（四甲基二硅撑）双（3—三甲硅基环戊二烯基）—四羰基二铁…

标题化合物（Ｍｅ２ＳｉＳｉＭｅ２）〔η＾５－（３－Ｍｅ３ＳｉＣ５Ｈ３）Ｆｅ（ＣＯ）２〕２／（μ－ＣＯ）２（Ａ）分子中的Ｆｅ－Ｆｅ键被钠汞齐还原断裂，生成相应的双铁负离子，分别与ＭｅＣＯＣｌ、ＰｈＣＯＣｌ、ＰｈＣＨ２Ｃｌ、ＣｌＣＨ２ＣＯＯＣ２Ｈ５和Ｐｈ３ＳｎＣｌ进行亲核取代反应，生成在铁原子上引入相应取代基的产物（Ｍｅ２ＳｉＳｉＭｅ２）〔η＾５－（３－Ｍｅ３ＳｉＣ５Ｈ３）Ｆｅ（ＣＯ）２Ｒ〕２（Ｒ：Ｍ     

类水滑石[CdxMg6—xAl2（OH）16]^2＋[S.2H2O]^2—l的合成与表征

用中温水热法合成了类水滑石〔ＣｄｘＭｇ６－ｘＡｌ２（ＯＨ）１６〕＾２＋〔Ｓ．２Ｈ２Ｏ〕＾２－，探讨了ＰＨ值、投入Ｃｄ＾２＋离子的量以及硫化时间等条件对合成的影响，并用ＸＲＤ、ＦＴ－ＩＲ、ＤＴＡ－ＴＧ等手段进行了表征，找出了合成层间嵌入Ｓ＾２－离子的含Ｃｄ类水滑石的最佳条件。     

Co-Mo/TiO2和Co-Mo/γ-Al2O3加氢脱硫催化剂的研究

本文考察了ＣｏＭｏ／ＴｉＯ２和ＣｏＭｏ／γ－Ａｌ２Ｏ３催化剂的加氢脱硫性能及表面结构变化和处理条件对其活性的影响，担体ＴｉＯ２（Ａ）和ＴｉＯ２（Ｂ）分别采用ＴｉＯＳＯ４水解法制备，结果表明，催化剂的活性顺序为ＣｏＭｏ／ＴｉＯ２（Ａ）＞ＣｏＭｏ／ＴｉＯ２（Ｂ）＞ＣｏＭｏ／γ－Ａｌ２Ｏ３，催化剂的预处理条件对催化剂的加氢脱硫和加氢活性有很大影响，ＴｉＯ２担体上Ｍｏ物种主要以八面体配位构型存在，Ｍｏ＾－     

金属键有机化合物的研究—非对称型η^5—取代环戊二烯…

通过η＾５－Ｒ＾１Ｃ５Ｈ４（ＣＯ）３ＭＨａ与η＾５－Ｒ＾２Ｃ５Ｈ４（ＣＯ）２ＭＮａ（Ｍ＝Ｍｏ，Ｗ）以及η＾５－Ｒ＾１Ｃ５Ｈ４（ＣＯ）３ＭｏＮａ与η＾５－Ｒ＾２Ｃ５Ｈ４（ＣＯ）３ＷＮａ在Ｆｅ２（ＳＯ４）３醋酸水溶液作用下的交叉氧化偶联反应，合成了７个新的非对称型金属单键化合物η＾５－Ｒ＾１Ｃ５Ｈ４（ＣＯ）３Ｍｏ－Ｍｏ（ＣＯ）３Ｃ５Ｈ４Ｒ＾２－η＾５（Ｒ＾１，Ｒ＾２：Ｃ（Ｏ）Ｍｅ，ＣＯ２Ｅｔ），η＾５     

碳基铁—硫醇（硫酚）—格氏试剂体系与芳酰氯反应的研究：…

通过Ｆｅ３（ＣＯ）１２、硫醇（硫酚）和ＥｔＭｇＢｒ所形成的络盐［（μ－ＣＯ）（μ－ＲＳ）Ｆｅ２（ＣＯ６）》－Ｍｇ＾＋Ｂｒ与氯代芳酰氯的原位反应，合成了通式为（μ－ＲＳ）（μ－ｏ－ＣｌＣ６Ｈ４ＣＯ）Ｆｅ２（ＣＯ６）和（μ－ＲＳ）（μ－ｍ－ＣｌＣ６Ｈ４ＣＯ）Ｆｅ２（ＣＯ）６（Ｒ＝ｎ－Ｂｕ，ｔ－Ｂｕ，Ｐｈ）的６个新桥芳酰基铁硫配合物，并用Ｃ／Ｈ分析、ＩＲ和＾１ＨＮＭＲ表征了它们的结构。     

钨硅系列三元杂多阴离柱撑阴离子粘土的合成及表征

采用离子交换法将过渡金属离了三元取代钨杂多阴离子引入Ｚｎ２Ａｌ型阴离子粘土层内，得到柱撑水滑石Ｚｎ２Ａｌ（ＯＨ）６－ＳｉＷ９Ｚ３Ｏ４０（Ｚ＝Ｔｉ＾４＋，Ｍｏ＾６＋）及Ｚｎ２Ａｌ（ＯＨ）６－ＳｉＷ９Ｆｅ３（Ｈ２Ｏ２）３Ｏ３７。ＺＲＤ及ＩＲ表明，杂多阴离子引入水滑石层间后，水滑石层内高度为１．０ｎｍ。     

同时测定水中阴,阳离子的单柱阴离子排斥—阳离子交换色谱法

采用单柱离子色谱系统和电导检测的方法,以丙二酸为淋洗液,同时有效地分离、检测了溶液中ＳＯ４＾２－、Ｃｌ＾－、ＮＯ３＾－、Ｆ＾－、ＮＨ４＾＋、Ｋ＾＋、Ｍｇ＾２＋、Ｃａ＾２＋９种离子。研究了丙二酸浓度和流速对各离子保留时间及电导检测行为的影响。该法用于目前市售饮用水中的阴阳离子分析,得到了满意的结果。     

丙醇—溴化十六烷基三甲胺—硫酸铵—水体系萃取分离汞（Ⅱ）

研究了丙醇－溴化十六烷基三甲胺９ＣＴＭＡＢ）－（ＮＨ４）２ＳＯ４－水体系萃取分离泵的行为及与常见离子分离条件。试验表明：调节ｐＨ１．０或３．０,能使Ｈｇ从Ｆｅ＾３＋,Ｃｏ＾２＋,Ｎｉ＾２＋ｍ,Ｚｎ＾２＋,Ｍｎ＾２＋,Ｃｕ＾２＋,Ａｌ６３＋等离子混合液中分离出来。     

溶胶-凝胶制备技术与新型催化材料Ⅲ.溶胶粒子表面修饰方法制备催化膜

提出用溶胶粒子表面修饰方法，结合溶胶－凝胶技术制备无机催化膜，该方法的基本原理是利用合适的金属配合物在胶粒表面吸附作用，经溶胶－凝胶过程，将活性组分结合到无机膜中，实验测定结果表明：（ＮｉＥＤＴＡ）＾２－，ＶＯ＾－３，ＭｏＯ＾２－４，（Ｐｄ（ＮＨ３）４＾２＋，ＰｄＣｌ＾２－４，ＰｔＣｌ＾２－６和ＲｈＣｌ＾３－６可用来修饰ＡｌＯＯＨ溶胶，以Ｐｄ／γ－Ａｌ２Ｏ３催化膜的制备为例，经三次溶胶－凝胶过程，     

钙—亚硫酰氯电池的研究

应用交流阻抗，恒电流，ＳＥＭ等方法，研究了Ｃａ－ＳＯＣｌ２电池中ＣａＣｌ２（ＳＥＩ）膜的性质，不同电解质和添加剂对电极性的影响，结果表明，ＣａＣｌ２ＳＥＩ膜在阳极反应电阻下降，ＣｕＣｌ２，ＣｕＢｒ２可改变ＣａＣｌ２沉积形态，提高阴极性能，组装的Ｃａ－ＳＯＣｌ２电池可高速率放电，在５０ｍＡ．ｃｍ＾－２的条件下，达到了１７．５ｍＡｈ．ｃｍ＾－２。     

阴离子对水的羟基伸缩振动拉曼光谱的影响

通过比较纯水、NaX(X=F, Cl, Br, I)、Na2S、NaOH、NaNO3、Na2CO3、Na2SO4溶液的羟基伸缩振动拉曼光谱, 发现所研究的阴离子对水的结构都有破坏作用. 通过比较阴离子对水的羟基伸缩振动拉曼光谱的影响, 可将所研究的阴离子分为两类, 一类阴离子有F−、OH−、S2−、CO32−, 另一类阴离子有Cl−、Br−、I−、NO3−和SO42−. 它们的主要区别在于对羟基伸缩振动拉曼光谱3600 cm−1、2900−3100 cm−1处影响不同, 产生这些区别的原因在于阴离子与水分子之间氢键的强弱. 阴离子对水的羟基伸缩振动拉曼光谱的影响因素有离子半径、离子电荷和离子结构, 它们的影响程度为离子结构>离子电荷>离子半径.     

Observation of the first hydration layer of isolated cations and anions through the FTIR-ATR difference spectra

The attenuated total reflectance-Fourier transform infrared (ATR-FTIR) difference spectra of the dilute aqueous (NH4)2SO4, Na2SO4, MgSO4, ZnSO4, NaClO4, and Mg(ClO4)2 solutions by pure water were obtained at various concentrations. In the difference spectra of aqueous (NH4)2SO4 solutions, a peak at approximately 3039 cm(-1), two shoulders at approximately 3155 and approximately 2894 cm(-1), and a peak at approximately 1445 cm(-1) were ascribed to N-H stretching and bending vibrations, respectively. A small negative peak was resolved at approximately 3660 cm(-1) in the difference spectra of (NH4)2SO4, which is the sole contribution of SO4(2-) either in the O-H stretching or in the O-H bending region. The positive peaks of the difference spectra in the O-H stretching region for Na2SO4, MgSO4, and ZnSO4 systems, which constantly appeared at approximately 3423, approximately 3136, and approximately 3103 cm(-1) respectively, were suggested to be the contribution of the interactions between metal cations (Na+, Mg2+, and Zn2+) and water molecules, especially from the first hydrated layer of the cations. In the region of 800-1200 cm(-1), the normally infrared-prohibited nu1 (SO4(2-)) band was observed as a weak peak at approximately 981 cm(-1) even at very dilute concentrations (0.10 mol dm(-3)) due to the disturbance of the water molecules hydrated with SO4(2-), even though such a feature may increasingly result from associated ions with increasing concentration. The spectra of the water molecules directly influenced by ClO4-, i.e., mostly the first layer of hydrated water, in NaClO4 and Mg(ClO4)2 solutions were obtained by subtracting the corresponding spectra of the same metal sulfate solutions at the same concentrations from the perchlorate solutions. A positive peak at approximately 3583 +/- 6 cm(-1) and a negative peak at approximately 3184 +/- 25 cm(-1) were obtained as the result of the subtraction. The positive peak was attributed to the water molecules weakly hydrogen-bonded with ClO4-, while the negative one to the reduction of water molecules with fully hydrogen-bonded five-molecule tetrahedral nearest neighbor structure on the introduction of ClO4-.     

IR, 1H NMR, mass, XRD and TGA/DTA investigations on the ciprofloxacin/iodine charge-transfer complex

Raman and infrared spectra of two polymorphous minerals with the chemical formula Fe3+(SO4)(OH)·2H2O, monoclinic butlerite and orthorhombic parabutlerite, are studied and the spectra assigned. Observed bands are attributed to the (SO4)2- stretching and bending vibrations, hydrogen bonded water molecules, stretching and bending vibrations of hydroxyl ions, water librational modes, Fe-O and Fe-OH stretching vibrations, Fe-OH bending vibrations and lattice vibrations. The O-H?O hydrogen bond lengths in the structures of both minerals are calculated from the wavenumbers of the stretching vibrations. One symmetrically distinct (SO4)2- unit in the structure of butlerite and two symmetrically distinct (SO4)2- units in the structure of parabutlerite are inferred from the Raman and infrared spectra. This conclusion agrees with the published crystal structures of both mineral phases.     

A Raman spectroscopic study of the uranyl phosphate mineral bergenite

Raman spectroscopy at 298 and 77 K of bergenite has been used to characterise this uranyl phosphate mineral. Bands at 995, 971 and 961 cm-1 (298 K) and 1006, 996, 971, 960 and 948 cm-1 (77K) are assigned to the nu1(PO4)3- symmetric stretching vibration. Three bands at 1059, 1107 and 1152 cm-1 (298 K) and 1061, 1114 and 1164 cm-1 (77 K) are attributed to the nu3(PO4)3- antisymmetric stretching vibrations. Two bands at 810 and 798 cm-1 (298 K) and 812 and 800 cm-1 (77 K) are attributed to the nu1 symmetric stretching vibration of the (UO2)2+ units. Bands at 860 cm-1 (298 K) and 866 cm-1 (77 K) are assigned to the nu3 antisymmetric stretching vibrations of the (UO2)2+ units. UO bond lengths in uranyls, calculated using the wavenumbers of the nu1 and nu3(UO2)2+ vibrations with empirical relations by Bartlett and Cooney, are in agreement with the X-ray single crystal structure data. Bands at (444, 432, 408 cm-1) (298 K), and (446, 434, 410 and 393 cm-1) (77 K) are assigned to the split doubly degenerate nu2(PO4)3- in-plane bending vibrations. The band at 547 cm-1 (298 K) and 549 cm-1 (77 K) are attributed to the nu4(PO4)3- out-of-plane bending vibrations. Raman bands at 3607, 3459, 3295 and 2944 cm-1 are attributed to water stretching vibrations and enable the calculation of hydrogen bond distances of >3.2, 2.847, 2.740 and 2.637 A. These bands prove the presence of structurally nonequivalent hydrogen bonded water molecules in the structure of bergenite.     

FTIR spectroscopic investigations of supersaturated NaClO4 aerosols

Supersaturated NaClO4 aerosols have been studied using a Fourier transform infrared (FTIR) spectrometer coupled with an aerosol flow tube (AFT). Compared with previous Raman results, the water O-H stretching envelope in the supersaturated solutions of NaClO4 aerosols was more structured in response to changing RH, revealing at the same time the existence of water monomers weakly hydrogen-bonded with ClO4- at extremely high concentrations. Due to enhanced ion interactions in the supersaturated solutions of NaClO4 aerosols, the formation of contact ion pairs (CIPs) could be observed without component decomposition for the nondegenerate nu1 band of ClO4-, and the degenerate nu3 band of ClO4- was successfully related to the formation of CIPs in NaClO4 solutions. Based on these observations, a new mechanism featured by the attack of ClO4- upon hydrated Na+ for CIPs formation in the supersaturated solutions of NaClO4 aerosols was further proposed. The anhydrous NaClO4, characterized by the upper limit deliquescence relative humidity (DRH) of approximately 43% and the disappearance of the nu1 band of ClO4- in the infrared spectra, was observed to form on the silicon windows at low RHs.     

NIR spectroscopy of jarosites

Near-infrared (NIR) spectroscopy has been used to analyse a suite of synthesised jarosites of formula Mn(Fe3+)6(SO4)4(OH)12 where M is K, Na, Ag, Pb, NH4+ and H3O+. Whilst the spectra of the jarosites show a common pattern, differences in the spectra are observed which enable the minerals to be distinguished. The NIR bands in the 6300-7000 cm-1 region are attributed to the first fundamental overtone of the infrared and Raman hydroxyl stretching vibrations. The NIR spectrum of the ammonium-jarosite shows additional bands at 6460 and 6143 cm-1, attributed to the first fundamental overtones of NH stretching vibrations. A set of bands are observed in the 4700-5500 cm-1 region which are assigned to combination bands of the hydroxyl stretching and deformation vibrations. The ammonium-jarosite shows additional bands at 4730 and 4621 cm-1, attributed to the combination of NH stretching and bending vibrations. NIR spectroscopy has the ability to distinguish between the jarosite minerals even when the formula of the minerals is closely related. The NIR spectroscopic technique has great potential as a mineral exploratory tool on planets and in particular Mars.     

In search of covalently bound tetra- and penta-oxygen species: a photoelectron spectroscopic and Ab initio investigation of MO4- and MO5- (M = Li,Na, K,Cs)

Although neutral and ionic O4(0/-/+) species have been observed experimentally and considered for energetic materials, O4(2-) and O5(2-) dianions have not yet been explored. O4(2-) is valent isoelectronic to the well-known ClO3- and SO3(2-) anions, and O5(2-) is valent isoelectronic to ClO4- and SO4(2-). All are stable, common anions in solutions and inorganic salts. In this article, we explore the possibility of making covalently bound O4(2-) and O5(2-) species stabilized in the forms of M+O4(2-) and M+O5(2-) (M = Li, Na, K, Cs) in the gas phase. Laser vaporization experiments using M-containing targets and an O2-seeded carrier gas yielded very intense mass peaks corresponding to MO4- and MO5-. To elucidate the structure and bonding of the newly observed MO4- and MO5- species, we measured their photoelectron spectra and then compared them with ab initio calculations and the spectra of ClO3-, Na+SO3(2-), ClO4-, and Na+SO4(2-). Careful analyses of the experimental and ab initio results showed, however, that the observed species are of the forms, O2-M+O2- and O2-M+O3-. The more interesting M+O4(2-) and M+O5(2-) species were found to be higher-energy isomers, but they are true minima on the potential energy surfaces, which suggests that it might be possible to synthesize bulk materials containing covalently bound tetra- and pentatomic oxygen building blocks.     

Vibrational study and spectra-structure correlations in ammonium saccharinate: comparison with the alkali saccharinates

The FT IR spectra, at temperatures from liquid-nitrogen boiling (LNT) up to room temperature (RT), as well as the RT Raman solid-state spectra of protonated and deuterated ammonium saccharinate and of a series of alkali (Na, K, Rb, Cs) saccharinates are studied. The spectral assignments are aided with ab initio calculations on the free saccharinato anion at the HF/6-31 + + G(d,p) level. Attention is paid to the ND, CO and SO2 stretching regions. Correlation splitting is believed to be responsible for the presence of a v(CO) doublet. The averaged v(CO) frequency in (purely ionic) ammonium saccharinate is found to be the lowest in the so far studied saccharinates, along with the assumptions that the v(CO) frequency (or the corresponding averaged value) can have predictive value for the type of the metal-to-saccharinato ligand/ion bonding. The appreciably higher contribution of the dominating internal coordinate in the corresponding normal vibration in case of v(as)(SO2) than in v(s)(SO2) makes it suitable for spectra-structure correlations. Contrary to RT, even though no phase transitions were observed in the studied temperature range, some polycentered character is prescribed to the hydrogen bonds in which the ammonium ions of effective symmetry C8 participate at LNT. Certain structural predictions about the saccharinates of K, Rb and Cs are made.     

氮气笼型水合物的激光拉曼光谱

在253K和16MPa的压力下,于实验室内合成了氮气水合物,用显微共焦拉曼光谱对其N-N和O-H键伸缩振动的光谱特征进行了研究．结果表明,氮气水合物中的N-N和O—H键的拉曼峰分别为2322．4和3092．1cm^-1,与天然的空气水合物中的数据十分接近．另外,还测定了液氮和溶解于水中的氮分子中N—N键的拉曼峰值,分别为2326．6和2325．0cm^-1．氮气笼型水合物分解的拉曼谱图表明,氮分子同时进入水合物的大笼和小笼中,但由于氮分子在大、小笼中的环境氛围十分接近,其拉曼位移相差不大,故拉曼谱图只能显示N—N键伸缩振动一个峰．     

Vibrational spectroscopy of selected minerals of the rosasite group

Minerals in the rosasite group namely rosasite, glaucosphaerite, kolwezite, mcguinnessite have been studied by a combination of infrared and Raman spectroscopy. The spectral patterns for the minerals rosasite, glaucosphaerite, kolwezite and mcguinnessite are similar to that of malachite implying the molecular structure is similar to malachite. A comparison is made with the spectrum of malachite. The rosasite mineral group is characterised by two OH stretching vibrations at approximately 3401 and 3311 cm-1. Two intense bands observed at approximately 1096 and 1046 cm-1 are assigned to nu1(CO3)2- symmetric stretching vibration and the delta OH deformation mode. Multiple bands are found in the 800-900 and 650-750 cm-1 regions attributed to the nu2 and nu4 bending modes confirming the symmetry reduction of the carbonate anion in the rosasite mineral group as C2v or Cs. A band at approximately 560 cm-1 is assigned to a CuO stretching mode.