Neptunium
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Neptunium
Neptunium () is a chemical element with the symbol Np and atomic number 93. A silvery radioactive metallic element, neptunium is the first transuranic element and belongs to the actinide series. Its most stable isotope, 237Np, is a by-product of nuclear reactors and plutonium production and it can be used as a component in neutron detection equipment. Neptunium is also found in trace amounts in uranium ores.
CharacteristicsSilvery in appearance, neptunium metal is fairly chemically reactive and is found in at least three allotropes:
CompoundsThis element has four ionic oxidation states while in solution:
Neptunium forms tri- and tetrahalides such as NpF3, NpF4, NpCl4, NpBr3, NpI3, and oxides of the various compositions such as are found in the uranium-oxygen system, including Np3O8 and NpO2. NpF5 is volatile like uranium hexafluoride. See fluoride volatility and uranium enrichment. Neptunium like other actinides readily forms a dioxide neptunyl core (NpO2). In the environment, this neptunyl core readily complexes with carbonate as well as other oxygen moieties (OH-, NO2-, NO3-, and SO4-2) to form charged complexes which tend to be readily mobile with low affinities to soil.
UsesPrecursor in Plutonium-238 Production237Np is irradiated with neutrons to create 238Pu, a rare and valuable isotope for spacecraft and military applications. 237Np will capture a neutron to form 238Np and beta decay with a half life of two days to 238Pu. Weapons applicationsNeptunium is fissionable, and could theoretically be used as fuel in a fast neutron reactor or a nuclear weapon. In 1992, the U.S. Department of Energy declassified the statement that Np-237 "can be used for a nuclear explosive device".[1] It is not believed that an actual weapon has ever been constructed using neptunium. In September 2002, researchers at the University of California Los Alamos National Laboratory created the first known nuclear critical mass using neptunium in combination with enriched uranium, discovering that the critical mass of neptunium is less than previously predicted[2], showing that it "is about as good a bomb material as U-235." US officials in March 2004, planned to move the nation's supply of separated neptunium to a site in Nevada. HistoryNeptunium (named for the planet Neptune, the next planet out from Uranus, after which uranium was named) was first discovered by Edwin McMillan and Philip H. Abelson in the year 1940 in Berkeley, California. Initially predicted by Walter Russell's "spiral" organization of the periodic table, it was found at the Berkeley Radiation Laboratory of the University of California, Berkeley where the team produced the neptunium isotope 239Np (2.4 day half-life) by bombarding uranium with slow moving neutrons. It was the first transuranium element produced synthetically and the first actinide series transuranium element discovered. OccurrenceTrace amounts of neptunium are found naturally as decay products from transmutation reactions in uranium ores. Artificial 237Np is produced through the reduction of 237NpF3 with barium or lithium vapor at around 1200 °C and is most often extracted from spent nuclear fuel rods as a by-product in plutonium production. By weight, neptunium-237 discharges are about five percent as great as plutonium discharges and about 0.05 percent of spent nuclear fuel discharges. [3] Nuclear synthesis
Since nearly all neptunium is produced in this way or consists of heavier isotopes which decay quickly, one gets nearly pure 237Np by chemical separation of neptunium from spent nuclear fuel. Role in nuclear wasteNeptunium-237 is the most mobile actinide in the deep geological repository environment.[4] This makes it and its predecessors such as americium-241 candidates of interest for destruction by nuclear transmutation.[5] 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 a smoke detector includes about 5% neptunium after 22 years, and about 10% after 43 years. After the 432-year americium-241 half-life, a smoke detector's original americium would be more than half neptunium. Isotopes19 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-lifes that are less than 4.5 days, and the majority of these have half lifes that are less than 50 minutes. This element also has 4 meta states, with the most stable being 236mNp (t½ 22.5 hours). The isotopes of neptunium range in atomic weight from 225.0339 u (225Np) to 244.068 u (244Np). 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 element 92 (uranium) isotopes (alpha emission produces element 91, protactinium, however) and the primary products after are element 94 (plutonium) isotopes. 237Np is fissionable[2]. 237Np eventually decays to form bismuth-209, unlike most other common heavy nuclei which decay to make isotopes of lead. This decay chain is known as the neptunium series. Neptunium in Popular Culture
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