The title Sm(III) compound, {[Sm(C(9)H(7)O(3))(3)(H(2)O)]·H(2)O}(n), was obtained under hydrothermal conditions. Its structure is isotypic with the analogous Eu complex. The latter was reported incorrectly in space group P1 by Yan et al. [J. Mol. Struct. (2008), 891, 298-304]. This was corrected by Marsh [Acta Cryst. B65, 782-783] to P-1. The Sm(III) ion is nine-coordinated by O atoms from one coordinating water molecule and the remaining ones from the 3-(3-hy-droxy-phen-yl)prop-2-enoatate anions (one bidentate, two bidentate and bridging, two monodentate bridging), leading to a distorted tricapped trigonal-prismatic coordination polyhedron surrounded by solvent water mol-ecules. In the crystal, extensive intermolecular O-H⋯O hydrogen-bonding inter-actions and π-π inter-actions [centroid-centroid separation = 3.9393 (1) Å] lead to the formation of a three-dimensional supra-molecular network.
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http://dx.doi.org/10.1107/S1600536812013724 | DOI Listing |
Acta Crystallogr E Crystallogr Commun
October 2024
Faculty of Environment and Information Sciences Yokohama National University, 79-7 Tokiwadai Hodogaya-ku Yokohama-shi Kanagawa 240-8501 Japan.
The title compound, a hydrate of 3,5-di-amino-1,2,4-triazole (DATA), CHN·HO, was synthesized in the presence of sodium perchlorate. The evaporation of HO from its aqueous solution resulted in anhydrous DATA, suggesting that sodium perchlorate was required to precipitate the DATA hydrate. The DATA hydrate crystallizes in the 2/ space group in the form of needle-shaped crystals with one DATA and one water mol-ecule in the asymmetric unit.
View Article and Find Full Text PDFIn the hydrated title complex, [Fe(dpa)(N)]·HO (dpa is 2,2'-di-pyridyl-amine, CHN), the Fe ion is coordinated in a distorted octa-hedral manner by two neutral, chelating dpa ligands and two anionic, monodentate azide (N ) ions in a -configuration. Distortion results from different Fe-N bond lengths [2.1397 (13)-2.
View Article and Find Full Text PDFUrolithiasis
November 2024
Guangdong Province Hospital of Chinese Medicine, Guangzhou, Guangdong Province, China.
Jackstone calculi are a rare and distinctive type of urinary stone characterized by their radiating spicule structure. They are primarily found in the bladder, and also occur in the renal pelvis. Because jackstone calculi are infrequently encountered in clinical practice, studies on their pathophysiology and clinical implications are relatively limited.
View Article and Find Full Text PDFActa Crystallogr E Crystallogr Commun
September 2024
Institute of Inorganic Chemistry, Leipzig University, Johannisallee 29, D-04103 Leipzig, Germany.
In the structure of the title salt, {[Ba(μ-CHNO)(μ-HO)(HO)]·HO} , the barium ion and all three oxygen atoms of the water mol-ecules reside on a mirror plane. The hydrogen atoms of the bridging water and the solvate water mol-ecules are arranged across a mirror plane whereas all atoms of the monodentate aqua ligand are situated on this mirror plane. The distorted ninefold coord-ination of the Ba ions is completed with four nitroso-, two carbonyl- and three aqua-O atoms at the distances of 2.
View Article and Find Full Text PDFIUCrdata
August 2024
Department of Chemistry and Biochemistry Fordham University, 441 East Fordham Road Bronx NY 10458 USA.
The title structure, {[Cu(CHNO)][Cu(CN)]·[Cu(CHNO)(HO)]·HO} , is made up of diperiodic honeycomb CuCN networks built from [Cu(CN)] units, together with two independent Cu complexes: six-coord-inate [Cu(CHCHCH(NH)CHOH)] cations, and five-coordinate [Cu(CHCHCH(NH)CHO)·HO] neutral species. The two Cu complexes are not covalently bonded to the CuCN networks. Strong O-H⋯O hydrogen bonds link the Cu complexes into pairs and the pairs are hydrogen bonded into chains along the crystallographic axis the hydrate water mol-ecule.
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