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Historical Background
In 1841, Swedish chemist Carl Gustaf Mosander extracted the rare earth element didymia from lanthana. In 1879, French chemist Paul Emile Lecoq de Boisbaudran isolated a new earth, samaria, from didymia obtained from the mineral samarskite. Six years later, in 1885, a German chemist named Carl F. von Welsbach separated didymium into two elements, praseodymium and neodymium. Praseodymium occurs along with other rare-earth elements in a variety of minerals, but monazite and bastnasite are the two main commercial sources. Praesodymium was prepared in relatively pure form in 1931. Today, praseodymium is mostly obtained through an ion exchange process from monazite sand, a material rich in rare earth elements. |