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1.
Previously unknown compounds AI
I(BUO5)2·nH2O (AI
I = Mg, Ca, Sr, Ba; n = 0-7) were synthesized. Their structure and thermal decomposition were studied by X-ray diffraction, IR spectroscopy, and thermal analysis. 相似文献
2.
Procedures for the synthesis of Li4[UO2(CO3)3]·1.5H2O, Na4[UO2(CO3)3], K4[UO2(CO3)3], (NH4)4[UO2(CO3)3], and K3Na[UO2(CO3)3] were optimized. The structures of these compounds and their thermolysis were studied by X-ray diffraction, precision IR spectroscopy, and thermal analysis. The standard enthalpies of formation of these compounds at 298.15 K were determined by reaction calorimetry. 相似文献
3.
Previously unknown alkaline-earth metal uranogermanates of the general formula MII[HGeUO6]2·nH2O (MII = Mg, Ca) were prepared in the form of higher and intermediate hydrates and anhydrous compounds. The compounds were studied by X-ray diffraction, IR spectroscopy, and thermal analysis. 相似文献
4.
The optimum procedures for synthesis of UO2CO3 and Na4[UO2(CO3)3] were developed. The structures of these compounds and their thermal decomposition were studied by X-ray diffraction, precision IR spectroscopy, and thermography. The standard enthalpy of formation of crystalline Na4[UO2(CO3)3] at 298.16 K was determined to be -4010.0±8.0 kJ mol-
1. 相似文献
5.
A. V. Knyazev N. G. Chernorukov M. S. Sheiman S. C. Ponomarev Yu. S. Sazhina 《Radiochemistry》2006,48(5):434-436
The standard enthalpy of formation of crystalline Ba2Sm2/3UO6 at 298.15 K, ?3040.0±7.5 kJ mol?1, was determined by reaction calorimetry. The heat capacity of the compound in the range 80–300 K was measured by adiabatic vacuum calorimetry, and its thermodynamic functions were calculated. Its standard entropy of formation at 298.15 K is ?592.5±1.0 J mol?1 K?1, and the Gibbs energy of formation at 298.15 K, ?2863.5±8.0 kJ mol?1. The standard thermodynamic functions of the reactions of the Ba2Sm2/3UO6 synthesis were calculated and discussed. 相似文献
6.
7.
N. G. Chernorukov A. V. Knyazev M. S. Sheiman S. C. Ponomarev T. A. Gur’eva 《Radiochemistry》2006,48(5):437-440
The standard enthalpy of formation of crystalline Lu(HSiUO6)3 · 10H2O at 298.15 K, ?10668.0±16.0 kJ mol?1, and the standard enthalpy of its dehydration were determined by reaction calorimetry. The heat capacity of this compound in the range 80–300 K was measured by adiabatic vacuum calorimetry, and its thermodynamic functions were calculated. The standard entropy of formation at 298.15 K is ?3812.9±1.2 J mol?1 K?1, and the standard Gibbs energy of formation at 298.15 K, ?9531.0±16.5 kJ mol?1. The standard thermodynamic functions of the reactions of the synthesis of lutetium uranosilicate were calculated and discussed. 相似文献
8.
The solubility of poorly soluble uranoarsenates MAsUO6·H2O in water and aqueous HClO4 was determined. The solubility products and Gibbs energies of formation of these compounds were evaluated from the experimental data using the principles of equilibrium thermodynamics. The state of uranoarsenates in aqueous solutions in the range not studied experimentally was estimated. 相似文献
9.
A synthetic analog of soddyite mineral, (UO2)2SiO4·2H2O, was prepared by hydrolyzing ammonium uranosilicate under hydrothermal conditions. The germanium-containing structural analog of soddyite, (UO2)2GeO4·2H2O, was synthesized by precipitation from solution. The compound UO2(BO2)2 was prepared by reaction with molten boron oxide. The structures and properties of the compounds prepared were studied by X-ray diffraction analysis, IR spectroscopy, and thermography. The enthalpies of formation of the compounds were determined by adiabatic reaction calorimetry. 相似文献
10.
O. V. Nipruk N. G. Chernorukov Yu. P. Pykhova N. S. Godovanova A. A. Eremina 《Radiochemistry》2011,53(5):483-490
The state of uranyl phosphates and arsenates (UO2)3(PO4)2·nH2O and (UO2)3(AsO4)2·nH2O in aqueous solutions in the interval of pH 1–14 was studied by X-ray diffraction, IR spectroscopy, thermography, and chemical
analysis. The composition and structure of the initial solid phases vary depending on the solution acidity. The equilibrium
constants of the reactions occurring in the heterogeneous systems (UO2)3(BVO4)2·nH2O (BV = P, As)-aqueous solution were calculated. The speciation diagrams of the solid phases and equilibrium solutions were plotted. 相似文献