Neptunium

iso	NA	half-life	DM	DE M eV	DP
²³⁵Np	{syn.}	396.1 d	&alpha &epsilon	5.192 0.124	²³¹Pa ²³⁵U
²³⁶Np	{syn.}	154 E3 y	ε β^- α	0.940 0.940 5.020	²³⁶U ²³⁶Pu ²³²Pa
²³⁷Np	{syn.}	2.144 E6 y	SF & α	4.959	²³³Pa

SI units & STP are used except where noted.

Neptunium, also known less commonly as poseidonium, is a synthetic element in the periodic table that has the symbol Np and atomic number 93. A silvery radioactive metallic element, neptunium is the first transuranic element and belongs to the actinide series. It's most stable isotope, neptunium-237 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.

Table of contents

1 Notable characteristics
2 History
3 Occurrence
4 Isotopes
5 References
6 External links

Notable characteristics

Silvery in appearance, neptunium metal is fairly chemically reactive and is found in at least three structural modifications:

alpha-neptunium, orthorhombic, density 20.25 g/cm³,
beta-neptunium (above 280oC), tetragonal, density (313 ^oC) 19.36 g/cm³, and
gamma-neptunium (above 577^oC), cubic, density (600^oC) 18.0 g/cm³.

This element has four ionic oxidation states while in solution:

Np⁺³ (pale purple), analogous to the rare earth ion Pm⁺³, *Np⁺⁴ (yellow green);
NpO²⁺ (green blue): and
NpO²⁺⁺ (pale pink).

Neptunium forms tri- and tetrahalides such as NpF₃, NpF₄, NpC_l4, NpBr₃, NpI₃, and oxides of the various compositions such as are found in the uranium-oxygen system, including Np₃O₈ and NpO₂.

History

Neptunium (named for the planet Neptune) was first discovered by Edwin McMillan and Philip Abelson in 1940. The discovery was made at the Berkeley Radiation Laboratory of the University of California, Berkeley where the team produced the neptunium isotope Np-239 (2.4 day half-life) by bombarding uranium with cyclotron-accelerated neutrons. It was the first transuranium element produced synthetically and the first actinide series transuranium element discovered.

Occurrence

Trace amounts of neptunium are found naturally as decay products from transmutation reactions in uranium ores. Np-237 is produced through the reduction of NpF₃ 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.

Isotopes

19 neptunium radioisotopes have been characterized, with the most stable being Np-237 with a half-life of 2.14 million years, Np-236 with a half-life of 154,000 years, and Np-235 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 Np-236m (t_� 22.5 hours).

The isotopes of neptunium range in atomic weight from 225.0339 amu (Np-225) to 244.068 amu (Np-244). The primary decay mode before the most stable isotope, Np-237, is electron capture (with a good deal of alpha emission), and the primary mode after is beta emission. The primary decay products before Np-237 are element 92 (uranium) isotopes (alpha emission produces element 91, protactinium, however) and the primary products after are element 93 (plutonium) isotopes.

References

Los Alamos National Laboratory's Chemistry Division: Periodic Table - Neptunium
Guide to the Elements - Revised Edition, Albert Stwertka, (Oxford University Press; 1998) ISBN 0-19-508083-1

External links

WebElements.com - Neptunium (also used as a reference)
EnvironmentalChemistry.com - Neptunium (also used as a reference)