磁几何阻挫材料羟基氯化钴的中红外光谱特征

使用3种光谱仪测量了磁几何阻挫材料羟基氯化钴Co₂(OH)₃Cl的中红外(4000—400 cm^-1)吸收光谱,筛选出确信为Co₂(OH)₃Cl的本征吸收峰数据,结合已知的晶体结构参数,指认了官能团和指纹区相应谱峰的来源.在指认中着重探讨了羟基伸缩振动基频模vOH的具体实验数据,根据固体中氢键的特点,以Co₃—O平均距离为基准,推算了本样品 关键词： 红外光谱 几何阻挫 羟基氯化钴 三聚氢键     

Microstructured hydroxyl environments and Raman spectroscopy in selected basic transition-metal halides

Raman vibrational spectra of the selected basic (hydroxyl OH and deuteroxyl OD) transition-metal halides, geometrically frustrated material series α-, β-, γ-Cu₂(OH)₃Cl, α-Cu₂(OH)₃Br, β-Ni₂(OH)₃Cl, β-Co₂(OH)₃Cl, β-Co₂(OH)₃Br, γ-Cu₂(OD)₃Cl, and β-Co₂(OD)₃Cl are measured at room temperature and analysed to investigate the relationship between the microstructured OH environments and their respective Raman spectra. Among these selected samples, the last two are used to determine the OH stretching vibration region (3600 cm^-1—3300 cm^-1) and OH bending vibration region (1000 cm^-1—600 cm^-1) of OH systems in the spectra. Through the comparative analysis of the distances d(metal—O), d(O—halogen), and d(OH), the strong metal—O interaction and trimeric hydrogen bond (C_3v, C_s or C₁ symmetry) are found in every material, but both determine simultaneously an ultimate d(OH), and therefore an OH stretching vibration frequency. According to the approximately linear relationship between the OH stretching vibration frequency and d(OH), some unavailable d(OH) are guessed and some doubtful d(OH) are suggested to be corrected. In addition, it is demonstrated in brief that the OH bending vibration frequency is also of importance to check the more detailed crystal microstructure relating to the OH group.     

磁几何阻挫材料天然绿盐铜矿的中红外和拉曼光谱分析

在室温情况下,利用FTIR光谱仪测得了天然磁几何阻挫材料绿盐铜矿(Atacamite,β-Cu2 (OH)3Cl)的中红外光谱4 000～400 cm-1,同时还通过激光显微拉曼光谱仪获得了它的拉曼光谱4 000～95 cm-1.结合它的晶体结构参数,确认了官能团区4 000～2 500～1 000 cm-1和指纹区1...     

Raman and mid-infrared spectroscopic study of the phase transitions in octafluoronaphthalene at elevated pressures

Raman and mid-infrared spectra of C₁₀F₈ have been obtained under hydrostatic pressures up to 17 kbar in a diamond anvil cell. The C₁₀F₈ I–II phase change, previously observed by neutron diffraction at about 0.8 kbar, has been confirmed. No evidence was found to support the existence of a furtt ier phase change between 4 and 6 kbar indicated by the neutron work, although this is certainly not precluded as the extra spectral features expected in this case are extremely small. The mode Grüneisen parameters, γ_i, allow a clear distinction between internal and external molecular modes, and scale roughly in accord with Zallen's relation γ_i$\text{\$}\text{?}$v_i^?2.     

Mössbauer spectroscopic study of synthetic lipscombite and barbosalite at room temperature

Barbosalite and lipscombite hydroxyphosphates have been prepared and characterized by Mössbauer spectroscopy. These phases have been shown to be constituted of chains of Fe—oxygen octahedra sharing faces. The principal difference in the arrangement of the ions in these structures is the organization of the octahedra in the chains. In barbosalite, the chains are composed only of trimeric groups (Fe₃O₁₂) separated by a vacant octahedral site, while lipscombite chains are composed of groups of (2n + 1) iron cations,n varying from 0 to 5 or 6. The relative abundance of the different groups was calculated from published X-ray diffraction data and used to attribute the three ferric and the two ferrous doublets observed in the Mössbauer spectrum of lipscombite. This attribution is confirmed by the comparison with the results obtained on barbosalite.     

Neutron in-beam Mössbauer spectroscopic study of iron disulfide at room temperature

An in-beam emission Mössbauer spectrum of ⁵⁷Fe arising from the ⁵⁶Fe(n, γ) ⁵⁷Fe reaction in iron disulfide at room temperature was measured with a parallel plate avalanche counter. It was clearly observed that the nuclear reaction and the following process lead to the production of a new chemical species of iron different from the parent compound.     

A neutron diffraction study of ferroelectric PbHAsO4 at room temperature

A single-crystal neutron-diffraction structural study of PbHAsO₄ in its ferroelectric phase at room temperature (24°C) is presented as part of an investigation of a family of monetites. The crystal structure of PbHAsO₄, and its phase transition mechanism are discussed. Comparison of the crystal structures of PbHPO₄ and PbHAsO₄ reveals that these two ferroelectrics are isomorphous. The role of protons in structural phase transition of PbHAsO₄ is also discussed.     

Raman spectroscopic study of the uranyl oxyhydroxide hydrates: becquerelite,billietite, curite,schoepite and vandendriesscheite

Raman and infrared spectra of five uranyl oxyhydroxide hydrates, becquerelite, billietite, curite, schoepite and vandendriesscheite, are reported. The observed bands are attributed to the (UO₂)²⁺ stretching and bending vibrations, U OH bending vibrations and H₂O and (OH)⁻ stretching, bending and libration modes. The U O bond lengths in uranyls and the O H···O bond lengths are calculated from the wavenumbers assigned to the stretching vibrations. They are close to the values inferred and/or predicted from the X‐ray single‐crystal structure. The complex hydrogen‐bonding network arrangement was proved in the structures of all the minerals studied. This hydrogen bonding contributes to the stability of these uranyl minerals. Copyright © 2006 John Wiley & Sons, Ltd. John Wiley & Sons, Ltd.     

Raman scattering and photoluminescence of zinc telluride nanopowders at room temperature

Zinc telluride (ZnTe) powders were synthesized in sodium hydroxide solution by the hydrothermal method under different conditions, in which zinc and tellurium powders were used as precursors. Their structures were characterized by X-ray diffractometer, X-ray photoelectron spectroscopy, transmission electron microscopy, and micro-Raman spectrometer. The results indicate that the powders are composed of ZnTe nanocrystals with zincblende structure and contain some impurities, and the average sizes of ZnTe nanocrystals are about 67, 92, and 112 nm when they were grown at 120 °C for 1, 2, and 6 h, respectively. The Raman spectra show three peaks centered at about 205, 410, and 616 cm⁻¹, which are attributed to the longitudinal optical phonon vibration modes of ZnTe. The photoluminescence (PL) of ZnTe nanopowders were also investigated at room temperature and the PL spectra show three emission peaks at about 555, 578, and 701 nm, which are related to the complex defects and isolelectronic oxygen trap.     

Raman spectra of forsterite and fayalite at high pressures and room temperature

Abstract

Raman spectra of the two pure end-members of olivine (forsterite and fayalite) were studied at high pressures and room temperature in a diamond-anvil cell using both single-crystals and polycrystalline samples in pressure mediums of either an ethanol-methanol mixture or H₂O. Variations with pressure were studied up to 170kbar for fayalite and to 300kbar for forsterite. Two intensive Raman bands of fayalite were definitely observable at high pressures, but only one of them can be reliably determined. Both have a linear variation within experimental uncertainty. Because of interference from the high spectral background, we found that nearly all the weak bands of forsterite could not be reliably determined at high pressures. However, the pressure variations of all bands of forsterite which can be reliably determined are non-linear. The rates of frequency change for the intense bands of forsterite determined in the present experiment are consistent with those of natural forsterites determined by Besson et al. ¹ and Gillet et al. ², but are in a slight discordance with those reported by Chopelas³. Furthermore, there is no evidence for the olivine ? spinel phase transition occurring at room temperature.     

还原温度对氧化石墨烯结构及室温下H_2敏感性能的影响

以氧化石墨凝胶制备的氧化石墨烯(GO)溶胶为前驱体,在100—350℃温度下还原获得不同还原程度的还原氧化石墨烯(rGO)样品,并采用旋涂工艺制备还原氧化石墨烯气敏薄膜元件.采用X射线衍射、拉曼光谱、傅里叶变换红外光谱和气敏测试等手段研究还原温度对样品结构、官能团和气敏性能的影响.结果表明:经热还原处理的氧化石墨烯结构向较为有序的类石墨结构转变,还原温度为200℃时,样品处于GO向rGO转变的过渡阶段,还原温度达到250℃时,则表现出还原氧化石墨烯特性;无序程度随还原温度的升高先由0.85增大至1.59,随后减小至1.41,总体呈现增加趋势;氧化石墨烯表面含氧官能团随还原温度的升高逐渐热解失去,不同含氧官能团的失去温度范围不同;热还原氧化石墨烯具有优异的室温H_2敏感性能,随着还原温度的升高,元件灵敏度逐渐减小,响应-恢复时间逐渐增大,最佳灵敏度为88.56%,响应时间为30 s.     

Raman spectroscopic study of the phosphate mineral churchite‐(Y) YPO4·2H2O

Raman spectroscopy has been used to study the rare‐earth mineral churchite‐(Y) of formula (Y,REE)(PO₄) ·2H₂O, where rare‐earth element (REE) is a rare‐earth element. The mineral contains yttrium and, depending on the locality, a range of rare‐earth metals. The Raman spectra of two churchite‐(Y) mineral samples from Jáchymov and Medvědín in the Czech Republic were compared with the Raman spectra of churchite‐(Y) downloaded from the RRUFF data base. The Raman spectra of churchite‐(Y) are characterized by an intense sharp band at 975 cm⁻¹ assigned to the ν₁ (PO₄³⁻) symmetric stretching mode. A lower intensity band observed at around 1065 cm⁻¹ is attributed to the ν₃ (PO₄³⁻) antisymmetric stretching mode. The (PO₄³⁻) bending modes are observed at 497 cm⁻¹ (ν₂) and 563 cm⁻¹ (ν₄). Some small differences in the band positions between the four churchite‐(Y) samples from four different localities were found. These differences may be ascribed to the different compositions of the churchite‐(Y) minerals. Copyright © 2009 John Wiley & Sons, Ltd.     

Raman spectroscopic study of the uranyl phosphate minerals phosphuranylite and yingjiangite

Raman spectra of phosphuranylite and yingjiangite were measured and interpreted, and compared with the published infrared spectra of both minerals. U O bond lengths were calculated using the Bartlett–Cooney empirical relations and the O HċO hydrogen bond lengths were inferred on the basis of Libowitzky's empirical relation. The presence of oxonium and (H₃O)⁺ ions, expected from the single crystal structure analysis of phosphuranylite, was not inferred from the Raman spectra. It was assumed that phosphuranylite and yingjiangite are identical and the name yingjiangite should be discarded because the name phosphuranylite has priority. Copyright © 2007 John Wiley & Sons, Ltd.     

Raman spectroscopic and SEM analysis of sodium‐zippeite

Raman at 298 and 77 K and infrared spectra of two samples of sodium‐zippeite were studied and interpreted. U O bond lengths in uranyl were calculated and compared with those inferred from the X‐ray single crystal structure data of a synthetic sodium‐zippeite analogue. Hydrogen‐bonding network in the studied samples is discussed. O H…O bond lengths were calculated and compared with those predicted from the X‐ray single crystal structure analysis. Copyright © 2007 John Wiley & Sons, Ltd.     

Performance study of the PTFE-THGEM at room and low temperature

GPM based on THGEM has shown its competitive strength compared to the conventional PMT, espe- cially in the low background research such as dark matter detection. A kind of THGEM made from PTFE, named PTFE-THGEM, is developed for the GPM to be used in CDEX. The PTFE has a lot of advantages especially its low level radioactivity. The PTFE-THGEM was tested at room and cryogenic temperature. It has a high gain in different gases and shows good stability at room temperature. The gain of a single PTFE-THGEM reached 112 at 117 K. The penning effect is also discussed in this paper to explain the ＂abnormal＂ phenomena of the gain in different gases.     

A Raman and infrared spectroscopic study of Ca2+ dominant members of the mixite group from the Czech Republic

The minerals of the mixite group—zálesíite CaCu₆[(AsO₄)₂(AsO₃OH)(OH)₆]·3H₂O from abandoned uranium deposit Zálesí, Czech Republic and calciopetersite CaCu₆[(PO₄)₂(PO₃OH)(OH)₆]·3H₂O from a quarry near Domašov na Bystřicí, northern Moravia, Czech Republic—were studied by Raman and infrared spectroscopy. The observed bands were assigned to the stretching and bending vibrations of (AsO₄)³⁻ and (AsO₃OH)²⁻ ions in zálesíite, and (PO₄)³⁻ and (PO₃OH)²⁻ in calciopetersite, and to molecular water, hydroxyl ions, and Cu‐(O,OH) units in both minerals. O H···O hydrogen‐bond lengths in zálesíite and calciopetersite structures were calculated with Libowitzky's empirical relation. Copyright © 2010 John Wiley & Sons, Ltd.     

Raman and infrared spectroscopic study of the molybdate‐containing uranyl mineral calcurmolite

Raman and infrared spectra of calcurmolite were recorded and interpreted from the uranium and molybdenum polyhedra, water molecules and hydroxyls point of view. U O bond lengths in uranyl and Mo O bond lengths in MoO₆ octahedra were calculated and O H…O bond lengths were inferred from the spectra. The mineral calcurmolite is characterised by bands assigned to the vibrations of the UO₂ units. These units provide intense Raman bands at 930, 900 and 868 and 823 cm⁻¹. These bands are attributed to the anti‐symmetric and symmetric stretching modes of the UO₂ units, respectively. Raman bands at 794, 700, 644, 378 and 354 cm⁻¹ are attributed to vibrations of the MoO₄ units. The bands at 693 and 668 cm⁻¹ are assigned to the anti‐symmetric and symmetric A_g modes of the terminal MO₂ units. Similar bands are observed at 797 and 773 cm⁻¹ for koechlinite and 798 and 775 cm⁻¹ for lindgrenite. It is probable that some of the bands in the low wavenumber region are attributable to the bending modes of MO₂ units. Copyright © 2008 John Wiley & Sons, Ltd.     

Raman and infrared study of phyllosilicates containing heavy metals (Sb,Bi): bismutoferrite and chapmanite

The kaolinite‐like phyllosilicate minerals bismutoferrite BiFe³⁺₂Si₂O₈(OH) and chapmanite SbFe³⁺₂Si₂O₈(OH) have been studied by Raman spectroscopy and complemented with infrared spectra. Tentatively interpreted spectra were related to their molecular structure. The antisymmetric and symmetric stretching vibrations of the Si O Si bridges, δ SiOSi and δ OSiO bending vibrations, ν (Si O_terminal)⁻ stretching vibrations, ν OH stretching vibrations of hydroxyl ions, and δ OH bending vibrations were attributed to the observed bands. Infrared bands in the range 3289–3470 cm⁻¹ and Raman bands in the range 1590–1667 cm⁻¹ were assigned to adsorbed water. O H···O hydrogen‐bond lengths were calculated from the Raman and infrared spectra. Copyright © 2009 John Wiley & Sons, Ltd.     

Fine fluorescence and absorption spectra of hypericin in a polymer matrix at a temperature of 4.2 K

Monochromatic photoexcitation and selective registration in bands of purely electronic S₁↔S₀ transitions resulted in fine fluorescence and absorption (fluorescence excitation) spectra of hypericin in polyvinylbutyral at a temperature of 4.2 K. Vibration analysis of the spectra is done and conclusions are made about the form of many normal vibrations. It is found that the formation of intramolecular hydrogen bonds in the hypericin structure has a substantial effect on the relative position of the electronic vibrational levels of the pigment molecule. Institute of Molecular and Atomic Physics of the National Academy of Sciences of Belarus, 70, F. Skorina ave., Minsk 200072, Belarus. Translated from Zhurnal Prikladnoi Spektroskopii, Vol. 65, No. 4, pp. 539–545, July–August, 1998.     

Ultrasound-promoted green approach for the synthesis of sulfonamides using natural,stable and reusable Natrolite nanozeolite catalyst at room temperature

Natural Natrolite nanozeolite has been investigated as an efficient and reusable catalyst for the N-sulfonylation of amines under ultrasound irradiation at room temperature. Compared with traditional methods, the significant advantages for method are green solvent, milder and cleaner conditions, higher purity and yields, shorter reaction time, easier work-up procedure and the lower generation of waste or pollutions. The catalyst can be recovered and reused several times without significant loss of its catalytic activity.