Protactinium-231 (which is formed by the alpha decay of uranium-235 followed by beta decay of thorium-231) could possibly sustain a nuclear chain reaction; Walter Seifritz has estimated that it might in principle be used to build a nuclear weapon with a critical mass of 750±180 kg. Other authors have concluded that such chain reactions would not be possible.
Protactinium was first identified in 1913, when Kasimir Fajans and O. H. Göhring encountered the short-lived isotope 234m-Pa (half-life of about 1.17 minute), during their studies of the decay chain of 238-U. They gave the new element the name Brevium (Latin brevis, brief, short); the name was changed to Protoactinium in 1918 when two groups of scientists (Otto Hahn and Lise Meitner of Germany and Frederick Soddy and John Cranston of the UK) independently discovered 231-Pa. The name was shortened to Protactinium in 1949.
Aristid von Grosse prepared 2 mg of Pa2O5 in 1927, and in 1934 performed the first isolation of elemental protactinium from 0.1 mg of Pa2O5, by converting the oxide to an iodide and then cracking it in a high vacuum with an electrically heated filament by the reaction 2PaI5 → 2Pa + 5I2 (iodide process).
In 1961, the United Kingdom Atomic Energy Authority was able to produce 125 g of 99.9% pure protactinium, processing 60 tons of waste material in a 12-stage process and spending 500,000 USD. For many years, this was the world's only supply of the element. It is reported that the metal was sold to laboratories for a cost of 2,800 USD / g in the following years.
See also Protactinium compounds.
The primary decay mode for isotopes of Pa lighter than (and including) the most stable isotope 231-Pa (ie, 212Pa to 231Pa) is alpha decay and the primary mode for the heavier isotopes (ie, 232Pa to 240Pa) is beta minus (β−) decay. The primary decay products of isotopes of Pa lighter than (and including) 231-Pa are element Ac (actinium) isotopes and the primary decay products for the heavier isotopes of Pa are element U (uranium) isotopes.