Europium (Eu) is a very reactive silvery metal (the most reactive of the REE) with atomic number (Z) of 63, electronic configuration of [Xe]4f75d06s2, atomic weight of 151.965 and melting point of 1095 K. It is a Group IIIB inner transition element and one of the lanthanide and rare earth elements. Europium has two natural isotopes, 151Eu (47.82%) and 153Eu (52.18%), neither being radioactive. Discovered in 1886 and purified in 1901, Eu is named after Europe.
Europium is typically a trace element in most rocks and minerals. It is refractory and under most conditions is lithophile and found in the trivalent state. Under highly reducing conditions, such as found in magmatic environments, Eu3+ is reduced to Eu2+ leading to a 17% increase in size (Eu2+ is essentially identical in size to Sr2+) and anomalous geochemical behavior. The major importance of europium in geochemistry is that it is one of the middle rare earth elements (or lanthanides), among the most useful trace elements in all...
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© 1998 Kluwer Academic Publishers
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McLennan, S.M. (1998). Europium . In: Geochemistry. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4496-8_119
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DOI: https://doi.org/10.1007/1-4020-4496-8_119
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