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Talybov G. M. Ezizbeyli A. R. Mammadbayli E. H. Shirinova N. A. Guliyeva N. M. 《Russian Journal of Organic Chemistry》2020,56(3):552-554
Russian Journal of Organic Chemistry - Alkoxyiodination of alkyl allyl ethers with elemental iodine in allyl and propargyl alcohols in the presence of clinoptilolite [(NaK)4CaAl6Si30O72] gave the... 相似文献
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Farzaliev V. M. Allakhverdiev M. A. Magerramov A. M. Shirinova N. A. Dzhavadova L. A. Rzaeva I. A. Khalilova A. Z. Aliev F. Yu. 《Russian Journal of Applied Chemistry》2001,74(1):114-117
3-Substituted thietanes were prepared by reaction of 1,2-epithio-3-chloropropane with various nucleophiles in aqueous solutions and were characterized. The inhibiting power of these compounds in cumene oxidation was studied. 相似文献
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A. F. Shirinova M. I. Chiragov S. E. Jafarov M. R. Gasanli 《Crystallography Reports》2012,57(5):742-745
The crystal structure of a clinopyroxene is determined by X-ray diffraction. The unit cell parameters are as follows: a = 9.732(7) ?, b = 8.896(6) ?, c = 5.280(4) ?, and ?? = 106.160(11)°; V = 439.1(5) ?3; space group C2/c; and Z = 4. The structure is determined by the direct method and refined in the anisotropic approximation by the full-matrix least-squares method (R[F 2 > 2??(F 2)] = 0.027, wR(F 2) = 0.072). According to the results of the X-ray structure analysis, the crystal chemical formula of the compound is (Ca0.8Fe0.2)(Mg0.8Fe0.2)Si2O6. In the structure, columns of (Mg, Fe)-octahedra are connected on two sides with Si2O6 chains. The resulting structural units have the [(Mg,Fe)2(Si2O6)2]4? composition. These units form a heterogeneous framework, which is typical of all pyroxene structures. The [(Mg,Fe)2(Si2O6)2]2? composition of the framework corresponds to the ratio [(Mg,Fe) + Si]: O = 3: 6 (1: 2). The (Ca, Fe) atoms are located in the holes of the framework. 相似文献
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O. H. Akperov A. M. Maharramov E. O. Akperov E. A. Shirinova 《Journal of Dispersion Science and Technology》2018,39(9):1244-1251
The capability of the ammonium salt of the cross-linked maleic acid–allylpropionate–styrene terpolymer for the adsorption of Cu2+ from aqueous solutions was examined. Effect of the various experimental parameters on removal degree of the copper ions was investigated. Equilibrium data were fitted to the Langmuir, Freundlich, Dubinin–Radushkevich, and Temkin isotherm models. Kinetics studies suggested that the adsorption allowed pseudo-second-order reaction. The negative values of ΔG° and the positive value of ΔH° indicate that the sorption process is spontaneous and endothermic in nature. The positive value of ΔS° shows the increasing randomness during adsorption process. Considering the FTIR and UV–vis spectra of the sorbent after sorption, it is concluded that Cu2+ enters a complex with carboxylate and ester groups of the sorbent. 相似文献
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A. F. Shirinova V. N. Khrustalev H. R. Samedov M. I. Chiragov 《Crystallography Reports》2006,51(1):37-41
Transparent prismatic single crystals of borate cancrinite (Na,Ca)2[Na6(AlSiO4)6](BO3) · 2H2O are prepared through hydrothermal crystallization. The parameters of the hexagonal unit cell and intensities of 10806 reflections are measured on an Enraf—Nonius CAD4 automated diffractometer. The compound crystallizes in the hexagonal crystal system with the unit cell parameters a = 12.745(4) Å, c = 5.180(2) Å, V = 728.6(4) Å3, and space group P63. The structure is determined by direct methods and refined using the full-matrix least-squares procedure in the anisotropic approximation for the non-hydrogen atoms. The refinement of the structure is performed to the final discrepancy factor R 1 = 0.027 for 2889 unique reflections with I > 2 σ (I). In the structure of the borate cancrinite, the AlO4 and SiO4 tetrahedra form a zeolite-like framework in which twelve-membered hexagonal channels are occupied by sodium atoms and BO3 groups, whereas six-membered channels are filled with sodium and calcium atoms and water molecules. The mean interatomic distances are found to be as follows: (Si-O)mean = 1.614 Å and (Al-O)mean = 1.741 Å in the AlO4 and SiO4 tetrahedra, (Na-O)mean = 2.542 Å in the seven-vertex sodium polyhedra, and [(Na,Ca)-O]mean = 2.589 Å in the ditrigonal bipyramids. 相似文献
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