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1.
The high-frequency refractive index of PbGa2S4 crystal has been calculated using the Harrison bonding-orbital method. Satisfactory agreement between the calculation results and experimental data is obtained.  相似文献   

2.
The results of electron paramagnetic resonance (EPR) studies of Ce3+ impurity ions in single crystals of lead thiogallate PbGa2S4 have been reported. The Ce3+ ions substitute for Pb2+ ions in the crystal lattice of PbGa2S4. A number of paramagnetic cerium centers in lead thiogallate have been observed. The spectra are described by the spin Hamiltonian of rhombic symmetry with the effective spin S = 1/2. The g factors of the main cerium centers have been determined. A large number of paramagnetic centers are due to both nonequivalent positions of lead and local charge compensation under the substitution Ce3+ ?? Pb2+.  相似文献   

3.
Optical reflection spectra are measured and calculated in PbGa2S4 crystals in the region of resonances related to excitons with large oscillator strength and binding energy (Frenkel excitons). The splitting of the upper valence band in the center of the Brillouin zone due to crystal field (Δcf) and spin orbit (Δso) interaction are determined. Optical reflection spectra are measured and calculated according to Kramers-Kronig relations in the region of 3-6 eV in Ес and Ес polarizations, and the optical constants n, k, ε1 and ε2 are determined. The observed electronic transitions in PbGa2S4 crystals are discussed in the frame of theoretical energy band structure calculation for thiogallate crystals.  相似文献   

4.
张季  王迪  张德明  张庆礼  万松明  孙敦陆  殷绍唐 《物理学报》2013,62(3):37802-037802
通过偏振拉曼光谱和第一性原理计算对非线性光学晶体BaBPO5的 晶格振动模式进行了研究. 实验得到了不同几何配置下、在100–1600 cm-1范围内的晶体偏振拉曼光 谱与傅里叶变换红外吸收谱, 结合因子群分析方法研究了晶体的外振动与内振动模式特征. 分析表明拉曼振动主要来自于PO4四面体和BO4四面体的振动, 且PO4基团振动具有较强的拉曼与红外活性. 此外,根据第一性原理对晶体拉曼振动进行了数值模拟, 进一步明确了拉曼峰与晶体中原子振动的对应关系, 计算表明拉曼光谱中位于672 cm-1峰位来自晶体中B–O–P键的伸缩振动, 这是晶体中PO4四面体和BO4四面体共顶点连接的特征结构在光谱中的体现.  相似文献   

5.
Raman scattering in Rb2TeBr6 and Cs2TeBr6 crystals is studied. The phonon spectra of the crystals are calculated using the factor group method. The number of Raman-active modes, their symmetries, and selection rules are found. Observed Raman spectrum lines are identified with atomic vibration modes of the crystal.  相似文献   

6.
Raman scattering and optical absorption in crystalline S4N4 have been measured both as a function of pressure at 295 K and low temperatures. Polarized single crystal Raman data were also obtained as an aid in the assignment of the Raman active phonons. The pressure coefficients of the Raman active external and S-S stretching modes show a discontinuity near 7 kbar indicative of a second order phase change. The optical absorption edge at about 2.5 eV of a sublimed film of S4N4 shows red shifts of 1.3 × 10?5 eV bar?1 and 6.3 × 10?4 eV K?1 with pressure and temperature respectively. In the light of these results, the electronic, vibrational and structural properties of the crystal are discussed.  相似文献   

7.
Birefringence of PbGa2S4 single crystals is studied in the spectral range of 0.45–0.8 μm at T = 300 K. The obtained results are analyzed, and conclusions on the bond character in lead thiogallate are drawn.  相似文献   

8.
We report and comment for the first time the Raman spectrum of ZnGa2Se4. Looking for family trends we compare the present results with those obtained in other gallium defect chalcopyrites. The proportionality law between the frequencies of corresponding phonons in different compounds is verified for all the modes with the exception of the lowest energy polar modes. Evidence of the peculiarity of these modes is obtained, confirming what reported for ZnxCd1-xGa2S4 pseudoternary compounds.  相似文献   

9.
The origin of the low-lying modes of KH2PO4 and KD2PO4 in the ferroelectric phase has been clarified by the z(xy)z? Raman scattering experiments. The “S-mode”, which has been usually assigned to the proton tunneling mode in KH2PO4 at T<Tc, has been found in the z(xy)z? spectrum of KD2PO4 in contrast to the x(xy)y spectrum. It has been found that the frequency of the “S-mode” of KD2PO4 is higher than that of KH2PO4. These results have shown that the “S-mode” is far from the proton tunneling mode nor the proton/deuteron mode at all. From the present Raman spectroscopy, it is concluded that the “S-mode” is assigned to the libration mode of the PO4 tertahedrons.  相似文献   

10.
Raman spectrum of burgessite, Co2(H2O)4[AsO3OH]2· H2O, was studied, interpreted and compared with its infrared spectrum. The stretching and bending vibrations of (AsO3) and As‐OH units, as well as the stretching, bending and libration modes of water molecules and hydroxyl ions were assigned. The range of O H···O hydrogen bond lengths was inferred from the Raman and infrared spectra of burgessite. The presence of (AsO3OH)2− units in the crystal structure of burgessite was proved, which is in agreement with its recently solved crystal structure. Raman and infrared spectra of erythrite inferred from the RRUFF database are used for comparison. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

11.
The polarized Raman and reflection spectra of a single crystal YbAl3(BO3)4 at room temperature were studied. Raman active vibrational modes A 1, E TO, and E LO are identified. In the Raman spectrum, we detected an intense line at a frequency of 1018 cm−1, which refers to internal vibrations of the BO3 group and is known to be promising for use in amplifiers based on stimulated Raman scattering. From the simulation of reflection spectra by the method of dispersion analysis the frequencies of A 2 vibrational modes were determined. Intense bands observed in the low-temperature transmission spectra in the range of f-f transitions in the Yb3+ ion are attributed to electron-phonon transitions. The Raman lines are compared with electron-phonon lines in the transmission spectrum.  相似文献   

12.
Abstract

We present the Raman spectrum of Tm3Al5O12 single crystal and its pressure dependence for hydrostatic pressure up to 11GPa and room temperature. Tm3Al5O12 belongs to the crystal family of rare earth garnets (Re3A12(AlO4)3, Re: Gd, Tb, Dy, Er,…), which crystallize in the body-centered cubic lattice and contains eight molecular units in the conventional unit cell, Group theory predicts 25 Raman active modes for these compounds, while experimentally are observed 15 modes. As crystal volume decreases all Raman peaks exhibit pressure coefficients varying from 0.7 to 5.6cm?1/ GPa. A large part of the vibrational spectra of these compounds could be explained taking into account the vibrational properties of molecular subunits, namely AlO4.  相似文献   

13.
The results of electron paramagnetic resonance (EPR) studies of Dy3+ ions in lead thiogallate PbGa2S4 single crystals have been presented. It has been shown that the ground state of these ions corresponds to the lowest Stark sublevel Γ6 of the term 6 H 15/2. The spectra are well described by the axially symmetric spin Hamiltonian with the effective spin S = 1/2 with the factors g = 15.06 and g = 2.47. The Dy3+ ions substitute Pb2+ ions in the crystal lattice of PbGa2S4. The observed hyperfine structure has allowed to unambiguously interpret the EPR spectra. The hyperfine interaction constants of two odd isotopes of dysprosium in lead thiogallate single crystals have been found to be A = 675 × 10?4 cm?1 and A = 111 × 10?4 cm?1 for 163Dy and A = 472 × 10?4 cm?1 and A = 77 × 10?4 cm?1 for 161Dy.  相似文献   

14.
A group-theoretical vibrational modes symmetry analysis of SnI4 crystals has been made for the Brillouin zone center and polarized Raman scattering study in these crystals has been carried out. Correlation diagram showing the correspondence between the crystal vibrational modes and the free SnI4 molecule modes has been built. The nature and peculiarities of the low frequencies spectrum have been considered.  相似文献   

15.
The Raman spectrum of crystalline As4S3 has been investigated as a function of temperature from 4 to 430 K at ambient pressure, and as a function of pressure to 70 kbar at ambient temperature. The external mode frequencies which appear clearly separated from the internal modes exhibit stronger pressure and temperature sensitivity compared to the latter modes. At the β-As4S3 to α-As4S3 phase transition near 410 K, the external modes change discontinuously indicating a first-order phase transition. The internal mode frequencies remain practically unaffected. The dvdP and dvdT data are analyzed using well established approaches. Application of non-hydrostatic pressure (>60 kbar) appears to destroy the crystallinity of As4S3.  相似文献   

16.
Highly resolved spectra of S1 ? S0 and S2 ← S0 electronic transitions of sym-tribenzotridehydro [12] annulene (TBA) in polycrystalline methylcyclohexane matrices are obtained at 77 K. By comparison with the reinvestigated IR and Raman spectra of TBA several e' and a'1 modes are identified in the fluorescence spectrum. The lifetime and quantum yield of TBA fluorescence are equal to 38 ns and 0.15, respectively, at room temperature. The calculations of the electronic structure of TBA within the PPP CI approximation are performed.  相似文献   

17.
Polarized Raman measurements were recorded on a monoclinic brushite (CaHPO4.2H2O) crystal in the 800–1200 cm−1 spectral range, corresponding to the P O stretching modes. This study is a continuation of the investigation of the phosphate stretching modes observed in polarized infrared reflectance spectra of brushite crystal. In such ionic non‐centrosymmetric crystals, the splitting between the transverse and longitudinal components of the optic vibrations was observed in the polarized Raman spectra recorded at several scattering geometries. A″ symmetry modes of the brushite crystal were measured. Using a simple model based on the symmetry of the PO4 group, the Raman intensities of the stretching modes are calculated and compared with experimental bands. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

18.
The mineral gerstleyite is described as a sulfosalt as opposed to a sulfide. This study focuses on the Raman spectrum of gerstleyite Na2(Sb,As)8S13·2H2O and makes a comparison with the Raman spectra of other common sulfides including stibnite, cinnabar and realgar. The intense Raman bands of gerstleyite at 286 and 308 cm−1 are assigned to the SbS3E antisymmetric and A1 symmetric stretching modes of the SbS3 units. The band at 251 cm−1 is assigned to the bending mode of the SbS3 units. The mineral stibnite also has basic structural units of Sb2S3 and SbS3 pyramids with C3v symmetry. Raman bands of stibnite Sb2S3 at 250, 296, 372 and 448 cm−1 are assigned to Sb S stretching vibrations and the bands at 145 and 188 cm−1 to S Sb S bending modes. The Raman band for cinnabar HgS at 253 cm−1 fits well with the assignment of the band for gerstleyite at 251 cm−1 to the S Sb S bending mode. Raman bands in similar positions are observed for realgar AsS and orpiment As2S3. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

19.
Four one-phonon Raman lines have been found in CdIn2S4 (ZnIn2S4) spinels at 92 (72) cm-1, 186 (184) cm-1, 246 (253) cm-1, and 367 (372) cm-1 for incident photon energies well below the energy gap EG ~ 2.4 (2.2) eV at 300 K. For photon energies close to EG, the 367 cm-1 mode underwent a resonant enhancement in CdIn2S4 and four infrared active but Raman forbidden F1u modes appeared in the CdIn2S4 and ZnIn2S4 Raman spectra: TO modes at 226 (221) cm-1 and 309 (312) cm-1, and LO modes at 274 (272) cm-1 and 340 (342) cm-1.  相似文献   

20.
Raman spectroscopy complemented with infrared (IR) spectroscopy has been used to study the mineral schroeckingerite. The mineral is a multi‐anion mineral and has (UO2)2+, (SO4)2− and (CO3)2− units in its structure, and bands attributed to these vibrating units are readily identified in the Raman spectra. Symmetric stretching modes at 815, 983 and 1092 cm−1 are assigned to (UO2)2+, (SO4)2− and (CO3)2− units, respectively. The antisymmetric stretching modes of (UO2)2+, (SO4)2− are not observed in the Raman spectra but may be readily observed in the IR spectrum at 898 and 1180 cm−1. The antisymmetric stretching mode of (CO3)2− is observed in the Raman spectrum at 1374 cm−1, as is also the ν4 (CO3)2− bending modes at 742 and 707 cm−1. No ν2 (CO3)2− bending modes are observed in the Raman spectrum of schroeckingerite. All the spectroscopic evidence points to a highly ordered structure of this mineral. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

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