Dehydrogenation of Formic Acid Catalyzed by Water-Soluble Ruthenium Complexes: X-ray Crystal Structure of a Diruthenium Complex

2019 ◽  
Vol 2019 (7) ◽  
pp. 1046-1053 ◽  
Author(s):  
Soumyadip Patra ◽  
Mahendra K. Awasthi ◽  
Rohit K. Rai ◽  
Hemanta Deka ◽  
Shaikh M. Mobin ◽  
...  
Keyword(s):  
Crystal Structure ◽  
Formic Acid ◽  
Ruthenium Complexes ◽  
Water Soluble ◽  
X Ray ◽  
Acid Catalyzed ◽  
Diruthenium Complex

ChemInform Abstract: FORMIC ACID-CATALYZED REARRANGEMENT OF CAROTOL. X-RAY CRYSTAL STRUCTURE OF THE P-IODOBENZOATE OF ONE OF THE ALCOHOLS FORMED

1976 ◽  
Vol 7 (39) ◽  
pp. no-no
Author(s):  
L. H. ZALKOW ◽  
M. G. JUN. CLOWER ◽  
M. G. J. SMITH ◽  
D. VANDERVEER ◽  
J. A. BERTRAND
Keyword(s):  
Crystal Structure ◽  
Formic Acid ◽  
X Ray ◽  
Acid Catalyzed

Synthesis and Crystal Structure Determination of Cyclosporin H

2000 ◽  
Vol 65 (8) ◽  
pp. 1317-1328 ◽  
Author(s):  
Alexandr Jegorov ◽  
Ladislav Cvak ◽  
Aleš Husek ◽  
Petr Šimek ◽  
Anna Heydová ◽  
...  
Keyword(s):  
Crystal Structure ◽  
Amino Acids ◽  
Monoclinic Space Group ◽  
X Ray Diffraction ◽  
Synthesis And Crystal Structure ◽  
X Ray ◽  
Acid Catalyzed ◽  
Products Of Reaction ◽  
Cyclosporin H

Acid-catalyzed degradation of cyclosporin A was studied in various solvents and products of reaction were monitored by HPLC. Identification of amino acids and their chirality were determined after hydrolysis and derivatization by GC-MS. Cyclosporin H was isolated as the principal product and its structure was determined by X-ray diffraction: Cyclosporin H- diethyl ether-water (1 : 0.5 : 1) crystallizes in the monoclinic space group I2 with a = 12.338(2) Å, b = 18.963(2) Å, c = 34.074(3) Å, β = 96.47(2)°, Z = 4, and V = 7 921.4(17) Å3.

Formic acid-catalysed rearrangement of carotol. X-Ray crystal structure of the p-iodobenzoate of one of the alcohols formed

1976 ◽  
pp. 374 ◽  
Author(s):  
L. H. Zalkow ◽  
M. G. Clower ◽  
M. Gordon J. Smith ◽  
D. VanDerveer ◽  
J. A. Bertrand
Keyword(s):  
Crystal Structure ◽  
Formic Acid ◽  
X Ray

Ammoniovoltaite, (NH4)2Fe2+5Fe3+3Al(SO4)12(H2O)18, a new mineral from the Severo-Kambalny geothermal field, Kamchatka, Russia

2018 ◽  
Vol 82 (5) ◽  
pp. 1057-1077 ◽  
Author(s):  
Elena S. Zhitova ◽  
Oleg I. Siidra ◽  
Dmitry I. Belakovsky ◽  
Vladimir V. Shilovskikh ◽  
Anton A. Nuzhdaev ◽  
...  
Keyword(s):  
Crystal Structure ◽  
Room Temperature ◽  
Structure Refinement ◽  
Geothermal Field ◽  
Water Soluble ◽  
Ammonium Ion ◽  
New Mineral ◽  
X Ray Diffraction ◽  
X Ray ◽  
Mössbauer Data

AbstractAmmoniovoltaite, (NH4)2Fe2+5Fe3+3Al(SO4)12(H2O)18, is a new voltaite-group mineral. The mineral was discovered at the Severo-Kambalny (North-Kambalny) geothermal field, Kambalny volcanic ridge, Southern Kamchatka, Russia. Ammoniovoltaite forms at ~100°C around geothermal gas/steam vents in association with alunogen, tschermigite and pyrite. Crystals of ammoniovoltaite have euhedral habit, are up to 50 µm in size and grow on alunogen plates. Ammoniovoltaite is black with vitreous lustre, opaque, brittle and water-soluble. Neither cleavage nor parting is found, the fracture is conchoidal. The mineral is isotropic, with the refractive index n = 1.602(2) (589 nm). Infrared spectra contain an absorption band at 1433 cm–1 distinctive for the ammonium ion. The chemical composition is (iron content is given in accordance with Mössbauer data, H2O calculated from a crystal-structure refinement, wt.%): FeO 13.26, Fe2O3 11.58, MgO 2.33, ZnO 0.04, Al2O3 2.74, SO3 47.46, K2O 0.19, CaO 0.11, (NH4)2O 2.96, H2O 16.03, total 96.70. The empirical formula based on S = 12 atoms per formula unit is [(NH4)1.88K0.08Ca0.04]Σ2.00(Fe2+3.74Mg1.17Fe3+0.05Zn0.01)Σ4.97(Fe3+2.89Al0.09)Σ2.98Al1.00(SO4)12.00(H2O)18.00. The crystal structure has been refined to R1 = 0.031 and 0.030 on the basis of 1217 and 1462 unique reflections with I >2σ(I) collected at 100 K and room temperature, respectively. Ammoniovoltaite is the ammonium analogue of voltaite. The mineral is cubic, Fd$\bar{3}$c, a = 27.250(1) Å and V = 20234(3) Å3 (at 100 K); and a = 27.322(1) Å and V = 20396(3) Å3 (at RT), with Z = 16. The strongest lines of the powder X-ray diffraction pattern [d, Å (I, %) (hkl)] are: 9.67 (74) (022), 7.90 (56) (222), 5.58 (84) (422), 3.560 (100) (731), 3.418 (100) (008) and 2.8660 (37) (931). A brief review of ammonium minerals from various volcanically active geological environments is given.

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