protactinium (Pa)

Découverte et histoire

Découvert: 1917 · Kazimierz Fajans

In 1871, Dmitri Mendeleev predicted the existence of an element between thorium and uranium. The actinide series was unknown at the time, so Mendeleev positioned uranium below tungsten in group VI, and thorium below zirconium in group IV, leaving the space below tantalum in group V empty. Until the general acceptance of the actinide concept in the late 1940s, periodic tables were published with this structure. For a long time, chemists searched for eka-tantalum as an element with similar chemical properties to tantalum, making a discovery of protactinium nearly impossible. Tantalum's heavier analogue was later found to be the transuranic element dubnium – although dubnium is more chemically similar to protactinium, not tantalum. In 1900, William Crookes isolated protactinium as an intensely radioactive material from uranium; however, he could not characterize it as a new chemical element

Utilisations et applications

Protactinium is one of the rarest and most expensive naturally occurring elements. It is found in the form of two isotopes, 231Pa and 234Pa, with the isotope 234Pa occurring in two different energy states. Nearly all natural protactinium is 231Pa. It is an alpha emitter and is formed by the decay of uranium-235, whereas the beta-radiating 234Pa is produced as a result of uranium-238 decay. Nearly all uranium-238 (99.8%) decays first to the shorter-lived 234mPa isomer. Protactinium occurs in uraninite (pitchblende) at concentrations of about 0.3–3 parts 231Pa per million parts (ppm) of ore. Whereas the usual content is closer to 0.3 ppm (e.g. in Jáchymov, Czech Republic), some ores from the Democratic Republic of the Congo have about 3 ppm. Protactinium is homogeneously dispersed in most natural materials and in water, but at much lower concentrations on the order of one part per trillion

Isotopes

Thirty radioisotopes of protactinium have been discovered, ranging from 210Pa to 239Pa. The most stable are 231Pa with a half-life of 32,650 years, 233Pa with a half-life of 26.975 days, and 230Pa with a half-life of 17.4 days. All other isotopes have half-lives shorter than 1.6 days, and the majority of these have half-lives less than 1.8 seconds. Protactinium also has six nuclear isomers, with the most stable being 234mPa (half-life 1.159 minutes). The primary decay mode for the most stable isotope 231Pa and lighter isotopes (210Pa to 227Pa) is alpha decay, producing isotopes of actinium. The primary decay mode for 228Pa to 230Pa is electron capture or beta plus decay, producing isotopes of thorium, while the primary decay mode for the heavier isotopes (232Pa to 239Pa) is beta decay, producing isotopes of uranium.