Neptunium

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. This isotope, and the isotope neptunium-239, are also found in trace amounts in uranium ores due to neutron capture reactions and beta decay.

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Characteristics

Physical

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 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. 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.

{| class="wikitable" style="margin:auto; text-align:center;"

|+ Allotropes of neptunium

|-

!Allotrope

!α (measured at 20 °C)

!β (measured at 313 °C)

!γ (measured at 600 °C)

|-

!Transition temperature Each neptunium atom is coordinated to four others and the Np–Np bond lengths are 260 pm. It is the densest of all the actinides and the fifth-densest of all naturally occurring elements, behind only rhenium, platinum, iridium, and osmium. α-neptunium has semimetallic properties, such as strong covalent bonding and a high electrical resistivity, and its metallic physical properties are closer to those of the metalloids than the true metals. Some allotropes of the other actinides also exhibit similar behaviour, though to a lesser degree. The densities of different isotopes of neptunium in the alpha phase are expected to be observably different: α-²³⁵Np should have density 20.303 g/cm³; α-²³⁶Np, density 20.389 g/cm³; α-²³⁷Np, density 20.476 g/cm³.

β-neptunium takes on a distorted tetragonal close-packed structure. Four atoms of neptunium make up a unit cell, and the Np–Np bond lengths are 276 pm.

Alloys

Due to the presence of valence 5f electrons, neptunium and its alloys exhibit a very interesting magnetic behavior, like many other actinides. These can range from the itinerant band-like character characteristic of the transition metals to the local moment behavior typical of scandium, yttrium, and the lanthanides. This stems from 5f-orbital hybridization with the orbitals of the metal ligands, and the fact that the 5f orbital is relativistically destabilized and extends outwards. For example, pure neptunium is paramagnetic, NpAl₃ is ferromagnetic, NpGe₃ has no magnetic ordering, and NpSn₃ may be a heavy fermion material.

Chemical

Neptunium has five ionic oxidation states ranging from +3 to +7 when forming chemical compounds, which can be simultaneously observed in solutions. It is the heaviest actinide that can lose all its valence electrons in a stable compound. The most stable state in solution is +5, but the valence +4 is preferred in solid neptunium compounds. Neptunium metal is very reactive. Ions of neptunium are prone to hydrolysis and formation of coordination compounds.

Atomic

A neptunium atom has 93 electrons, arranged in the configuration <nowiki>[</nowiki>Rn<nowiki>]</nowiki>&nbsp;5f⁴&nbsp;6d¹&nbsp;7s². This differs from the configuration expected by the Aufbau principle in that one electron is in the 6d subshell instead of being as expected in the 5f subshell. This is because of the similarity of the electron energies of the 5f, 6d, and 7s subshells. In forming compounds and ions, all the valence electrons may be lost, leaving behind an inert core of inner electrons with the electron configuration of the noble gas radon; more commonly, only some of the valence electrons will be lost. The electron configuration for the tripositive ion Np³⁺ is [Rn]&nbsp;5f⁴, with the outermost 7s and 6d electrons lost first: this is exactly analogous to neptunium's lanthanide homolog promethium, and conforms to the trend set by the other actinides with their [Rn]&nbsp;5fⁿ electron configurations in the tripositive state. The first ionization potential of neptunium was measured to be at most in 1974, based on the assumption that the 7s electrons would ionize before 5f and 6d; more recent measurements have refined this to 6.2657&nbsp;eV.

Isotopes

thumb|The 4n + 1 [[decay chain of neptunium-237, commonly called the "neptunium series"]]

: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.

thumb|This nickel-clad neptunium sphere was used to experimentally determine the critical mass of Np at Los Alamos National Lab.

The isotopes neptunium-235, -236, and -237 are predicted to be fissile; Calculated values of the critical masses of neptunium-235, -236, and -237 respectively are 66.2&nbsp;kg, 6.79&nbsp;kg, and 63.6&nbsp;kg: the neptunium-236 value is even lower than that of plutonium-239 and ²³⁶Np also has a low neutron cross section.

Occurrence

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. 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. Additionally, ²⁴⁰Np must also occur as an intermediate decay product of ²⁴⁴Pu, which has been detected in meteorite dust in marine sediments on Earth.

Most neptunium (and plutonium) now encountered in the environment is due to atmospheric nuclear explosions that took place between the detonation of the first atomic bomb in 1945 and the ratification of the Partial Nuclear Test Ban Treaty in 1963. The total amount of neptunium released by these explosions and the few atmospheric tests that have been carried out since 1963 is estimated to be around 2500&nbsp;kg. The overwhelming majority of this is composed of the long-lived isotopes ²³⁶Np and ²³⁷Np since even the moderately long-lived ²³⁵Np (half-life 396&nbsp;days) would have decayed to less than one-billionth (10⁻⁹) its original concentration over the intervening decades. An additional very small amount of neptunium, produced by neutron irradiation of natural uranium in nuclear reactor cooling water, is released when the water is discharged into rivers or lakes. The concentration of ²³⁷Np in seawater is approximately 6.5&nbsp;×&nbsp;10⁻⁵&nbsp;millibecquerels per liter: this concentration is between 0.1% and 1% that of plutonium. Np(V) is also readily absorbed by concrete, which because of the element's radioactivity is a consideration that must be addressed when building nuclear waste storage facilities. When absorbed in concrete, it is reduced to Np(IV) in a relatively short period of time. Np(V) is also reduced by humic acids if they are present on the surface of goethite, hematite, and magnetite. Np(IV) is less mobile and efficiently adsorbed by tuff, granodiorite, and bentonite; although uptake by the latter is most pronounced in mildly acidic conditions. It also exhibits a strong tendency to bind to colloidal particulates, an effect that is enhanced when in surface soil with high clay content. The behavior provides an additional aid in the element's observed high mobility.

History

Background and early claims

thumb|right|alt=a table with a typical cell containing a two-letter symbol and a number|[[Dmitri Mendeleev's table of 1871, with an empty space at the position after uranium]]

When the first periodic table of the elements was published by Dmitri Mendeleev in the early 1870s, it showed a "&nbsp;—&nbsp;" 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.

After several months of work, Fermi's group had tentatively determined that lighter elements would disperse the energy of the captured neutron by emitting a proton or alpha particle and heavier elements would generally accomplish the same by emitting a gamma ray. This latter behavior would later result in the beta decay of a neutron into a proton, thus moving the resulting isotope one place up the periodic table. When Fermi's team bombarded uranium, they observed this behavior as well, which strongly suggested that the resulting isotope had an atomic number of 93. Fermi was initially reluctant to publicize such a claim, but after his team observed several unknown half-lives in the uranium bombardment products that did not match those of any known isotope, he published a paper entitled Possible Production of Elements of Atomic Number Higher than 92 in June 1934. For element 93, he proposed the name ausenium (atomic symbol Ao) after the Greek name Ausonia for Italy.

Several theoretical objections to the claims of Fermi's paper were quickly raised; in particular, the exact process that took place when an atom captured a neutron was not well understood at the time. This and Fermi's accidental discovery three months later that nuclear reactions could be induced by slow neutrons cast further doubt in the minds of many scientists, notably Aristid von Grosse and Ida Noddack, that the experiment was creating element 93. While von Grosse's claim that Fermi was actually producing protactinium (element 91) was quickly tested and disproved, Noddack's proposal that the uranium had been shattered into two or more much smaller fragments was simply ignored by most because existing nuclear theory did not include a way for this to be possible. Fermi and his team maintained that they were in fact synthesizing a new element, but the issue remained unresolved for several years.

Although the many different and unknown radioactive half-lives in the experiment's results showed that several nuclear reactions were occurring, Fermi's group could not prove that element 93 was being produced unless they could isolate it chemically. They and many other scientists attempted to accomplish this, including Otto Hahn and Lise Meitner who were among the best radiochemists in the world at the time and supporters of Fermi's claim, but they all failed. Much later, it was determined that the main reason for this failure was because the predictions of element 93's chemical properties were based on a periodic table which lacked the actinide series. This arrangement placed protactinium below tantalum, uranium below tungsten, and further suggested that element 93, at that point referred to as eka-rhenium, should be similar to the group 7 elements, including manganese and rhenium. Thorium, protactinium, and uranium, with their dominant oxidation states of +4, +5, and +6 respectively, fooled scientists into thinking they belonged below hafnium, tantalum, and tungsten, rather than below the lanthanide series, which was at the time viewed as a fluke, and whose members all have dominant +3 states; neptunium, on the other hand, has a much rarer, more unstable +7 state, with +4 and +5 being the most stable. Upon finding that plutonium and the other transuranic elements also have dominant +3 and +4 states, along with the discovery of the f-block, the actinide series was firmly established.

While the question of whether Fermi's experiment had produced element 93 was stalemated, two additional claims of the discovery of the element appeared, although unlike Fermi, they both claimed to have observed it in nature. The first of these claims was by Czech engineer Odolen Koblic in 1934 when he extracted a small amount of material from the wash water of heated pitchblende. He proposed the name bohemium for the element, but after being analyzed it turned out that the sample was a mixture of tungsten and vanadium. The other claim, in 1938 by Romanian physicist Horia Hulubei and French chemist Yvette Cauchois, claimed to have discovered the new element via spectroscopy in minerals. They named their element sequanium, but the claim was discounted because the prevailing theory at the time was that if it existed at all, element 93 would not exist naturally. However, as neptunium does in fact occur in nature in trace amounts, as demonstrated when it was found in uranium ore in 1952, it is possible that Hulubei and Cauchois did in fact observe neptunium.

Although by 1938 some scientists, including Niels Bohr, were still reluctant to accept that Fermi had actually produced a new element, he was nevertheless awarded the Nobel Prize in Physics in November 1938 "for his demonstrations of the existence of new radioactive elements produced by neutron irradiation, and for his related discovery of nuclear reactions brought about by slow neutrons". A month later, the almost totally unexpected discovery of nuclear fission by Hahn, Meitner, and Otto Frisch put an end to the possibility that Fermi had discovered element 93 because most of the unknown half-lives that had been observed by Fermi's team were rapidly identified as those of fission products.

Perhaps the closest of all attempts to produce the missing element 93 was that conducted by the Japanese physicist Yoshio Nishina working with chemist Kenjiro Kimura in 1940, just before the outbreak of the Pacific War in 1941: they bombarded ²³⁸U with fast neutrons. However, while slow neutrons tend to induce neutron capture through a (n, γ) reaction, fast neutrons tend to induce a "knock-out" (n, 2n) reaction, where one neutron is added and two more are removed, resulting in the net loss of a neutron. Nishina and Kimura, having tested this technique on ²³²Th and successfully produced the known ²³¹Th and its long-lived beta decay daughter ²³¹Pa (both occurring in the natural decay chain of ²³⁵U), therefore correctly assigned the new 6.75-day half-life activity they observed to the new isotope ²³⁷U. They confirmed that this isotope was also a beta emitter and must hence decay to the unknown nuclide ²³⁷Np. They attempted to isolate this nuclide by carrying it with its supposed lighter congener rhenium, but no beta or alpha decay was observed from the rhenium-containing fraction: Nishina and Kimura thus correctly speculated that the half-life of ²³⁷Np, like that of ²³¹Pa, was very long and hence its activity would be so weak as to be unmeasurable by their equipment, thus concluding the last and closest unsuccessful search for transuranic elements.

Discovery

thumb|The 60-inch cyclotron at the Lawrence Radiation Laboratory, University of California, Berkeley, in August 1939|alt=Black-and-white picture of heavy machinery with two operators sitting aside.

As research on nuclear fission progressed in early 1939, Edwin McMillan at the Berkeley Radiation Laboratory of the University of California, Berkeley decided to run an experiment bombarding uranium using the powerful 60-inch (1.52 m) cyclotron that had recently been built at the university. The purpose was to separate the various fission products produced by the bombardment by exploiting the enormous force that the fragments gain from their mutual electrical repulsion after fissioning. Although he did not discover anything of note from this, McMillan did observe two new beta decay half-lives in the uranium trioxide target itself, which meant that whatever was producing the radioactivity had not violently repelled each other like normal fission products. He quickly realized that one of the half-lives closely matched the known 23-minute decay period of uranium-239, but the other half-life of 2.3 days was unknown. McMillan took the results of his experiment to chemist and fellow Berkeley professor Emilio Segrè to attempt to isolate the source of the radioactivity. Both scientists began their work using the prevailing theory that element 93 would have similar chemistry to rhenium, but Segrè rapidly determined that McMillan's sample was not at all similar to rhenium. Instead, when he reacted it with hydrogen fluoride (HF) with a strong oxidizing agent present, it behaved much like members of the rare earths. Since these elements comprise a large percentage of fission products, Segrè and McMillan decided that the half-life must have been simply another fission product, titling the paper "An Unsuccessful Search for Transuranium Elements".

However, as more information about fission became available, the possibility that the fragments of nuclear fission could still have been present in the target became more remote. McMillan and several scientists, including Philip H. Abelson, attempted again to determine what was producing the unknown half-life. In early 1940, McMillan realized that his 1939 experiment with Segrè had failed to test the chemical reactions of the radioactive source with sufficient rigor. In a new experiment, McMillan tried subjecting the unknown substance to HF in the presence of a reducing agent, something he had not done before. This reaction resulted in the sample precipitating with the HF, an action that definitively ruled out the possibility that the unknown substance was a rare-earth metal.

Shortly after this, Abelson, who had received his graduate degree from the university, visited Berkeley for a short vacation and McMillan asked the more able chemist to assist with the separation of the experiment's results. Abelson very quickly observed that whatever was producing the 2.3-day half-life did not have chemistry like any known element and was actually more similar to uranium than a rare-earth metal. This discovery finally allowed the source to be isolated and later, in 1945, led to the classification of the actinide series. As a final step, McMillan and Abelson prepared a much larger sample of bombarded uranium that had a prominent 23-minute half-life from ²³⁹U and demonstrated conclusively that the unknown 2.3-day half-life increased in strength in concert with a decrease in the 23-minute activity through the following reaction: They did not propose a name for the element in the paper, but they soon decided on the name neptunium since Neptune is the next planet beyond Uranus in the Solar System, which uranium is named after. McMillan and Abelson's success compared to Nishina and Kimura's near miss can be attributed to the favorable half-life of ²³⁹Np for radiochemical analysis and quick decay of ²³⁹U, in contrast to the slower decay of ²³⁷U and extremely long half-life of ²³⁷Np. The discovery of plutonium had to wait until the end of 1940, when Glenn T. Seaborg and his team identified the isotope plutonium-238.

In 1942, Hahn and Fritz Strassmann, and independently Kurt Starke, reported the confirmation of element 93 in Berlin. Hahn's group did not pursue element 94, likely because they were discouraged by McMillan and Abelson's lack of success in isolating it. Since they had access to the stronger cyclotron at Paris at this point, Hahn's group would likely have been able to detect element 94 had they tried, albeit in tiny quantities (a few becquerels).

Much of the research into the properties of neptunium since then has been focused on understanding how to confine it as a portion of nuclear waste. Because it has isotopes with very long half-lives, it is of particular concern in the context of designing confinement facilities that can last for thousands of years. It has found some limited uses as a radioactive tracer and a precursor for various nuclear reactions to produce useful plutonium isotopes. However, most of the neptunium that is produced as a reaction byproduct in nuclear power stations is considered to be a waste product.

• When an ²³⁵U atom captures a neutron, it is converted to an excited state of ²³⁶U. About 85.5% of the excited ²³⁶U nuclei undergo fission, but the remainder decay to the ground state of ²³⁶U by emitting gamma radiation. Further neutron capture forms ²³⁷U which has a half-life of 7 days and quickly decays to ²³⁷Np through beta decay. During beta decay, the excited ²³⁷U emits an electron, while the atomic weak interaction converts a neutron to a proton, thus creating ²³⁷Np. However, even this fraction still amounts to more than fifty tons per year globally.

Purification methods

Recovering uranium and plutonium from spent nuclear fuel for reuse is one of the major processes of the nuclear fuel cycle. As it has a long half-life of just over 2&nbsp;million years, the alpha emitter ²³⁷Np is one of the major isotopes of the minor actinides separated from spent nuclear fuel. Many separation methods have been used to separate out the neptunium, operating on small and large scales. The small-scale purification operations have the goals of preparing pure neptunium as a precursor of metallic neptunium and its compounds, and also to isolate and preconcentrate neptunium in samples for analysis. Currently, commercial reprocessing plants use the Purex process, involving the solvent extraction of uranium and plutonium with tributyl phosphate.

Chemistry and compounds

Solution chemistry

thumb|upright=1.6|right|Neptunium ions in solution

When it is in an aqueous solution, neptunium can exist in any of its five possible oxidation states (+3 to +7) and each of these show a characteristic color.

{| class="wikitable" style="float:right; clear:right; margin-left:1em; margin-top:0;"

|-

! Oxidation <br />state !! Representative compound

|-

| +2 || [K(2.2.2-crypt)][NpCp'₃]

|-

| +3 || Neptunium(III) chloride, NpCl₃

|-

| +4 || Neptunium(IV) oxide, NpO₂

|-

| +5 || Neptunium(V) fluoride, NpF₅

|-

| +6 || Neptunium(VI) fluoride, NpF₆

|-

| +7 || Neptunium(VII) oxide-hydroxide, NpO₂(OH)₃

|}

In acidic solutions, the neptunium(III) to neptunium(VII) ions exist as Np³⁺, Np⁴⁺, , , and . In basic solutions, they exist as the oxides and hydroxides Np(OH)₃, NpO₂, NpO₂OH, NpO₂(OH)₂, and . Not as much work has been done to characterize neptunium in basic solutions.

; Neptunium(III) :

Np(III) or Np³⁺ exists as hydrated complexes in acidic solutions, . In the presence of oxygen, it is quickly oxidized to Np(IV) unless strong reducing agents are also present. Nevertheless, it is the second-least easily hydrolyzed neptunium ion in water, forming the NpOH²⁺ ion.

; Neptunium(IV) :

thumb|Np(IV) in 8 M HClNp(IV) or Np⁴⁺ is pale yellow-green in acidic solutions,

Because the Np(V) ion is very stable, it can only form a hydroxide in high acidity levels. When placed in a 0.1&nbsp;M sodium perchlorate solution, it does not react significantly for a period of months, although a higher molar concentration of 3.0&nbsp;M will result in it reacting to the solid hydroxide NpO₂OH almost immediately. Np(VI) hydroxide is more reactive but it is still fairly stable in acidic solutions. It will form the compound NpO₃·H₂O in the presence of ozone under various carbon dioxide pressures. Np(VII) has not been well-studied and no neutral hydroxides have been reported. It probably exists mostly as .

Oxides

Three anhydrous neptunium oxides have been reported, NpO₂, Np₂O₅, and Np₃O₈, though some studies have stated that only the first two of these exist, suggesting that claims of Np₃O₈ are actually the result of mistaken analysis of Np₂O₅. However, as the full extent of the reactions that occur between neptunium and oxygen has yet to be researched, it is not certain which of these claims is accurate. Although neptunium oxides have not been produced with neptunium in oxidation states as high as those possible with the adjacent actinide uranium, neptunium oxides are more stable at lower oxidation states. This behavior is illustrated by the fact that NpO₂ can be produced by simply burning neptunium salts of oxyacids in air.

The greenish-brown NpO₂ is very stable over a large range of pressures and temperatures and does not undergo phase transitions at low temperatures. It does show a phase transition from face-centered cubic to orthorhombic at around 33–37&nbsp;GPa, although it returns to its original phase when pressure is released. It remains stable under oxygen pressures up to 2.84&nbsp;MPa and temperatures up to 400&nbsp;°C.

Np₂O₅ is black-brown in color and monoclinic with a lattice size of 418×658×409&nbsp;picometres. It is relatively unstable and decomposes to NpO₂ and O₂ at 420–695&nbsp;°C. Although Np₂O₅ was initially subject to several studies that claimed to produce it with mutually contradictory methods, it was eventually prepared successfully by heating neptunium peroxide to 300–350&nbsp;°C for 2–3 hours or by heating it under a layer of water in an ampoule at 180&nbsp;°C.

Neptunium also forms a large number of oxide compounds with a wide variety of elements, although the neptunate oxides formed with alkali metals and alkaline earth metals have been by far the most studied. Ternary neptunium oxides are generally formed by reacting NpO₂ with the oxide of another element or by precipitating from an alkaline solution. Li₅NpO₆ has been prepared by reacting Li₂O and NpO₂ at 400&nbsp;°C for 16 hours or by reacting Li₂O₂ with NpO₃·H₂O at 400&nbsp;°C for 16 hours in a quartz tube and flowing oxygen. Alkali neptunate compounds K₃NpO₅, Cs₃NpO₅, and Rb₃NpO₅ are all produced by a similar reaction:

: NpO₂ + 3 MO₂ → M₃NpO₅&nbsp;(M = K, Cs, Rb)

The oxide compounds KNpO₄, CsNpO₄, and RbNpO₄ are formed by reacting Np(VII) () with a compound of the alkali metal nitrate and ozone. Additional compounds have been produced by reacting NpO₃ and water with solid alkali and alkaline peroxides at temperatures of 400–600&nbsp;°C for 15–30 hours. Some of these include Ba₃(NpO₅)₂, Ba₂NaNpO₆, and Ba₂LiNpO₆. Also, a considerable number of hexavalent neptunium oxides are formed by reacting solid-state NpO₂ with various alkali or alkaline earth oxides in an environment of flowing oxygen. Many of the resulting compounds also have an equivalent compound that substitutes uranium for neptunium. Some compounds that have been characterized include Na₂Np₂O₇, Na₄NpO₅, Na₆NpO₆, and Na₂NpO₄. These can be obtained by heating different combinations of NpO₂ and Na₂O to various temperature thresholds and further heating will also cause these compounds to exhibit different neptunium allotropes. The lithium neptunate oxides Li₆NpO₆ and Li₄NpO₅ can be obtained with similar reactions of NpO₂ and Li₂O.

A large number of additional alkali and alkaline neptunium oxide compounds such as Cs₄Np₅O₁₇ and Cs₂Np₃O₁₀ have been characterized with various production methods. Neptunium has also been observed to form ternary oxides with many additional elements in groups 3 through 7, although these compounds are much less well studied.

Halides

Although neptunium halide compounds have not been nearly as well studied as its oxides, a fairly large number have been successfully characterized. Of these, neptunium fluorides have been the most extensively researched, largely because of their potential use in separating the element from nuclear waste products. Four binary neptunium fluoride compounds, NpF₃, NpF₄, NpF₅, and NpF₆, have been reported. The first two are fairly stable and were first prepared in 1947 through the following reactions:

:2 NpO₂ + H₂ + 6 HF → 2 NpF₃ + 4 H₂O&nbsp;&nbsp;&nbsp;(400°C)

:2 NpF₃ + O₂ + 2 HF → 2 NpF₄ + H₂O&nbsp;&nbsp;(400°C)

Later, NpF₄ was obtained directly by heating NpO₂ to various temperatures in mixtures of either hydrogen fluoride or pure fluorine gas. NpF₅ is much more difficult to form and most known preparation methods involve reacting NpF₄ or NpF₆ compounds with various other fluoride compounds. NpF₅ will decompose into NpF₄ and NpF₆ when heated to around 320&nbsp;°C.

NpF₆ or neptunium hexafluoride is extremely volatile, as are its adjacent actinide compounds uranium hexafluoride (UF₆) and plutonium hexafluoride (PuF₆). This volatility has attracted a large amount of interest to the compound in an attempt to devise a simple method for extracting neptunium from spent nuclear power station fuel rods. NpF₆ was first prepared in 1943 by reacting NpF₃ and gaseous fluorine at very high temperatures and the first bulk quantities were obtained in 1958 by heating NpF₄ and dripping pure fluorine on it in a specially prepared apparatus. Additional methods that have successfully produced neptunium hexafluoride include reacting BrF₃ and BrF₅ with NpF₄ and by reacting several different neptunium oxide and fluoride compounds with anhydrous hydrogen fluorides.

Four neptunium oxyfluoride compounds, NpO₂F, NpOF₃, NpO₂F₂, and NpOF₄, have been reported, although none of them have been extensively studied. NpO₂F₂ is a pinkish solid and can be prepared by reacting NpO₃·H₂O and Np₂F₅ with pure fluorine at around 330&nbsp;°C. NpOF₃ and NpOF₄ can be produced by reacting neptunium oxides with anhydrous hydrogen fluoride at various temperatures. Neptunium also forms a wide variety of fluoride compounds with various elements. Some of these that have been characterized include CsNpF₆, Rb₂NpF₇, Na₃NpF₈, and K₃NpO₂F₅.

Two neptunium chlorides, NpCl₃ and NpCl₄, have been characterized. Although several attempts to obtain NpCl₅ have been made, they have not been successful. NpCl₃ is produced by reducing neptunium dioxide with hydrogen and carbon tetrachloride (CCl₄) and NpCl₄ by reacting a neptunium oxide with CCl₄ at around 500&nbsp;°C. Other neptunium chloride compounds have also been reported, including NpOCl₂, Cs₂NpCl₆, Cs₃NpO₂Cl₄, and Cs₂NaNpCl₆. Neptunium bromides NpBr₃ and NpBr₄ have also been produced; the latter by reacting aluminium bromide with NpO₂ at 350&nbsp;°C and the former in an almost identical procedure but with zinc present. The neptunium iodide NpI₃ has also been prepared by the same method as NpBr₃.

Chalcogenides, pnictides, and carbides

Neptunium chalcogen and pnictogen compounds have been well studied primarily as part of research into their electronic and magnetic properties and their interactions in the natural environment. Pnictide and carbide compounds have also attracted interest because of their presence in the fuel of several advanced nuclear reactor designs, although the latter group has not had nearly as much research as the former.

; Chalcogenides :

A wide variety of neptunium sulfide compounds have been characterized, including the pure sulfide compounds NpS, NpS₃, Np₂S₅, Np₃S₅, Np₂S₃, and Np₃S₄. Of these, Np₂S₃, prepared by reacting NpO₂ with hydrogen sulfide and carbon disulfide at around 1000&nbsp;°C, is the most well-studied and three allotropic forms are known. The α form exists up to around 1230&nbsp;°C, the β up to 1530&nbsp;°C, and the γ form, which can also exist as Np₃S₄, at higher temperatures. NpS can be produced by reacting Np₂S₃ and neptunium metal at 1600&nbsp;°C and Np₃S₅ can be prepared by the decomposition of Np₂S₃ at 500&nbsp;°C or by reacting sulfur and neptunium hydride at 650&nbsp;°C. Np₂S₅ is made by heating a mixture of Np₃S₅ and pure sulfur to 500&nbsp;°C. All of the neptunium sulfides except for the β and γ forms of Np₂S₃ are isostructural with the equivalent uranium sulfide and several, including NpS, α−Np₂S₃, and β−Np₂S₃ are also isostructural with the equivalent plutonium sulfide. The oxysulfides NpOS, Np₄O₄S₃, and Np₂O₂S have also been produced, although the latter two have not been well studied. NpOS was first prepared in 1985 by vacuum sealing NpO₂, Np₃S₅, and pure sulfur in a quartz tube and heating it to 900&nbsp;°C for one week.

Neptunium selenide compounds that have been reported include NpSe, NpSe₃, Np₂Se₃, Np₂Se₅, Np₃Se₄, and Np₃Se₅. All of these have only been obtained by heating neptunium hydride and selenium metal to various temperatures in a vacuum for an extended period of time and Np₂Se₃ is only known to exist in the γ allotrope at relatively high temperatures. Two neptunium oxyselenide compounds are known, NpOSe and Np₂O₂Se, are formed with similar methods by replacing the neptunium hydride with neptunium dioxide. The known neptunium telluride compounds NpTe, NpTe₃, Np₃Te₄, Np₂Te₃, and Np₂O₂Te are formed by similar procedures to the selenides and Np₂O₂Te is isostructural to the equivalent uranium and plutonium compounds. No neptunium−polonium compounds have been reported.

; Pnictides and carbides :

Neptunium nitride (NpN) was first prepared in 1953 by reacting neptunium hydride and ammonia gas at around 750&nbsp;°C in a quartz capillary tube. Later, it was produced by reacting different mixtures of nitrogen and hydrogen with neptunium metal at various temperatures. It has also been produced by the reduction of neptunium dioxide with diatomic nitrogen gas at 1550&nbsp;°C. NpN is isomorphous with uranium mononitride (UN) and plutonium mononitride (PuN) and has a melting point of 2830&nbsp;°C under a nitrogen pressure of around 1 MPa. Two neptunium phosphide compounds have been reported, NpP and Np₃P₄. The first has a face centered cubic structure and is prepared by converting neptunium metal to a powder and then reacting it with phosphine gas at 350&nbsp;°C. Np₃P₄ can be produced by reacting neptunium metal with red phosphorus at 740&nbsp;°C in a vacuum and then allowing any extra phosphorus to sublimate away. The compound is non-reactive with water but will react with nitric acid to produce Np(IV) solution.

Three neptunium arsenide compounds have been prepared, NpAs, NpAs₂, and Np₃As₄. The first two were first produced by heating arsenic and neptunium hydride in a vacuum-sealed tube for about a week. Later, NpAs was also made by confining neptunium metal and arsenic in a vacuum tube, separating them with a quartz membrane, and heating them to just below neptunium's melting point of 639&nbsp;°C, which is slightly higher than the arsenic's sublimation point of 615&nbsp;°C. Np₃As₄ is prepared by a similar procedure using iodine as a transporting agent. NpAs₂ crystals are brownish gold and Np₃As₄ is black. The neptunium antimonide compound NpSb was produced in 1971 by placing equal quantities of both elements in a vacuum tube, heating them to the melting point of antimony, and then heating it further to 1000&nbsp;°C for sixteen days. This procedure also produced trace amounts of an additional antimonide compound Np₃Sb₄. One neptunium-bismuth compound, NpBi, has also been reported.

The neptunium carbides NpC, Np₂C₃, and NpC₂ (tentative) have been reported, but have not characterized in detail despite the high importance and utility of actinide carbides as advanced nuclear reactor fuel. NpC is a non-stoichiometric compound, and could be better labelled as NpC_x (0.82 ≤ x ≤ 0.96). It may be obtained from the reaction of neptunium hydride with graphite at 1400&nbsp;°C or by heating the constituent elements together in an electric arc furnace using a tungsten electrode. It reacts with excess carbon to form pure Np₂C₃. NpC₂ is formed from heating NpO₂ in a graphite crucible at 2660–2800&nbsp;°C.

Other inorganic

; Hydrides :

Neptunium reacts with hydrogen in a similar manner to its neighbor plutonium, forming the hydrides NpH_2+x (face-centered cubic) and NpH₃ (hexagonal). These are isostructural with the corresponding plutonium hydrides, although unlike PuH_2+x, the lattice parameters of NpH_2+x become greater as the hydrogen content (x) increases. The hydrides require extreme care in handling as they decompose in a vacuum at 300&nbsp;°C to form finely divided neptunium metal, which is pyrophoric.

; Phosphates, sulfates, and carbonates :

Being chemically stable, neptunium phosphates have been investigated for potential use in immobilizing nuclear waste. Neptunium pyrophosphate (α-NpP₂O₇), a green solid, has been produced in the reaction between neptunium dioxide and boron phosphate at 1100&nbsp;°C, though neptunium(IV) phosphate has so far remained elusive. The series of compounds NpM₂(PO₄)₃, where M is an alkali metal (Li, Na, K, Rb, or Cs), are all known. Some neptunium sulfates have been characterized, both aqueous and solid and at various oxidation states of neptunium (IV through VI have been observed). Additionally, neptunium carbonates have been investigated to achieve a better understanding of the behavior of neptunium in geological repositories and the environment, where it may come into contact with carbonate and bicarbonate aqueous solutions and form soluble complexes.

Organometallic

thumb|upright=1.2|Structure of neptunocene

A few organoneptunium compounds are known and chemically characterized, although not as many as for uranium due to neptunium's scarcity and radioactivity. The most well known organoneptunium compounds are the cyclopentadienyl and cyclooctatetraenyl compounds and their derivatives. The trivalent cyclopentadienyl compound Np(C₅H₅)₃·THF was obtained in 1972 from reacting Np(C₅H₅)₃Cl with sodium, although the simpler Np(C₅H₅) could not be obtained.

Solid state

Few neptunium(III) coordination compounds are known, because Np(III) is readily oxidized by atmospheric oxygen while in aqueous solution. However, sodium formaldehyde sulfoxylate can reduce Np(IV) to Np(III), stabilizing the lower oxidation state and forming various sparingly soluble Np(III) coordination complexes, such as ·11H₂O, ·H₂O, and . For the former, NpX²⁺ and (X = Cl, Br) were obtained in 1966 in concentrated LiCl and LiBr solutions, respectively: for the latter, 1970 experiments discovered that the ion could form sulfate complexes in acidic solutions, such as and ; these were found to have higher stability constants than the neptunyl ion ().

: <chem>^{237}_{93}Np + ^{1}_{0}n -> ^{238}_{93}Np ->[\beta^-][2.117 \ \ce{d}] ^{238}_{94}Pu</chem>

²³⁸Pu also exists in sizable quantities in spent nuclear fuel but would have to be separated from other isotopes of plutonium. Irradiating neptunium-237 with electron beams, provoking bremsstrahlung, also produces quite pure samples of the isotope plutonium-236, useful as a tracer to determine plutonium concentration in the environment. It is not believed that an actual weapon has ever been constructed using neptunium. As of 2009, the world production of neptunium-237 by commercial power reactors was over 1000 critical masses a year, but to extract the isotope from irradiated fuel elements would be a major industrial undertaking. showing that it "is about as good a bomb material as [uranium-235]".

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Role in nuclear waste

Neptunium accumulates in commercial household ionization-chamber smoke detectors from decay of the (typically) 0.2 microgram of americium-241 initially present as a source of ionizing radiation. With a half-life of 432 years, the americium-241 in an ionization smoke detector includes about 3% neptunium after 20 years, and about 15% after 100 years.

Under oxidizing conditions, neptunium-237 is the most mobile actinide in the deep geological repository environment of the Yucca Mountain project in Nevada. This makes it and its predecessors such as americium-241 candidates of interest for destruction by nuclear transmutation. Due to its long half-life, neptunium will become the major contributor of the total radiotoxicity at Yucca Mountain in 10,000 years. As it is unclear what happens to the non-reprocessed spent fuel containment in that long time span, an extraction and transmutation of neptunium after spent fuel reprocessing could help to minimize the contamination of the environment if the nuclear waste could be mobilized after several thousand years.<!---->

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Biological role and precautions

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.