In 1841, Mosander extracted the rare earth didymium from lanthana. In 1874, Per Teodor Cleve concluded that didymium was in fact two elements, and in 1879, Lecoq de Boisbaudran isolated a new earth, samarium, from didymium obtained from the mineral samarskite. In 1885, the Austrian chemist baron Carl Auer von Welsbach separated didymium into two elements, praseodymium and neodymium, which gave salts of different colors.
Leo Moser (son of Ludwig Moser, founder of the Moser Glassworks in what is now Karlovy Vary, Bohemia, in the Czech Republic, not to be confused with Leo Moser, a mathematician) investigated the use of praseodymium in glass coloration in the late 1920s. The result was a yellow-green glass given the name "Prasemit". However, a similar color could be achieved with colorants costing only a minute fraction of what praseodymium cost in the late 1920s, such that the color was not popular, few pieces were made, and examples are now extremely rare. Moser also blended praseodymium with neodymium to produce "Heliolite" glass ("Heliolit" in German), which was more widely accepted. The first enduring commercial use of praseodymium, which continues today, is in the form of a yellow-orange stain for ceramics, "Praseodymium Yellow", which is a solid-solution of praseodymium in the zirconium silicate (zircon) lattice. This stain has no hint of green in it. By contrast, at sufficiently high loadings, praseodymium glass is distinctly green, rather than pure yellow.
Using classical separation methods, praseodymium was always difficult to purify. Much less abundant than the lanthanum and neodymium from which it was being separated (cerium having long since been removed by redox chemistry), praseodymium ended up being dispersed among a large number of fractions, and the resulting yields of purified material were low. RJ Callow presents a purification scheme using double ammonium nitrate crystallization, whereby the rare earths in monazite (under steady-state conditions, using appropriate recycling of mixed fractions) provided 10% of the rare earth content as a fraction containing 40% praseodymium. In the late 1950's, the Lindsay Chemical Division of the American Potash and Chemical Corporation, at the time the largest producer of rare earths in the world, offered praseodymium salts, purified in this manner, in 30% and 45% grades. The cheapest of these were the double ammonium nitrates, straight from the purification scheme: 30%: $6.30/lb. ($3.85/lb. in 50-lb. quantities), or 45%: $8.20/lb. ($4.95/lb. in 50-lb. quantities) (Reference: Lindsay, Price List, dated October 1, 1958). The one-pound prices for the corresponding oxides were 22.50 and 29.90 for the two purities. This product line soon vanished from the price lists, and was replaced by praseodymium as purified by ion-exchange. By 1959, 99% praseodymium oxide was priced at $40/lb. and the 99.9% grade was priced at $50 per pound, or alternatively at 20 or 25 cents per gram, respectively, in small lots.
Praseodymium has historically been a rare earth whose supply has exceeded demand. This has occasionally led to its being offered more cheaply than the far more abundant neodymium. Unwanted as such, much praseodymium has been marketed as a mixture with lanthanum and cerium, or "LCP" for the first letters of each of the constituents, for use in replacing the traditional lanthanide mixtures that were inexpensively made from monazite or bastnaesite. LCP is what remains of such mixtures, after the desirable neodymium, and all the heavier, rarer and more valuable lanthanides have been removed, by solvent extraction. However, as technology progresses, praseodymium has been found possible to incorporate into neodymium-iron-boron magnets, thereby extending the supply of the much in demand neodymium. So LC is starting to replace LCP as a result.
Praseodymium also makes up about 5% of misch metal.
See also Praseodymium compounds.
The isotopes of praseodymium range in atomic weight from 120.955 u (121Pr) to 158.955 u (159Pr). The primary decay mode before the stable isotope, 141Pr, is electron capture and the primary mode after is beta minus decay. The primary decay products before 141Pr are element 58 (cerium) isotopes and the primary products after are element 60 (neodymium) isotopes.
R.J. Callow, "The Industrial Chemistry of the Lanthanons, Yttrium, Thorium and Uranium", Pergamon Press, 1967.
Price Lists, Lindsay Chemical Division, American Potash & Chemical Corporation, West Chicago, Illinois, dated October 1, 1958 or January 20, 1959.