Ti+(CO2)2Ar和Ti+(CO2)n(n=3-7)络合物离子的红外光解离光谱 (cited: 1)

利用脉冲激光溅射-超声分子束载带方法制备了气相Ti⁺(CO₂)₂Ar和Ti⁺(CO₂)_n(n=3-7)络合物离子．采用红外光解离光谱研究了这些选定的质量离子的振动光谱． 对于每一种络合物离子, 在CO伸缩振动频率范围都观察到了振动峰,表明这些离子具有插入的OTi⁺CO(CO₂)_n-1结构． 对于n≦5的OTi⁺CO(CO₂)_n-1离子,其CO振动和CO₂的反对称伸缩振动频率都比自由的CO和CO₂的频率要高,表明CO和CO₂配体与中心金属离子之间主要是静电相互作用．实验结果还表明TiO⁺可以直接络合五个配体(1个CO和4个CO₂分子)．对于n=2络合物体系,除了插入的OTi⁺CO(CO₂)结构以外,还观察到了具有弯曲结构的OCO-Ti⁺-OCO异构体的存在     

[Au25(SR)18]-团簇的相干振动动力学研究

利用飞秒时间分辨光谱,可观测叠加在电子态动力学上的相干振动动力学. 从金团簇的相干振动中,不仅能提取电子与振动的耦合信息,也能得到力学性质和电子结构,进而有望实现微小质量探测等应用. 本文利用飞秒时间分辨的瞬态吸收探测了[Au₂₅(SR)₁₈]^-团簇的相干振动动力学,通过对相干振动的频率、相位、波长分布的详细分析进一步揭示了其来源. 在[Au₂₅(SR)₁₈]^-团簇的飞秒瞬态吸收动力学中可以观测到频率为40 cm^-1和80 cm^-1的两种振动,均来源于团簇中心Au₁₃核的振动. 通过对相干振动的相位分析发现频率为80 cm^-1的振动来自于对电子态之间吸收频率的调制,而频率为40 cm^-1的振动来源于对电子态之间吸收强度的调制. 同时,研究发现[Au₂₅(SR)₁₈]^-团簇相干振动的频率对其表面配体不敏感,该振动是来源于Au₁₃核的本征性质.     

Resonance Raman Study of Aggregated Meso-tetra(4-pyridinium) porphyrin Diacid

研究了近激子吸收带激发下四-(4-吡啶基)卟啉二酸(H₈TPyP⁶⁺)聚集体的共振拉曼光谱．测量了H₈TPyP⁶⁺单体和聚集体的紫外可见吸收谱和共振光散射光谱．在氘代位移的基础上结合相关体系振动光谱研究,对测得的H₈TPyP⁶⁺)单体和聚集体的拉曼谱带进行了指认．聚集体的形成导致H₈TPyP⁶⁺的卟啉环CC/CN面内伸缩振动向低波数方向位移2～6 cm^-1,而卟啉环鞍形面外振动带向高波数方向位移12cm^-1．基于拉曼谱带的强度和频率变化分析了聚集引起的H₈TPyP⁶⁺分子内结构变化和分子间氢键作用     

OCS经由F 31Π里德堡态生成CO(X1Σ+)+S(1D2)产物的波长相关性光解离

本文利用时间切片离子速度成像技术在134∽140 nm波段研究了OCS分子经由F 3¹Π里德堡态的真空紫外光解离动力学. 在选取的5个分别对应OCS(F 3¹Π, v₁=0∽4)的伸缩振动激发的光解波长，实验测得了来自CO(X¹Σ⁺)+S(¹D₂)产物通道的SS(¹D₂))实验影像，并获得了总平动能谱和CO(X¹Σ⁺, v)共生产物的振动布居及角分布. 结果分析表明OCS分子解离生成CO(X¹Σ⁺)+S(¹D₂)产物的过程经历了上态F 3¹Π 与C_?v和C_s构型的下电子态间非绝热耦合过程. 实验结果显示了很强的波长相关性：OCS (F 3¹Π, v₁)的较低转动激发态(v₁=0∽2)和较高转动激发态(v₁=3, 4)的CO(X¹Σ⁺)产物的振动布居和角分布具有显著差异，表明该解离过程中具有不同的解离机理. 本结果提供了振动耦合可能对真空紫外光解离动力学产生关键作用的相关证据.     

采用二维坐标和变分方法计算磷烷阳离子的伞型振动

提出一个新的二维变分方法计算PH₃⁺(X²A₂")的对称伸缩振动(v1)和伞形振动(v2). 因为采用了对称化的笛卡尔坐标,所以动能项变得简单,同时伞形振动模式也能得到很好的反映. 相比采用经常使用的一维模型计算伞形振动,这个二维模型不需要约化质量的假设,同时也考虑了v1和v2振动模式之间的相互作用. 用二维模型对PH₃⁺首次进行了计算, 前七个能级的理论值和实验值的平均相对误差小于3 cm^{-1. 用相同的方法也计算了NH₃,结果没有PH₃+理想,说明这个方法有一定的局限性.}     

晶体电光和非线性光学效应的离子基团理论(Ⅱ)——利用(IO3)-1离子基团的分子轨道计算α-LiIO3晶体的倍频系数

本文对碘酸盐晶体的倍频效应提出了一个(IO₃)^-1离子基团模型,并用(IO₃)^-1离子基团的分子轨道计算了α-LiIO₃的倍频系数,计算值和实验值符合得很好。由此得出以下结论:碘酸盐晶体的倍频效应主要由(IO₃)^-1离子基团和它的共价键轨道所决定。而在(IO₃)^-1离子基团中,对倍频效应作出主要贡献的是碘的孤对电子轨道和氧的|2σ>,|2P_y>轨道。     

时间切片离子速度成像技术关于MgO在193 nm的光解反应动力学研究

本文利用时间切片离子速度成像技术对MgO分子在193 nm下的光解反应动力学进行了研究. 实验通过产物Mg的速度和角度分布分析,发现了三个光解反应路径. 路径一为MgO(X¹Σ⁺)态分子吸收一个光子到MgO(G¹π) 态,由于G¹π, 3³π和1⁵π态之间的自旋轨道耦合作用,反应沿着1⁵π的势能面解离生成产物Mg(³P_u)+O(³P_g). 路径二、三分别为MgO(A¹π)态分子吸收一个光子到MgO(G¹π)态和MgO(4¹π) 态,进而解离生成产物Mg(³P_u)+O(³P_g)和Mg(¹S_g)+O(¹S_g). 光解离路径的各向异性参数与振动能级的寿命以及转动和振动自旋轨道态的耦合有关. 从总动能分析得到D₀(Mg-O)=21645±50 cm^-1.     

He-H2S复合物的六维从头算势能面和束缚态

采用[CCSD(T)]-F12a/aug-cc-pVTZ方法，同时在基组中引入中心键函数(3s3p2d1f1g)构建了He-H$_2$S复合物的高精度六维势能面. 除分子间振动坐标，同时考虑了H₂S分子内的v₁对称伸缩振动Q₁正则模、v₂弯曲振动Q₂正则模和v₃反对称伸缩振动Q₃正则模三种振动模式. 将计算得到的六维势能面在Q₁，Q₂和Q₃方向上分别做积分得到H₂S单体分别处于振动基态、v和v₃激发态下的He-H₂S的三个振动平均势能面. 计算结果表明，每个平均势能面都有一个T形全局极小值、一个平面局部极小值、两个平面内鞍点和一个平面外鞍点. 全局极小值的几何构型位于R=3.46 ?，θ=109.9°和φ=0.0°，势阱深度为35.301 ^-1. 在径向部分采用离散变量表象法和角度部分采用有限基组表象法并结合Lanczos循环算法计算了He-H₂S的振转能级和束缚态. 计算发现He-(para-H₂S)在H₂S的v₂和v₃区域的带心位移分别为0.025 cm^-1和0.031 cm^-1，而He-(ortho-H₂S)的带心位移分别为0.041 cm^-1和0.060 cm^-1，都表现为蓝移.     

尺寸和微结构效应对软锰矿红外光谱的影响

合成了纳米纤维状的软锰矿β-MnO₂,其研磨后粒子形貌由纳米纤维转变为纳米粒子,相结构并没有转变．纳米纤维状粒子中心锰离子局域环境有轻微改变．当粒子形貌从长纳米纤维变到短纳米纤维再到纳米粒子时,傅里叶转换红外光谱A_2u频率逐渐从514 cm^-1到574 cm^-1再到617 cm^-1．研究发现依据功能团分析无法确定额外的振动波段来源于不同尺寸和形状粒子的A_2u．通过X射线衍射的Rietveld精修和红外光谱,认为两种MnO₆的八面体构型,如4长+2短,4短+2长,在由不同路线合成的软锰矿中都会存在．微结构对软锰矿傅里叶转换红外光谱最大振动频率的影响是显著的．在红外和远红外区域的四个振动波段都做了分类.     

CO2对790 nm附近水线的压力加宽和位移

采用高灵敏的激光光腔衰荡光谱技术研究了CO₂对¹⁶O水分子v²+3v³振动带跃迁线的压力诱导效应. 为了抑制水的自碰撞效应,水的压力在实验中低于0.5 Torr. 基于铷原子吸收线和超稳法布里-珀罗标准确定了跃迁谱线高达10^-5 cm^-1精度的绝对频率. 采用软碰撞模型对吸收线进行模拟,获得了对应的线形参数.     

Infrared spectra of catalysts and adsorbed molecules

The infrared absorption spectra of water adsorbed on Al₂O₃ and NiO-Al₂O₃ catalysts have been studied in the range 4000–1200 cm^–1. For all the catalysts, broad bands are observed at 3400 and 1640 cm^–1, characteristic of the stretching and bending vibrations of the OH groups in liquid water. The bands observed in the spectrum of alumina prepared from suspension in isopropyl alcohol are produced by water molecules and isopropyl alcohol molecules absorbed on the catalyst surface. The influence of treatment with heavy water and thermal treatment on the position of the infrared absorption bands in the spectrum of alumina is discussed.     

FIR absorption studies of neodymium sulphate by FTIR at low temperatures

Far infrared (FIR) spectra of neodymium sulphate octahydrate and its deuterated analogue crystals were studied in the 400-50 cm⁻¹ region. Measurements were carried out at ambient and low temperatures. A quasi structure model was used to identify the absorption bands and for the assignment of the spectral information. Bands pertaining to librational modes hindered rotations, and translation modes arising from different molecular groups, ions and bondings were obtained. Low temperature measurements were quite useful for revealing the removal of degeneracy, sharpening of the bands, shifting of the frequency and in the identification of weak bands. Deuteration of the crystals was used to identify the bands pertaining to water molecules present in the lattice and in the coordinated water. The isotopic shift arising from the corresponding bands of H₂O and D₂O was found to be 1.053 at a temperature of 290 K and 1.043 at 60 K.     

Raman and IR spectra of K4Nb6O17and K4Nb6O17·3H2O single crystals

Polarised Raman and IR spectra of K₄Nb₆O₁₇ and K₄Nb₆O₁₇· 3H₂O single crystals were measured. The obtained spectra are discussed using the factor group approach for the orthorhombic P2₁nb space group and assignment of bands to the respective motions of atoms is proposed. In particular, we have shown that the bands above 770 cm⁻¹ can be attributed to the stretching modes of short niobium–oxygen bonds, which are present in this material due to the pronounced layered structure, whereas the potassium atoms contribute to the bands observed below 180 cm⁻¹. Our studies have revealed that intercalation of water molecules leads to shifts, broadening and changes in intensity of some bands. These changes have been attributed to slight changes in the bond lengths and angles, interactions of the water molecules with K atoms and structural disorder introduced by the intercalated water molecules. However, the main structural framework was preserved. Copyright © 2010 John Wiley & Sons, Ltd.     

Raman spectroscopic study of the uranyl carbonate mineral zellerite

Raman and infrared spectra of the uranyl mineral zellerite, Ca[(UO₂)(CO₃)₂(H₂O)₂]·3H₂O, were measured and tentatively interpreted. U O bond in uranyl and O H···O hydrogen bonds were calculated from the vibrational spectra. The presence of structurally nonequivalent water molecules in the crystal structure of zellerite was inferred. A proposed chemical formula of zellerite is supported. Raman bands at 3514, 3375 and 2945 cm⁻¹and broad infrared bands at 3513, 3396 and 3326 cm⁻¹ are related to the ν OH stretching vibrations of hydrogen‐bonded water molecules. Observed wavenumbers of these vibrations prove that in fact hydrogen bonds participate in the crystal structure of zellerite. The presence of two bands at 1618 and 1681 cm⁻¹ proves structurally distinct and nonequivalent water molecules in the crystal structure of zellerite. Copyright © 2008 John Wiley & Sons, Ltd.     

Fourier Transform Vibrational Spectra of Magnesium Hydrogenphosphate Trihydrate. I. The O-H Stretching Region∗

Abstract

The Fourier transform (FT) infrared and Raman spectra of newberyite, MgHPH₄ - 3H₂O are studied in the region where the stretching vibrations of the water molecules (protiated and deuterated) and the O-H/O-D stretches of the hydrogenphosphate anions are expected to appear. The O-H stretching vibrations give rise to a complex feature known as the A,B,C trio. Since neither of the maxima found below 3000 cm^?1 represents a true band arising from a given fundamental, it is pointless to correlate their frequencies with the observed O…O distances. In the water stretching region, the two bands with highest frequencies undoubtedly correspond to the anti symmetric and symmetric stretch of one type of the water molecules. The stretching vibrations of one of the remaining two types of H₂O molecules are clearly uncoupled and the O-H oscillator involved in the weaker hydrogen bond is responsible for a band at 3376 cm^?1 whereas the rest of the water stretchings are apparently overlapped yielding the complex band below 3320 cm^?1. Thus the situation is again complicated and the correlations between the frequencies and the O_w…O distances are inappropriate. The two bands at highest frequencies (3522 and 3483 cm^?1 at RT) exhibit a positive temperature coefficient.

     

Fourier transform infrared spectral study of N,N′-dimethylformamide-water-rhodamine 6G mixture

Infrared absorption spectra of N,N′-dimethyl formamide in the absence and presence of water, rhodamine 6G and water–rhodamine 6G mixture are reported. Assignment of observed bands has been made on the basis of density functional theory calculations and available assignments in the literature. Certain bands show changes in their positions and intensities when water is added to N,N′-dimethylformamide. This is due to hydrogen bonding interaction between these molecules. Similar changes are also observed for dimethylformamide and Rh6G mixture to a lesser extent. The presence of Rh6G in a dimethylformamide–water mixture reverses these spectral changes due to preferential solvation of Cl^? by water molecules. Solvation reduces or nullifies the hydrogen bonding between dimethylformamide and water in the mixture.     

Strengths of H2O lines in the 5000–5750 cm-1 region

Measurements of the strengths of 311 lines of water vapor have been made with high resolution in the region 5000–5750 cm^-1. The strength data of lines in the (011) and (110) bands are analyzed to determine the band strengths and the coefficients of the F factors. The band strengths of the (011) and (110) bands were found to be 20.65±0.21 and 0.384±0.015 cm^-2atm^-1 at 296 K, respectively. Many of the measured strengths in the (011) and (110) bands differ from the calculated values because of strong Coriolis interactions. Also included in the present work are measurements of strengths of four lines in the (030) band and 36 lines in the “hot” band (021)-(010).     

Infrared Spectra Interpretations of Clay-Adsorbed Water in Relation to the “Anomalous” Water Controversy

Abstract

The nature of surface adsorbed water has been the subject of countless investigations. Much of the discussion has centered around the degree and strength of H-bonding to surface groups and between adjacent water molecules.^1,2 Water condensed into glass or quartz capillaries sometimes has unusual properties. This unusual water has been referred to as “orthowater,”³ “anomalous water,”^4,5,6 and “polywater”^7,8 and was thought by some to be polymers of water formed by specific surface catalysis.^1–3 Several possible structures of “polywater” have been suggested which require formation of symmetrical or very strong H-bonds between water molecules.^4,6,7 Infrared spectra of polywater have been presented^7,8 and the strongest absorption band which appeared at 1595 cm^?1 was assigned to the symmetric O-H-O bond. However, more recent investigations suggest that the observed polywater bands may actually be SO₄ ^2-, -COOH^?, or HCO₃ ^? bands, impurities collected by surface diffusion,⁹ or bands of a HNO₃ solution formed by corona discharge.¹⁰ Other observers^11,12 suggest that polywater may be a hydrosol formed by surface contaminates.     

Laser-induced fluorescence spectroscopy of FeS in the visible region

The laser-induced fluorescence excitation spectra of jet-cooled FeS molecules have been recorded in the energy range of 18 900-21 600 cm⁻¹, in which four parallel and one perpendicular transitions were identified for the first time. Spectroscopic constants of the observed excited states of FeS were determined by analyzing their rotationally resolved spectra. In addition, the lifetimes of most observed bands were also measured.     

Raman spectroscopy of hydrogen‐arsenate group (AsO3OH) in solid‐state compounds: copper mineral phase geminite Cu(AsO3OH)·H2O from different geological environments

The participation of hydrogen‐arsenate group (AsO₃OH)²⁻ in solid‐state compounds may serve as a model example for explaining and clarifying the behaviour of As and other elements during weathering processes in natural environment. The mineral geminite, a hydrated hydrogen‐arsenate mineral of ideal formula Cu(AsO₃OH)·H₂O, has been studied by Raman and infrared spectroscopies. Two samples of geminite of different origin were investigated and the spectra proved quite similar. In the Raman spectra of geminite, six bands are observed at 741, 812, 836, 851, 859 and 885 cm⁻¹ (Salsigne, France), and 743, 813, 843, 853, 871 and 885 cm⁻¹ (Jáchymov, Czech Republic). The band at 851/853 cm⁻¹ is assigned to the ν₁ (AsO₃OH)²⁻ symmetric stretching mode; the other bands are assigned to the ν₃ (AsO₃OH)²⁻ split triply degenerate antisymmetric stretching mode. Raman bands at 309, 333, 345 and 364/310, 333 and 345 cm⁻¹ are attributed to the ν₂ (AsO₃OH)²⁻ bending mode, and a set of higher wavenumber bands (in the range 400–500 cm⁻¹) is assigned to the ν₄ (AsO₃OH)²⁻ split triply degenerate bending mode. A very complex set of overlapping bands is observed in both the Raman and infrared spectra. Raman bands are observed at 2289, 2433, 2737, 2855, 3235, 3377, 3449 and 3521/2288, 2438, 2814, 3152, 3314, 3448 and 3521 cm⁻¹. Two Raman bands at 2289 and 2433/2288 and 2438 cm⁻¹ are ascribed to the strong hydrogen bonded water molecules. The Raman bands at 3235, 3305 and 3377/3152 and 3314 cm⁻¹ may be assigned to the ν OH stretching vibrations of water molecules. Two bands at 3449 and 3521/3448 and 3521 cm⁻¹ are assigned to the OH stretching vibrations of the (AsO₃OH)²⁻ units. The lengths of the O H···O hydrogen bonds vary in the range 2.60–2.94 Å (Raman) and 2.61–3.07 Å (infrared). Two Raman and infrared bands in the region of the bending vibrations of the water molecules prove that structurally non‐equivalent water molecules are present in the crystal structure of geminite. Copyright © 2009 John Wiley & Sons, Ltd.