A far-infrared investigation of cathodochromic sodalite

Sodalite absorption bands in the 50–350 cm⁻¹ region were studied using Fourier transform spectroscopy. Vibrational modes were identified using chemical substitution, H₂ and vacuum-annealing, and coloration studies. A bromosodalite band at 294 cm⁻¹ was assigned to an Si—O—Al mode based on Ge substitutions for Si. A bromosodalite band at 200 cm⁻¹ is assigned to an Na—cage vibration based on previous H₂annealing studies and chemical substitution of Ge for Si, Ga for Al and Cl and I for Br. A 107 cm⁻¹ band is the Na—Br related vibration, and substitution of 100% Cl for Br moved this band to 111 cm⁻¹, H₂ and vacuum-annealing studies show a correlation between the amount of Br removed from bromosodalite during annealing and the area of the 107 cm⁻¹ band. A band at 68 cm⁻¹ is the Na—Br mode based on 100% substitution of Cl for Br. Coloration studies in the 50–150 cm⁻¹ region show no changes attributable to F-center formation.     

The infrared spectrum of carbon suboxide in the ν6 fundamental region: Experimental observation and semirigid bender analysis

The infrared spectrum of carbon suboxide, C₃O₂, was measured at high resolution in the region from 500 to 600 cm⁻¹. The spectrum was recorded with a Bomem interferometer at a resolution of about 0.004 cm⁻¹; after deconvolution a resolution of about 0.002 cm⁻¹ was attained. Seven bands were identified and assigned to rovibrational transitions of ¹²C₃¹⁶O₂. These consist of the ν₆ fundamental band and some of the hot bands associated with the ν₇, 2ν₇, and 3ν₇ states. The data obtained on the ν₆ + nν₇ states were used as input for a semirigid bender fit yielding the effective CCC bending potential energy function in the ν₆ state together with a number of related parameters. From the results of the present work together with the results of previous semirigid bender fits it was found that C₃O₂ is bent at equilibrium with an equilibrium CCC bond angle of 156° and a barrier to linearity of 28 cm⁻¹.     

Raman spectroscopic study of the magnesium‐carbonate minerals—artinite and dypingite

Magnesium minerals are important in the understanding of the concept of geosequestration. The two hydrated hydroxy magnesium‐carbonate minerals artinite and dypingite were studied by Raman spectroscopy. Intense bands are observed at 1092 cm⁻¹ for artinite and at 1120 cm⁻¹ for dypingite, attributed ν₁ symmetric stretching mode of CO₃²⁻. The ν₃ antisymmetric stretching vibrations of CO₃²⁻ are extremely weak and are observed at 1412 and 1465 cm⁻¹ for artinite and at 1366, 1447 and 1524 cm⁻¹ for dypingite. Very weak Raman bands at 790 cm⁻¹ for artinite and 800 cm⁻¹ for dypingite are assigned to the CO₃²⁻ν₂ out‐of‐plane bend. The Raman band at 700 cm⁻¹ of artinite and at 725 and 760 cm⁻¹ of dypingite are ascribed to CO₃²⁻ν₂ in‐plane bending mode. The Raman spectrum of artinite in the OH stretching region is characterised by two sets of bands: (1) an intense band at 3593 cm⁻¹ assigned to the MgOH stretching vibrations and (2) the broad profile of overlapping bands at 3030 and 3229 cm⁻¹ attributed to water stretching vibrations. X‐ray diffraction studies show that the minerals are disordered. This is reflected in the difficulty of obtaining Raman spectra of reasonable quality, and explains why the Raman spectra of these minerals have not been previously or sufficiently described. Copyright © 2008 John Wiley & Sons, Ltd.     

Effects of metal ion on the water structure studied by the Raman O?H stretching spectrum

Raman spectra in the O H stretching region of aqueous salt solutions were measured and compared, and the effects of metal ions on water structure deduced. The effects of alkali ions, alkaline ions or the first‐row transition metals on water structure were found to be similar. Differences of metal ionic effects on water structure exist among Na⁺, Mg²⁺ and Al³⁺, and between Ca²⁺ and Mn²⁺ and Al³⁺ and Fe³⁺. The factors that influence the metal ionic effects on the water structure are the ionic charge, the outmost electronic structure and ionic size, the ionic charge being the most important. With a five‐component Gaussian deconvolution of the Raman spectra of the aqueous solutions of NaCl, MgCl₂, AlCl₃ and FeCl₃ with concentrations of 0 to ∼1mol/l, the ionic effects were found to be similar on the bands at 3233, 3393, 3511 and 3628 cm⁻¹, but different on the band at 3051 cm⁻¹. With increasing polarization of the metal ion, the band at 3051 cm⁻¹, due to strong hydrogen bonding, increases. Copyright © 2009 John Wiley & Sons, Ltd.     

High resolution spectrum of Ch3OH between 8 and 100cm−1

The FIR spectrum of CH₃OH between 8–100 cm⁻¹ has been measured by a high resolution Fourier transform spectrometer. A computer best fit program, based on the Taylor series expansion of the energy levels, has been used for the line assignments. The region between 40–100 cm⁻¹ is presented for the first time. The region between 8–40 cm⁻¹, covered in a previous work, is revisited in the light of the new measurements at higher frequencies, and new assignments are given. The available microwave and radio-frequency assignments have been inserted into the fit program. A catalogue of 6725 assigned MW and FIR lines below 101.8 cm⁻¹ is presented.     

High-resolution Fourier transform spectroscopy of D2CO in the 8- to 12-μm region

The Coriolis-coupled ν₃ (1100 cm⁻¹), ν₆ (989 cm⁻¹), and ν₄ (938 cm⁻¹) fundamental bands of D₂CO have been recorded with a BOMEM Model DA 3.002 Fourier transform spectrometer at an apodized resolution of 0.004 cm⁻¹. A total of 3704 transitions have been assigned in the 780- to 1200-cm⁻¹ spectral region. Constants have been determined for terms up to P⁶ in centrifugal distortion and up to P³ in Coriolis interaction. These constants reproduce the observed spectra with residuals for well-resolved lines that are less than 0.0004 cm⁻¹, one-tenth of the resolution. Relative signs of the transition moments have been determined by comparison of observed and calculated relative intensities of perturbed transitions. Five new assignments for far-infrared laser lines pumped by CO₂ lasers have been obtained as a result of calculations based on the determined constants.     

Tunable diode-laser spectra of the very weak ν10 absorption band of C2H3D

The C₂H₃D spectra from 730 to 780 cm⁻¹ have been investigated with a tunable diode laser spectrometer at Doppler-limited resolution and a wavenumber accuracy of better than 10⁻³ cm⁻¹. This resolution, combined with a long absorption path, has allowed the identification of K_a series lines belonging to the ν₁₀ level. A five-level combined analysis was performed, including previous data available for the energy states involved in the region around 1000 cm⁻¹.     

Raman spectroscopic study of the magnesium carbonate mineral hydromagnesite (Mg5[(CO3)4(OH)2]· 4H2O)

Magnesium minerals are important for understanding the concept of geosequestration. One method of studying the hydrated hydroxy magnesium carbonate minerals is through vibrational spectroscopy. A combination of Raman and infrared spectroscopy has been used to study the mineral hydromagnesite. An intense band is observed at 1121 cm⁻¹, attributed to the CO₃²⁻ν₁ symmetric stretching mode. A series of infrared bands at 1387, 1413 and 1474 cm⁻¹ are assigned to the CO₃²⁻ν₃ antisymmetric stretching modes. The CO₃²⁻ν₃ antisymmetric stretching vibrations are extremely weak in the Raman spectrum and are observed at 1404, 1451, 1490 and 1520 cm⁻¹. A series of Raman bands at 708, 716, 728 and 758 cm⁻¹ are assigned to the CO₃²⁻ν₂ in‐plane bending mode. The Raman spectrum in the OH stretching region is characterized by bands at 3416, 3516 and 3447 cm⁻¹. In the infrared spectrum, a broad band is found at 2940 cm⁻¹, which is assigned to water stretching vibrations. Infrared bands at 3430, 3446, 3511, 2648 and 3685 cm⁻¹ are attributed to MgOH stretching modes. Copyright © 2011 John Wiley & Sons, Ltd.     

Raman spectroscopy of halogen‐containing carbonates

Raman spectroscopy complemented with infrared spectroscopy has been used to study a series of selected natural halogenated carbonates from different origins, including bastnasite, parisite and northupite. The position of CO₃²⁻ symmetric stretching vibration varies with the mineral composition. An additional band for northupite at 1107 cm⁻¹ is observed. Raman spectra of bastnasite, parisite and northupite show single bands at 1433, 1420 and 1554 cm⁻¹, respectively, assigned to the ν₃ (CO₃)²⁻ asymmetric stretching mode. The observation of additional Raman bands for the ν₃ modes for some halogenated carbonates is significant in that it shows distortion of the CaO₆ octahedron. No ν₂ Raman bending modes are observed for these minerals. The band is observed in the infrared spectra, and multiple ν₂ modes at 844 and 867 cm⁻¹ are observed for parisite. A single intense infrared band is found at 879 cm⁻¹ for northupite. Raman bands are observed forthe carbonate ν₄ in‐phase bending modes at 722 cm⁻¹ for bastnasite, 736 and 684 cm⁻¹ for parisite and 714 cm⁻¹ for northupite. Multiple bands are observed in the OH stretching region for selected bastansites and parisites, indicating the presence of water and OH units in the mineral structure. The presence of such bands brings into question the actual formula of these halogenated carbonate minerals. Copyright © 2007 John Wiley & Sons, Ltd.     

Raman spectroscopic investigation of pure and ytterbium‐doped rare earth silicate crystals

Raman spectroscopy was used to study the molecular structure of a series of selected rare earth (RE) silicate crystals including Y₂SiO₅ (YSO), Lu₂SiO₅ (LSO), (Lu_0.5Y_0.5)₂SiO₅ (LYSO) and their ytterbium‐doped samples. Raman spectra show resolved bands below 500 cm⁻¹ region assigned to the modes of SiO₄ and oxygen vibrations. Multiple bands indicate the nonequivalence of the RE O bonds and the lifting of the degeneracy of the RE ion vibration. Low intensity bands below 500 cm⁻¹ are an indication of impurities. The (SiO₄)⁴⁻ tetrahedra are characterized by bands near 200 cm⁻¹ which show a separation of the components of ν₄ and ν₂, in the 500–700 cm⁻¹ region which are attributed to the distorting bending vibration and in the 880–1000 cm⁻¹ region which are attributed to the symmetric and antisymmetric stretching vibrational modes. The majority of the bands in the 300–610 cm⁻¹ region of Re₂SiO₅ were found to arise from vibrations involving both Si and RE ions, indicating that there is considerable mixing of Si displacements with Si O bending modes and RE O stretching modes. The Raman spectra of RE silicate crystals were analyzed in terms of the molecular structure of the crystals, which enabled separation of the bands attributed to distinct vibrational units. Copyright © 2007 John Wiley & Sons, Ltd.     

Remeasurement of the absolute intensities of CFC11 (CFCl3) and CFC12 (CF2Cl2)

The absolute intensities of the strong absorption bands of CFC11 (CFCl₃) and CFC12 (CF₂Cl₂) have been remeasured at 300 K in view of their importance in global climatic impact and ozone depletion studies. For CFC11, our new values are 1718 ± 17 cm⁻² atm⁻¹ (846 cm⁻¹ band) and 671 ± 8 cm⁻² atm⁻¹ (1085 cm⁻¹ band). The values we have now obtained for the CFC12 intensities are 1421 ± 12 cm⁻² atm⁻¹ (923 cm⁻¹ band), 1129 ± 11 cm⁻² atm⁻¹ (1102 cm⁻¹ band), and 717 ± 14 cm⁻² atm⁻¹ (1161 cm⁻¹ band).     

Raman spectroscopic study of the antimonate mineral brandholzite Mg[Sb2(OH)12]·6H2O

Raman spectra of brandholzite Mg[Sb₂(OH)₁₂]·6H₂O were studied, complemented with infrared spectra, and related to the structure of the mineral. An intense Raman sharp band at 618 cm⁻¹ is attributed to the SbO symmetric stretching mode. The low‐intensity band at 730 cm⁻¹ is ascribed to the SbO antisymmetric stretching vibration. Low‐intensity Raman bands were found at 503, 526 and 578 cm⁻¹. Corresponding infrared bands were observed at 527, 600, 637, 693, 741 and 788 cm⁻¹. Four Raman bands observed at 1043, 1092, 1160 and 1189 cm⁻¹ and eight infrared bands at 963, 1027, 1055, 1075, 1108, 1128, 1156 and 1196 cm⁻¹ are assigned to δ SbOH deformation modes. A complex pattern resulting from the overlapping band of the water and hydroxyl units is observed. Raman bands are observed at 3240, 3383, 3466, 3483 and 3552 cm⁻¹; infrared bands at 3248, 3434 and 3565 cm⁻¹. The Raman bands at 3240 and 3383 cm⁻¹ and the infrared band at 3248 cm⁻¹ are assigned to water‐stretching vibrations. The two higher wavenumber Raman bands observed at 3466 and 3552 cm⁻¹ and two infrared bands at 3434 and 3565 cm⁻¹ are assigned to the stretching vibrations of the hydroxyl units. Observed Raman and infrared bands in the OH stretching region are associated with O‐H···O hydrogen bonds and their lengths 2.72, 2.79, 2.86, 2.88 and 3.0 Å (Raman) and 2.73, 2.83 and 3.07 Å (infrared). Copyright © 2009 John Wiley & Sons, Ltd.     

Raman spectroscopic study of the antimonate mineral bahianite Al5Sb35+O14(OH)2

Raman spectroscopy has been used to characterize the antimonate mineral bahianite Al₅Sb₃⁵⁺O₁₄(OH)₂, a semi‐precious gemstone. The mineral is characterized by an intense Raman band at 818 cm⁻¹ assigned to Sb₃O₁₄¹³⁻ stretching vibrations. Other lower intensity bands at 843 and 856 cm⁻¹ are also assigned to this vibration, and this concept suggests the non‐equivalence of SbO units in the structure. Low‐intensity Raman bands at 669 and 682 cm⁻¹ are probably assignable to the OSbO antisymmetric stretching vibrations. Raman bands at 1756, 1808 and 1929 cm⁻¹ may be assigned to δ SbOH deformation modes, while the bands at 3462 and 3495 cm⁻¹ are assigned to AlOH stretching vibrations. The complexity in the low wave number region is attributed to the composition of the mineral. Copyright © 2009 John Wiley & Sons, Ltd.     

Raman spectroscopic study of the hydrogen‐arsenate mineral pharmacolite Ca(AsO3OH)·2H2O—implications for aquifer and sediment remediation

The removal of arsenate anions from aqueous media, sediments and wasted soils is of environmental significance. The reaction of gypsum with the arsenate anion results in pharmacolite mineral formation, together with related minerals. Raman and infrared (IR) spectroscopy have been used to study the mineral pharmacolite Ca(AsO₃OH)· 2H₂O. The mineral is characterised by an intense Raman band at 865 cm⁻¹ assigned to the ν₁ (AsO₃)²⁻ symmetric stretching mode. The equivalent IR band is found at 864 cm⁻¹. The low‐intensity Raman bands in the range from 844 to 886 cm⁻¹ provide evidence for ν₃ (AsO₃) antisymmetric stretching vibrations. A series of overlapping bands in the 300‐450 cm⁻¹ region are attributed to ν₂ and ν₄ (AsO₃) bending modes. Prominent Raman bands at around 3187 cm⁻¹ are assigned to the OH stretching vibrations of hydrogen‐bonded water molecules and the two sharp bands at 3425 and 3526 cm⁻¹ to the OH stretching vibrations of only weakly hydrogen‐bonded hydroxyls in (AsO₃OH)²⁻ units. Copyright © 2009 John Wiley & Sons, Ltd.     

The high-resolution spectrum of the ν1 (A1) band of 12CD3F

The spectrum of the ν₁ (A₁) band of ¹²CD₃F has been recorded with a resolution of 0.010 cm⁻¹ and deconvolved to 0.005 cm⁻¹. Over 1050 transitions have been assigned with K ≤ 16 and J ≤ 42. The spectrum is highly perturbed, exhibiting avoided crossings in most of the observed sub-bands. The origin of most of the local and global resonances has been determined and the coupling constants estimated. Due to the complexity of the spectrum resulting from the 24 potential interacting states in the region, the assigned frequencies were fitted in a restricted manner (K ≤ 3, J ≤ 15), to obtain the following effective constants for the band: ν₀ = 2090.8118(20) cm⁻¹, α^A = 1.19743 × 10⁻² cm⁻¹, and α^B = −1.8489 × 10⁻³ cm⁻¹. From an unrestricted least-squares analysis, fixing the above parameters the β's (D_v^x = D₀^x − β_v^x) were calculated to be β^J = 1.7776 × 10⁻⁷ cm⁻¹, β^JK = 8.3406 × 10⁻⁷ cm⁻¹, and β^K = −6.3829 × 10⁻⁷ cm⁻¹. These constants serve as good starting parameters for the global analysis necessary to fully analyze the 5-μm region of the ¹²CD₃F spectrum.     

High-resolution infrared spectrum of hydrogen peroxide: The ν6 fundamental band

The infrared spectrum of the ν₆ asymmetric deformation band of hydrogen peroxide (H₂O₂) was studied in the region 1100–1350 cm⁻¹ using the two techniques of Fourier transform spectroscopy at 0.02 cm⁻¹ resolution and tunable diode laser spectroscopy at Doppler-limited resolution. Details of the wavelength calibration procedures adopted are discussed. For the first time, accurate values of the molecular parameters of this torsionally doubled, vibrational band were obtained. A total of 708 assigned transitions have been analyzed to yield a set of 14 rovibrational constants for the lower torsion-vibration level (SD = 0.00487 cm⁻¹) and 13 rovibrational constants for the upper torsion-vibration level (SD = 0.00382 cm⁻¹). These hybrid bands are primarily A type with band centers at 1264.5812 ± 0.0009 and 1273.6830 ± 0.0009 cm⁻¹. Because of the absence of observed perturbations, the derived molecular constants can be used to calculate transition frequencies with a high degree of accuracy up to K_a = 6.     

Raman spectroscopy of the borosilicate mineral ferroaxinite

Raman spectroscopy, complemented by infrared spectroscopy, has been used to characterise the ferroaxinite minerals of the theoretical formula Ca₂Fe²⁺Al₂BSi₄O₁₅(OH), a ferrous aluminium borosilicate. The Raman spectra are complex but are subdivided into sections on the basis of the vibrating units. The Raman spectra are interpreted in terms of the addition of borate and silicate spectra. Three characteristic bands of ferroaxinite are observed at 1082, 1056 and 1025 cm⁻¹ and are attributed to BO₄ stretching vibrations. Bands at 1003, 991, 980 and 963 cm⁻¹ are assigned to SiO₄ stretching vibrations. Bands are found in these positions for each of the ferroaxinites studied. No Raman bands were found above 1100 cm⁻¹ showing that ferroaxinites contain only tetrahedral boron. The hydroxyl stretching region of ferroaxinites is characterised by a single Raman band between 3368 and 3376 cm⁻¹, the position of which is sample‐dependent. Bands for ferroaxinite at 678, 643, 618, 609, 588, 572, 546 cm⁻¹ may be attributed to the ν₄ bending modes and the three bands at 484, 444 and 428 cm⁻¹ may be attributed to the ν₂ bending modes of the (SiO₄)²⁻. Copyright © 2006 John Wiley & Sons, Ltd.     

The ν2 infrared band of 1-phosphapropyne CH3CP

The Fourier transform infrared spectrum of 1-phosphapropyne CH₃CP has been recorded in the region 1470–1580 cm⁻¹ with a resolution of 0.01 cm⁻¹, and the ν₂ band centered at 1558.7416(28) cm⁻¹ was analyzed. The 689 observed transitions with J′ and K′ values up to 69 and 8, respectively, were assigned. A set of the spectroscopic constants determined for the upper v₂ = 1 state reproduced the experimental wavenumbers with an rms error of 0.0025 cm⁻¹. No significant perturbations were observed. The ν₂ + ν₈ − ν₈ hot band, centered at 1553.5492(35) cm⁻¹, was also analyzed. The upper state constants determined from the 341 observed transitions with J′ and K′ values up to 53 and 6, respectively, reproduced the experimental wavenumbers with an rms error of 0.0047 cm⁻¹.     

Deuterated ammonia in krypton and nitrogen matrices: High-resolution spectroscopy of the ν2 mode

FTIR spectra of ND₃ in krypton and nitrogen matrices are recorded at low temperatures (7.5 K). The analysis of the ν₂ region shows that in krypton the rotation is slightly perturbed, with an inversion splitting of the ν₂ state equal to 2 cm⁻¹. In nitrogen, the inversion splitting has been searched for without success under a resolution of 0.06 cm⁻¹; in this matrix, a low-resolution measurement yields a librational frequency of 133 cm⁻¹. The present experimental results are compared with previous ones on NH₃ and with a recent theoretical model.     

Raman spectroscopy of the joaquinite minerals

Selected joaquinite minerals have been studied by Raman spectroscopy. The minerals are categorised into two groups depending upon whether bands occur in the 3250 to 3450 cm⁻¹ region and in the 3450 to 3600 cm⁻¹ region, or in the latter region only. The first set of bands is attributed to water stretching vibrations and the second set to OH stretching bands. In the literature, X‐ray diffraction could not identify the presence of OH units in the structure of joaquinite. Raman spectroscopy proves that the joaquinite mineral group contains OH units in their structure, and in some cases both water and OH units. A series of bands at 1123, 1062, 1031, 971, 912 and 892 cm⁻¹ are assigned to SiO stretching vibrations. Bands above 1000 cm⁻¹ are attributable to the ν_as modes of the (SiO₄)⁴⁻ and (Si₂O₇)⁶⁻ units. Bands that are observed at 738, around 700, 682 and around 668, 621 and 602 cm⁻¹ are attributed to O Si O bending modes. The patterns do not appear to match the published infrared spectral patterns of either (SiO₄)⁴⁻ or (Si₂O₇)⁶⁻ units. The reason is attributed to the actual formulation of the joaquinite mineral, in which significant amounts of Ti or Nb and Fe are found. Copyright © 2007 John Wiley & Sons, Ltd.