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Tantalum is a chemical element with symbol Ta and atomic number 73. Previously known as tantalium, its name comes from Tantalus, an antihero from Greek mythology Tantalum is a rare, hard, blue-gray, lustrous transition metal that is highly corrosion-resistant. It is part of the refractory metals group, which are widely used as minor components in alloys. The chemical inertness of tantalum makes it a valuable substance for laboratory equipment and a substitute for platinum. Tantalum is also used for medical implants and bone repair Its main use today is in tantalum capacitors in electronic equipment such as mobile phones, DVD players, video game systems and computers. Tantalum, always together with the chemically similar niobium, occurs in the minerals tantalite, columbite and coltan (a mix of columbite and tantalite).

Tantalum is a rare metal. Its abundance in the solar system can be estimated via spectroscopic study of the sun and chemical analyses of meteorites. In the solar system abundance list used in Wikipedia[1], its molar concentration relative to silicon is reported to be either 2.1×10−8 (Ahrens) or 3.8x10-8 (Kaye & Laby). Converted to fraction of all atoms in the primordial solar mix, [Ta] = 1.3E-12 per unit. In abundance, it ranks just above uranium at the tail end of the primordial elements list. A second table[2] lists a whole-earth concentration of [Ta] = 4000E-12 (4E-09) per unit. This enhanced concentration of Ta occurs because He and Ne have essentially disappeared from the earth, and both H and C have terrestrial abundances much lower than their solar abundances. Its concentration in the crust, however is reported to be around 2 parts per million by mass (ppm). Since its atomic mass is several times earth's mean, its atomic (molar) concentration will be several times lower so [Ta] = 5.00E-09 per unit is a reasonable guess. Tantalum is somewhat concentrated in the crust, but not to the extent of U or other active metals.

Nuclear properties[]

36 isotopes of Ta have been observed, ranging from 190Ta down to 155Ta. These lie within the band of predicted isotopes, which ranges from 247Ta to 154Ta. In addition, 37 isomers have been observed, 26 of them in the band 182Ta to 176Ta and 7 of them in the band 160Ta to 156Ta. It is not clear whether this concentration results from nuclear structure or limited search for isomers outside the bands given.

181Ta is the element's only stable isotope, although 179Ta (half-life 1.82 y) comes fairly close. Between them lies 180Ta, which has an 8.15 hr half-life, decays both by electron capture to 180Hf (branch ratio = 0.86) and by electron emission to 180W (BR = 0.14), and has a metastable isomer. That isomer 180m1Ta is unique. It is a high-spin isomer whose decay to its ground state (180Ta) is so strongly inhibited that it has never been observed. Since its decay by any other mode consumes energy, it never decays. It is the one and only stable isomer.

Above 181Ta, isotopes decay by beta emission with short half-lives. Below 179Ta, all isotopes decay by positron emission except for 155Ta whose reported half-life is too short for beta decay and so is predicted to decay by proton emission. Alpha decay is an active decay mode between 163Ta and 157Ta, for which N = 84, at which point alpha decay is replaced by some proton emission in 156Ta and near-total proton emission in 155Ta and 154Ta.

181Ta accounts for 0.99988 +/- 0.00002 of all Ta atoms. 180m1Ta provides the remaining 0.00012 +/- 0.00002 atoms. While 181Ta forms via either rapid neutron capture (r-process) or infrequent neutron capture (s-process), neither will produce 180m1Ta. The most likely possible route would be photon capture / neutron emission: 181Ta + gamma --> 180m1Ta + n.

References[]

  1. https://en.wikipedia.org/wiki/Abundances_of_the_elements_(data_page)
  2. "The Composition of the Earth", W.F. McDonough, Table 3; retrieved via Wayback from Ref. 1.