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Uranyl

The uranyl ion is an oxycation of uranium in the oxidation state +6, with the chemical formula UO2+2. It has a linear structure with short U–O bonds, indicative of the presence of multiple bonds between uranium and oxygen. Four or more ligands may be bound to the uranyl ion in an equatorial plane. The uranyl ion forms many complexes, particularly with ligands that have oxygen donor atoms. Complexes of the uranyl ion are important in the extraction of uranium from its ores and in nuclear fuel reprocessing. The uranyl ion is an oxycation of uranium in the oxidation state +6, with the chemical formula UO2+2. It has a linear structure with short U–O bonds, indicative of the presence of multiple bonds between uranium and oxygen. Four or more ligands may be bound to the uranyl ion in an equatorial plane. The uranyl ion forms many complexes, particularly with ligands that have oxygen donor atoms. Complexes of the uranyl ion are important in the extraction of uranium from its ores and in nuclear fuel reprocessing. The uranyl ion is linear and symmetrical, with both U–O bond lengths of about 180 pm. The bond lengths are indicative of the presence of multiple bonding between the uranium and oxygen atoms. Since uranium(VI) has the electronic configuration of the preceding noble gas, radon, the electrons used in forming the U–O bonds are supplied by the oxygen atoms. The electrons are donated into empty atomic orbitals on the uranium atom. The empty orbitals of lowest energy are 7s, 5f and 6d. In terms of valence bond theory the sigma bonds may be formed using dz2 and fz3 to construct sd, sf and df hybrid orbitals (the z-axis passes through the oxygen atoms). (dxz, dyz) and (fxz2 and fyz2) may be used to form pi bonds. Since the pair of d or f orbitals used in bonding are doubly degenerate this equates to an overall bond order of three. The uranyl ion is always associated with other ligands. The most common arrangement is for the so-called equatorial ligands to lie in a plane perpendicular to the O–U–O line and passing through the uranium atom. With four ligands, as in 2−, the uranium has a distorted octahedral environment. In many cases there are more than four equatorial ligands. The presence of the equatorial ligands lowers the symmetry of the uranyl ion from point group D∞h for the isolated ion to, for example, D4h in a distorted octahedral complex; this permits the involvement of d and f orbitals other than those used in U–O bonds. In uranyl fluoride, UO2F2, the uranium atom achieves a coordination number of 8 by forming a layer structure with two oxygen atoms in a uranyl configuration and six fluoride ions bridging between uranyl groups. A similar structure is found in α-uranium trioxide, with oxygen in place of fluoride, except that in that case the layers are connected by sharing oxygen atom from 'uranyl groups', which are identified by having relatively short U–O distances. A similar structure occurs in some uranates, such as calcium uranate, CaUO4, which may be written as Ca(UO2)O2 even though the structure does not contain isolated uranyl groups. The colour of uranyl compounds is due to ligand-to-metal charge transfer transitions at ca. 420 nm, on the blue edge of the visible spectrum. The exact location of the absorption band and NEXAFS bands depends on the nature of the equatorial ligands. Compounds containing the uranyl ion are usually yellow, though some compounds are red, orange or green. Uranyl compounds also exhibit luminescence. The first study of the green luminescence of uranium glass, by Brewster in 1849, began extensive studies of the spectroscopy of the uranyl ion. Detailed understanding of this spectrum was obtained 130 years later. It is now well-established that the uranyl luminescence is more specifically a phosphorescence, as it is due to a transition from the lowest triplet excited state to the singlet ground state. The luminescence from K2UO2(SO4)2 was involved in the discovery of radioactivity. The uranyl ion has characteristic νU–O stretching vibrations at ca. 880 cm−1 (Raman spectrum) and 950 cm−1 (infrared spectrum). These frequencies depend somewhat on which ligands are present in the equatorial plane. Correlations are available between the stretching frequency and U–O bond length. It has also been observed that the stretching frequency correlates with the position of the equatorial ligands in the spectrochemical series. The uranyl ion can be viewed as the end result of extensive hydrolysis of the highly charged, hypothetical, U6+ cation. The driving force for this hypothetical reaction is the reduction in charge density on the uranium atom. The number of water molecules attached to the uranyl ion in aqueous solution is mostly five. Further hydrolysis occurs, with a further reduction in charge density when one or more equatorial water molecules is replaced by a hydroxide ion. In fact the aqueous uranyl ion is a weak acid.

[ "Ion", "Uranium", "Phosphuranylite", "Curite", "Metatorbernite", "Compreignacite", "Uranyl carbonate" ]
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