FC(O)O自由基与NO2反应的量子化学研究

用量子化学DFT, MP2, G3和G3MP2方法对FC(O)O自由基与NO₂的反应机理进行了理论研究. 优化了反应势能面上各驻点的几何结构, 通过内禀反应坐标(IRC)计算和振动分析, 确认了反应中的过渡态, 并用过渡态理论(TST)计算了相关反应的速率常数.     

FC(O)O自由基与NO2反应的量子化学研究

用量子化学DFT, MP2, G3和G3MP2方法对FC(O)O自由基与NO₂的反应机理进行了理论研究. 优化了反应势能面上各驻点的几何结构, 通过内禀反应坐标(IRC)计算和振动分析, 确认了反应中的过渡态, 并用过渡态理论(TST)计算了相关反应的速率常数.     

应用离子选择性电极进行溶液热力学研究 Ⅴ:KCl在283.15K～318.15K间七个温度下由H~2O至DMF-H~2O混合溶剂的标准转移Gibbs自由和转移熵的测定

本文应用Corning一价阳离子选择电极与氯离子选择电极组成无液接可逆电池,测定电池在283.15K～318.15K间七个温度下的标准电动势及其温度系数,计算KCl从纯水到相应的DMF-H~2O混合溶剂的标准转移Gibbs自由能ΔG 和标准转移熵ΔS ,得出ΔG 和ΔS 随混合溶剂中DMF的摩尔分数x~DMF及温度T的变化规律.发现KCl的ΔS随x~DMF变化的趋势和NaCl的相反.从离子溶剂化作用及其对溶剂结构的影响作了讨论.     

应用离子选择性电极进行溶液热力学研究 Ⅴ:KCl在283.15K～318.15K间七个温度下由H~2O至DMF-H~2O混合溶剂的标准转移Gibbs自由和转移熵的测定

本文应用Corning一价阳离子选择电极与氯离子选择电极组成无液接可逆电池,测定电池在283.15K～318.15K间七个温度下的标准电动势及其温度系数,计算KCl从纯水到相应的DMF-H~2O混合溶剂的标准转移Gibbs自由能ΔG 和标准转移熵ΔS ,得出ΔG 和ΔS 随混合溶剂中DMF的摩尔分数x~DMF及温度T的变化规律.发现KCl的ΔS随x~DMF变化的趋势和NaCl的相反.从离子溶剂化作用及其对溶剂结构的影响作了讨论.     

稀土钬及铒钇丙氨酸配合物的量热与热分析研究

合成了两种固态稀土丙氨酸配合物[Ho2(Ala)4(H2O)8]Cl6和[ErY(Ala)4(H2O)8](ClO4)6 (Ala为丙氨酸),用量热和热分析方法研究了这两种配合物的热力学性质.用全自动高精密绝热量热计测定了在78～377 K温区内的低温热容.对于[Ho2(Ala)4(H2O)8]Cl6,在214～255 K温区内发现一固-固相变,其相变温度为235.09 K.对于[ErY(Ala)4(H2O)8](ClO4)6,在99～121 K温区内也发现一固-固相变,其相变温度为115.78 K. [Ho2(Ala)4(H2O)8]Cl6固-固相变焓为3.02 kJ• mol－1,相变熵为12.83 J•K－1•mol－1； [ErY(Ala)4(H2O)8](ClO4)6 固-固相变焓为1.96 kJ•mol－1,相变熵为16.90 J•K－1•mol－1.同时,用TG技术在40～800 ℃温区研究了两配合物的热稳定性.由TG/DTG曲线分析可知, [Ho2(Ala)4(H2O)8]Cl6从80 ℃到479 ℃热分解分两步完成, [ErY(Ala)4(H2O)8](ClO4)6从120 ℃到430 ℃热分解分三步完成.     

反相微乳液介质中Nd2(CO3)3·8H2 O的可控合成

以十六烷基三甲基溴化铵(CTAB)/正丁醇/正辛烷/硝酸钕[Nd(NO3)3]溶液(碳酸钠溶液)所组成的反相微乳液为反应介质, 采用微乳液溶剂热法合成了Nd2(CO3)3·8H2O, 并考察了水/核比([H2O]/[CTAB])和Nd(NO3)3的浓度对其形貌和尺寸的影响. 利用X射线衍射(XRD)、 热分析(DSC-TGA)、 扫描电子显微镜(SEM)和透射电子显微镜(TEM)等对Nd2(CO3)3·8H2O的晶型、 形貌及尺寸进行了表征, 并提出了不同形貌Nd2(CO3)3·8H2O形成的可能机理. 结果表明, 随着水/核比的增大, Nd2(CO3)3·8H2O的形貌从多面体变成鱼尾状, 再变成针状; 随着Nd(NO3)3浓度的增大, 针状Nd2(CO3)3·8H2O的尺寸逐渐减小.     

CO_2/H_2O混合绿色介质中的有机催化反应

绿色化学是化学发展的必然趋势。有效利用绿色溶剂是绿色化学的重要内容。CO2和H2O混合体系是具有很多特点的绿色反应介质,可以用于不同化学反应,特别是弱酸催化的反应,从而替代传统的有机酸和无机酸。本文讨论了CO2/H2O体系的酸性随温度和压力的变化,综述了在CO2/H2O混合绿色介质中有机化学反应研究进展,这些反应包括脱水反应、烷基化反应、香茅醛环化反应、重氮化反应、多元醇转化成环醚的反应、溴氧化反应、芳硝基化合物选择性还原、多糖水解反应、生物质转化反应、环氧丙烷水解反应、脱羧反应、醇氧化反应、对映选择氧化反应以及酮不对称还原;最后对CO2/H2O体系在化学反应中应用的发展趋势进行了探讨。     

Al(H2O)63+水交换反应溶剂效应的量子化学团簇模型-密度泛函理论方法研究

在气相模型、极化连续模型、超分子模型和超分子-极化连续模型的基础上,采用量子化学团簇模型密度泛函理论方法,在B3LYP/6-311+G(d,p)基组水平下系统地开展了以下研究:优化得到Al(H2O)63+水交换反应的反应物、过渡态和产物构型,采用MP2方法在相同基组水平下计算得到相应的单点能,考虑零点振动能、热力学校正项和熵等参数的影响,计算得到Al(H2O)63+水交换反应的Gibbs自由能变和反应速率常数kex.计算结果表明:GP-SM//MP2-PCM和GP-SM-PCM//MP2-PCM模型得到的kex相近,并且与文献值相符,说明GP-SM//MP2-PCM模型可以充分考虑真实溶剂效应和主体溶剂效应,适用于Al(H3O)63+体系水交换反应的模拟.     

ZrW1.7ⅥW0.3ⅤO7H0.3(OH)2·2H2O的合成与表征

分别利用微乳液水热法和酸蒸气水热法合成了杂多蓝化合物ZrW1.7ⅥW0.3ⅤO7H0.3(OH)2·2H2O.XRD测定结果表明,该化合物与ZrMo2O7(OH)2·2H2O具有相同晶体结构类型.使用Rietveld方法对产物进行了结构精修,并计算出了键参数和键价.运用EPR技术测定了该化合物中W的价态,并利用XPS能谱测定了W/W的比例.利用价键和规则,指出ZrW1.7ⅥW0.3ⅤO7H0.3(OH)2·2H2O中的W—O3—H0.15存在羟基化现象,并对杂多蓝化合物的红外吸收光谱进行了指认.     

煤炭燃烧过程中N2O消除反应机理的密度泛函理论研究

用密度泛函理论B3LYP方法对煤炭燃烧过程中N₂O的消除反应进行研究。选用6-311++G**和aug-cc-pVTZ基组,优化了反应通道上反应物、过渡态和产物的几何构型。预测了它们的热力学性质(总能量、焓、熵和吉布斯自由能)及其随温度的变化。预测N₂O+CO反应的活化能为200 kJ·mol^-1,与实验值193±8 kJ·mol^-1较一致。计算了500~1 800 K 温度范围的反应速率常数。在N₂O的分解中,N₂O与H和CN自由基的反应为动力学优先进行的反应,其活化能为50~55 kJ·mol^-1。在B3LYP/aug-cc-pVTZ level水平下,N₂O+CN反应是热力学最有利的自发反应,其吉布斯自由能变化为-407 kJ·mol^-1。     

Tetracyanonickelate compounds as sorptive materials and the substitution of their H2O content by D2O

The compounds NiNi(CN)₄·3,5H₂O and Ni(NH₃)₂Ni(CN)₄·H₂O have been studied to examine the possibility of substituting their H₂O or NH₃ content by D₂O. Contact with D₂O was performed after heating the compounds to several temperatures. Depending on the degree of decomposition of the original compounds different ranges of substitution were possible. In such manner the compounds NiNi(CN)₄·3,5D₂O, NiNi(CN)₄·5D₂O, Ni(NH₃)₂Ni(CN)₄·D₂O, and Ni(D₂O)₂Ni(CN)₄·D₂O were prepared and thermally they were less stable than the original ones. The substitution by D₂O is in agreement with the sorptive properties of the original tetracyanonickelate against different organic compounds using GC, since these could substitute the guest component and sometimes also the ligands during their decomposition.     

Tribochemistry and kinetics of Al2(SO4)3·xH2O decomposition

The thermal decomposition of tribochemically activated Al₂(SO₄)₃·xH₂O was studied by TG, DTA and EMF methods. For some of the intermediate solids, X-ray diffraction and IR-spectroscopy were applied to learn more about the reaction mechanism. Thermal and EMF studies confirmed that, even after mechanical activation of Al₂(SO₄)₃·xH₂O, Al₂O(SO₄)₂ is formed as an intermediate. Isothermal kinetic experiments demonstrated that the thermochemical sulphurization of inactivated Al₂(SO₄)₃·xH₂O has an activation energy of 102.2 kJ·mol^?1 in the temperature range 850–890 K. The activation energy for activated Al₂(SO₄)₃·xH₂O in the range 850–890 K is 55.0 kJ·mol^?1. The time of thermal decomposition is almost halved when Al₂(SO₄)₃·xH₂O is activated mechanically. The results permit conclusions concerning the efficiency of the tribochemical activation of Al₂(SO₄)₃·xH₂O and the chemical and kinetic mechanisms of the desulphurization process.     

Infrared spectra (700–200 cm−1) and6Li/7Li and H2O/D2O isotope effects for four isotopically substituted lithium formate monohydrates

The infrared spectra, in the 700–200 cm^–1 region, have been reported for⁶LiHCO₂ · H₂O,⁶LiHCO₂ · D₂O,⁷LiHCO₂ · H₂O and⁷LiHCO₂ · D₂O and the observed fundamental bands have been discussed taking into account the⁶Li/⁷Li and H₂O/D₂O isotope wavenumber shifts on the fundamental vibrations.

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Infrarotspektren (700–200 cm^–1) und⁶Li/⁷Li- und H₂O/D₂O-Isotopeneffekte für vier isotopensubstituierte Lithiumformat-monohydrate

Zusammenfassung Die Infrarotspektren in der Region von 700–200 cm^–1 werden für⁶LiHCO₂ · H₂O,⁶LiHCO₂ · D₂O,⁷LiHCO₂ · H₂O und⁷LiHCO₂ · D₂O angegeben und die beobachteten Grundschwingungen zusammen mit den isotopischen Verschiebungen der Wellenzahlen diskutiert.

     

DSC study of the phase transitions in [Ni(D2O)6](ClO4)2 and [Ni(H2O)6](ClO4)2

DSC measurements were carried out for [Ni(H₂O)₆](ClO₄)₂ (sampleH) and [Ni(D₂O)₆](ClO₄)₂ (sampleD) in the temperature range 300–380 K. For both compounds two anomalies on the DSC curves were detected. The results for sampleH are compared to those previously obtained using adiabatic calorimetry method. For both compounds studied in this work the high-temperature transition appears at the same temperature while the low-temperature one is shifted towards higher temperatures in sampleD. Disorder connected with H₂O or D₂O groups is suggested in the intermediate phase between the low- and high-temperature transitions.     

Synthesis and thermal investigation of Na2Cd(SO4)2·2H2O

The synthesis and thermal decomposition of Na₂(SO₄)₂·2H₂O in both air and nitrogen are described. The synthesis was performed by two different procedures, but in both cases the same product was obtained, corresponding to the general formula given above. The crystals obtained were investigated by methods of X-ray powder diffraction, and chemical and thermal analysis. The differences in thermal decomposition in air and nitrogen are discussed.     

Studies on synthesis, characterization and thermochemistry of Mg2[B2O4(OH)2]·H2O

A new magnesium borate Mg₂[B₂O₄(OH)₂]·H₂O has been synthesized by the method of phase transformation of double salt at hydrothermal condition and characterized by XRD, IR, TG and DSC. The enthalpy of solution of Mg₂[B₂O₄(OH)₂]·H₂O in 0.9764 mol L^–1 HCl was determined. With the incorporation of the enthalpies of solution of H₃BO₃ in HCl (aq), of MgO in (HCl+H₃BO₃) (aq), and the standard molar enthalpies of formation of MgO(s), H₃BO₃(s), and H₂O(l), the standard molar enthalpy of formation of –(3185.78±1.91) kJ mol^–1 of Mg₂[B₂O₄(OH)₂]·H₂O was obtained.This revised version was published online in November 2005 with corrections to the Cover Date.     

Freezing-point of mixtures of H 2 16 O and H 2 18 O

Freezing-point depression of mixtures of H ₂ ¹⁶ O and H ₂ ¹⁸ O were measured. The results showed that the freezing point of the mixture rose linearly with an increase in the molal concentration of H ₂ ¹⁸ O. The results suggested the formation of a solid solution of H ₂ ¹⁶ O and H ₂ ¹⁸ O by freezing, similar to that formed by H ₂ O–D ₂ O, and that H ₂ ¹⁸ O behaves as a different molecule than H ₂ ¹⁶ O.     

TG/DTA/MS Study of the thermal decomposition of FeSO4·6H2O

The thermal decomposition of FeSO₄·6H₂O was studied by mass spectroscopy coupled with DTA/TG thermal analysis under inert atmosphere. On the ground of TG measurements, the mechanism of decomposition of FeSO₄·6H₂O is: i) three dehydration steps FeSO₄·6H₂O FeSO₄·4H₂O+2H₂O FeSO₄·4H₂O FeSO₄·H₂O+3H₂O FeSO₄·H₂O FeSO4+H₂O ii) two decomposition steps 6FeSO₄ Fe₂(SO₄)₃+2Fe₂O₃+2SO₂ Fe₂(SO₄)3 Fe₂O₃+3SO₂+3/2O₂ The intermediate compound was identified as Fe₂(SO₄)₃ and the final product as the hematite Fe₂O₃.     

Isotopic substitution effects on the volumetric and viscosimetric properties of water-dimethylsulfoxide mixtures at 25°C

Densities and viscosities of binary mixtures (H₂O or D₂O) (1) + (DMSO or DMSO-D6)(2) have been measured over the entire mole fraction range; and the excess volumes, excess viscosities, and excess partial molar volumes Vf of the components have been obtained. All systems show negative excess volume V^e at all compositions, values for mixtures containing D₂O being more negative than those with H₂O byca. 0.03 cm³-mol^-1 at x₁, = 0.6, where a minimum is observed. The difference between DMSO and DMSO-D6 containing mixtures is negligible. The excess viscosity η^e is always positive and shows a maximum at x₁ = 0.65; at this composition, the substitution of H₂O with D₂O causes an excess viscosity increment ofca. 0.35 mPa-s, while deuteration of DMSO brings about a smaller increase,ca. 0.1 mPa-s. The trend of V ₂ ^E with concentration shows the characteristic features of moderately hydrophobic solutes in water (negative values and a minimum in the water-rich region), features that are slightly but significantly more marked in D₂O than in H₂O. The V ₂ ^E values in the water-diluted region and at x₁, =0 are more negative for D₂O than for H₂O.     

Synthesis and thermal decomposition of potassium peroxotitanate to K2Ti2O5

Potassium peroxotitanate was synthesized by the peroxo method. During the thermal decomposition K₂Ti₂O₅ can be obtained. The isothermal conditions for decomposition of K₂[Ti₂(O₂)₂(OH)₆]·3H₂O were determined on the base of DTA, TG and DSC results. DTA and TG curves were recorded in the temperature range 20 and 900°C at a heating rate of 10°C min^–1. The obtained intermediate compounds were characterized by means of quantitative analysis and IR spectroscopy. The mechanism of thermal decomposition of K₂[Ti₂(O₂)₂(OH)₆]·3H₂O to K₂Ti₂O₅ was studied. The optimal conditions for obtaining K₂Ti₂O₅ were determined (770°C for 10 h).