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Naturally occurring europium is composed of two isotopes, 151 Eu and 153 Eu, which occur in almost equal proportions; 153 Eu is slightly more abundant (52.2% natural abundance). While 153 Eu is stable, 151 Eu was found to be unstable to alpha decay with a half-life of 5 +11
Europium compounds fluoresce under UV light at 395 nm and 365 nm. [1] Europium compounds are compounds formed by the lanthanide metal europium (Eu). In these compounds, europium generally exhibits the +3 oxidation state, such as EuCl 3, Eu(NO 3) 3 and Eu(CH 3 COO) 3. Compounds with europium in the +2 oxidation state are also known.
Rare-earth element abundances of basalts, of both terrestrial and lunar origins [1]. The europium anomaly is the phenomenon whereby the europium (Eu) concentration in a mineral is either enriched or depleted relative to some standard, commonly a chondrite or mid-ocean ridge basalt (MORB).
Naturally occurring europium (63 Eu) is composed of two isotopes, 151 Eu and 153 Eu, with 153 Eu being the most abundant (52.2% natural abundance).While 153 Eu is observationally stable (theoretically can undergo alpha decay with half-life over 5.5×10 17 years), 151 Eu was found in 2007 to be unstable and undergo alpha decay. [4]
Europium hydride is the most common hydride of europium with a chemical formula EuH 2. In this compound, europium atom is in the +2 oxidation state and the hydrogen atoms are -1. [ 3 ] It is a ferromagnetic semiconductor .
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Europium(III) acetate is an inorganic salt of europium and acetic acid with the chemical formula of Eu(CH 3 COO) 3. In this compound, europium exhibits the +3 oxidation state . It can exist in the anhydrous form, sesqui hydrate [ a ] [ 1 ] and tetrahydrate. [ 2 ]
Europium(II) titanate has two different crystal forms depending on the temperature. The phase transition occurs at 282 K. [3] [6] The low temperature form crystallizes in the tetragonal space group I4/mcm (space group No. 140) with the lattice parameters a = 551.92(2) pm, c = 781.64(8) pm (measured at 90 K).