870s, it showed a " — " in place after uranium similar to several other places for then-undiscovered elements. Other subsequent tables of known elements, including a 1913 publication of the known radioactive isotopes by Kasimir Fajans, also show an empty place after uranium, element 92.
Up to and after the discovery of the final component of the atomic nucleus, the neutron in 1932, most scientists did not seriously consider the possibility of elements heavier than uranium. While nuclear theory at the time did not explicitly prohibit their existence, there was little evidence to suggest that they did. However, the discovery of induced radioactivity by Irène and Frédéric Joliot-Curie in late 1933 opened up an entirely new method of researching the elements and inspired a small group of Italian scientists led by Enrico Fermi to begin a series of experiments involving neutron bombardment. Although the Joliot-Curies' experiment involved bombarding a sample of 27Al with alpha particles to produce the radioactive 30P, Fermi realized that using neutrons, which have no electrical charge, would most likely produce even better results than the positively charged alpha particles. Accordingly, in March 1934 he began systematically subjecting all of the then-known elements to neutron bombardment to determine whether others could also be induced to radioactivity. …
Neptunium is a hard, silvery, ductile, radioactive actinide metal (all actinides are metals). In the periodic table, it is located to the right of the actinide uranium, to the left of the actinide plutonium and below the lanthanide promethium. Neptunium is a hard metal, having a bulk modulus of 118 GPa, comparable to that of manganese. Neptunium metal is similar to uranium in terms of physical workability. When exposed to air at normal temperatures, it forms a thin oxide layer. This reaction proceeds more rapidly as the temperature increases. Neptunium melts at 639 ± 3 °C: this low melting point, a property the metal shares with the neighboring element plutonium (which has melting point 639.4 °C), is due to the hybridization of the 5f and 6d orbitals and the formation of directional bonds in the metal. The boiling point of neptunium is not empirically known and the usually given value of 4174 °C is extrapolated from the vapor pressure of the element. If accurate, this would give neptunium the largest liquid range of any element (3535 K passes between its melting and boiling points).
Neptunium is found in at least three allotropes. Some claims of a fourth allotrope have been made, but they are so far not proven. This multiplicity of allotropes is common among the actinides. The crystal structures of neptunium, protactinium, uranium, and plutonium do not have clear analogs among the lanthanides and are more similar to those of the 3d transition metals. …
The longest-lived isotope of neptunium, 237Np, has a half-life of 2.14 million years, which is more than 2,000 times shorter than the age of the Earth. Therefore, any primordial neptunium would have decayed in the distant past. After only about 80 million years, the concentration of even the longest-lived isotope, 237Np, would have been reduced to less than one-trillionth (10−12) of its original amount. Thus neptunium is present in nature only in negligible amounts produced as intermediate decay products of other isotopes.
Trace amounts of the neptunium isotopes neptunium-237 and -239 are found naturally as decay products from transmutation reactions in uranium ores. 239Np and 237Np are the most common of these isotopes; they are directly formed from neutron capture by uranium-238 atoms. These neutrons come from the spontaneous fission of uranium-238, naturally neutron-induced fission of uranium-235, cosmic ray spallation of nuclei, and light elements absorbing alpha particles and emitting a neutron. The half-life of 239Np is very short, although the detection of its much longer-lived daughter 239Pu in nature in 1951 definitively established its natural occurrence. In 1952, 237Np was identified and isolated from concentrates of uranium ore from the Belgian Congo: in these minerals, the ratio of neptunium-237 to uranium is less than or equal to about 10−12 to 1. …
An important use of 237Np is as a precursor in plutonium-238 production, where it is irradiated with neutrons to form 238Pu, an alpha emitter for radioisotope thermal generators for spacecraft and military applications. 237Np will capture a neutron to form 238Np and beta decay with a half-life of just over two days to 238Pu.
Np
93
237
+
n
0
1
⟶
Np
93
238
→
2.117
d
β
−
Pu
94
238
{\displaystyle {\ce {^{237}_{93}Np + ^{1}_{0}n -> ^{238}_{93}Np ->[\beta^-][2.117 \ {\ce {d}}] ^{238}_{94}Pu}}}
238Pu also exists in sizable quantities in spent nuclear fuel but would have to be separated from other isotopes of plutonium. …
All nuclear data not otherwise stated is from the standard source:
Twenty-four neptunium radioisotopes have been characterized, with the most stable being 237Np with a half-life of 2.144 million years, 236Np with a half-life of 153,000 years, and 235Np with a half-life of 396.1 days. All of the remaining radioactive isotopes have half-lives that are less than 5 days.
Isotopes lighter than the most stable one, 237Np, decay primarily by electron capture, although some also decay by alpha emission to become protactinium. 237Np itself, being the beta-stable isobar of mass number 237, decays by alpha to 233Pa, with very rare spontaneous fission. Heavier isotopes generally decay by beta emission.
The decay of 237Np eventually yields bismuth-209 and thallium-205, unlike most other common heavy nuclei which decay into isotopes of lead. This decay chain is known as the neptunium series. This decay chain was virtually absent on Earth due to the short half-lives of all of its isotopes above bismuth-209, but is now being resurrected thanks to artificial production of neptunium (and uranium-233) on the tonne scale.
The isotopes neptunium-235, -236, and -237 are predicted to be fissile; although only neptunium-237's fissionability has been experimentally shown. Its critical mass is about 60 kg, only about 10 kg more than that of the commonly used uranium-235. …
Neptunium does not have a biological role, as it has a short half-life and occurs only in small traces naturally. Animal tests show it to be absorbed poorly (~1%) via the digestive tract. When injected, it concentrates in the bones, from which it is slowly released.
Finely divided neptunium metal presents a fire hazard because neptunium is pyrophoric; small grains will ignite spontaneously in air at room temperature.