Cr~(4+)∶Ca_2GeO_4多晶料的合成与表征

采用固相法合成Cr4+∶Ca2GeO4晶体原料,通过XRD分析确定了合成Cr4+∶Ca2GeO4多晶料的最佳温度,计算了Cr4+∶Ca2GeO4多晶料的晶格参数。XPS和荧光光谱分析表明多晶料中含有Cr4+。Cr4+∶Ca2GeO4多晶料具有宽的室温荧光光谱,光谱范围为1000~1600 nm,最强荧光发射峰位于1257 nm,这是Cr4+的3T2→3A2能级跃迁导致的荧光发射。     

Synthesis and characterization of Cr4+-doped CaO–GeO2–Li2O–B2O3(Al2O3) transparent glass-ceramics

Synthesis and devitrification behavior of Cr-doped CaO–GeO₂–Li₂O–B₂O₃(Al₂O₃) glasses have been studied. A range of glass compositions was found to yield transparent glass-ceramics after devitrification. The size of crystallites is below 1 μm. Glass-ceramic samples exhibit 1050–1600 nm broad-band emission with a maximum around 1260 nm, very similar to the emission of Cr⁴⁺:Ca₂GeO₄ bulk crystals. X-ray diffraction measurements indicate that the structure of crystallites exhibiting near infrared emission in glass-ceramics may be assigned to Cr⁴⁺:Ca₂GeO₄ with increased lattice parameters.     

Order Parameters and Distribution Function of 4'-(N-(p-Pentyloxy Carbonyloxy-Benzylidene)Amino) Valerophenone in Smectic Phase from X-ray Diffraction Measurements

Abstract

X-ray diffraction studies of 4'-(N (p-pentyloxycarbonyloxy-benzylidene)amino)valerophenone (PCBAV in short) oriented by a magnetic field is reported here. The compound has a smectic A phase which is identified by X-ray studies and texture studies. Orienta-tional order parameters (p ₂) and (P ₄) have been determined from the calculation of f(β), the orientational distribution function. An approximate expression for the angular part of the potential of the mean field is obtained from the temperature variation of the orientational distribution function. The value of d, the layer thickness, and D, the intermolecular distance, have been calculated. An approximate value for the translational order parameter τ₁ and average value of the root mean square displacement ?z²?½ are given. We could not get an accurate estimate of the translational order parameter due to the inaccuracy in the measurement of the intensity of the inner ring.     

(Nd3+,Yb3+):Ca3(VO4)2晶体的极化研究

本文回顾了(Nd3+,Yb3+):Ca3(VO4)2晶体的研究历程,通过对晶体结构和对晶体激光性能研究年代的对比,认为高的泵浦阈值是由于晶体中存在的对泵浦光和激光散射很强的畴壁结构未被发现而造成的.讨论了极化的原理、建立了极化装置,采用Laue定向法和X射线定向仪定向法结合解决了(Nd3+,Yb3+):Ca3(VO4)2这种大晶格常数(c＝3.8029nm)晶体的定向问题.把晶体的抛光面放入0.5mol;的温度为30℃的硼酸中腐蚀样品1h,用显微镜可以观察到畴结构.在～1100℃和电流密度为～10μA/mm2的条件下极化2h即可完成极化.变黑的极化样品可以通过把晶体放入马福炉中升温至850℃,保持1h,然后降至室温即可消除.     

Phase transitions in Cs5(HSO4)2(H2PO4)3 crystal

The symmetry (sp. gr.I $\bar 4$ 3d) and lattice parameters have been determined for the first time for Cs₅(H₂SO₄)₂(H₂PO₄)₃ crystals in the temperature range from 172 to 390 K. The thermal and optical properties of crystals, as well as their conductivity, have been investigated at elevated temperatures. It is shown that a crystal heated to T = 365 K undergoes a phase transition with symmetry lowering to the tetragonal phase (with the parameters a = 4.965(1) Å and c = 5.016(1) Å), while at T ≈ 390 K a phase transition to the cubic phase is presumably observed. With a decrease in temperature, a phase transition without a change in symmetry occurs at T = 240 K.     

X-ray Diffraction Study on MgSeO4. 6 H2O at Elevated Temperatures

The dehydration of MgSeO₄. 6 H₂O has been studied using an X-ray powder diffraction method at elevated temperatures. Five different solid phases have been identified in the temperature interval of 20–450 °C: MgSeO₄. 6 H₂O; MgSeO₄. 5 H₂O (with a small amount of MgSeO₄. 4 H₂O), MgSeO₄. 2 H₂O, amorphous MgSeO₄ and crystalline MgSeO₄. MgSeO₄. 5 H₂O crystallizes in the triclinic system with the lattice parameters: a = 6.403(2) Å, b = 10.576(5) Å, c = 6.196(3) Å, α = 98.63(2)°, β = 110.36(2)°, γ = 75.25(3)°, SG P1 . MgSeO₄. 2 H₂O forms orthorhombic crystals with lattice parameters: a = 10.304(1) Å, b = 10.351(9) Å, c = 9.138(9) Å. The crystalline anhydrous magnesium selenate crystallizes in the orthorhombic system with the lattice parameters: a = 4.925(2) Å, b = 9.026(5) Å, c = 6.816(6) Å. Additionally MgSeO₄. 4 H₂O has been prepared and studied roentgenographically: monoclinic system with the lattice constants: a = 6.064(4) Å, b = 13.773(7) Å, c = 8.062(6) Å, β = 91.82(7)°, SG P2₁/n. According to expectation the magnesium selenate hydrates are isomorphous with the corresponding magnesium sulphate hydrates.     

Ca3(PO4)2:Dy3+纳米荧光粉 的制备及发光性能研究

采用水热法制备出Ca3(PO4)2:Dy3+纳米荧光粉,通过XRD、SEM和荧光光谱对样品进行了分析,主要研究了制备工艺以及Dy3+离子掺杂浓度对材料发光性能的影响规律.研究结果表明:初始溶液pH值为7,反应釜填充度为80;,在180℃条件下反应24 h所得的Ca3(PO4)2:0.02 Dy3+纳米荧光粉发光性能最佳.SEM分析表明荧光粉颗粒的平均粒径为100 nm,分散性好.     

新型激光自倍频晶体Cr:Nd:GdCa4O(BO3)3

首次利用提拉法生长了优质铬离子敏化激光自倍频晶体Cr:Nd:GdCa4O(BO3)3(Cr:Nd:GdCOB),发现当铬离子和钕离子双掺时,由于协同效应使铬离子容易进入GdCOB晶体中,测量了Cr:Nd:GdCOB和Nd:GdCOB晶体的室温透过谱和荧光谱.Cr:Nd:GdCOB晶体在蓝紫外区比Nd:GdCOB晶体具有更强的吸收,适合于利用闪光灯泵浦.利用闪光灯泵浦分别对长度为7mm,沿最佳倍频方向(θ＝66.8°,φ＝132.6°)切割的Cr:Nd:GdCOB和Nd:GdCOB晶体进行自倍频实验.Cr:Nd:GdCOB的激发阈值为0.9J,而Nd:GdCOB的激发阈值为1.0J.在10J的输入能量时,Cr:Nd:GdCOB输出绿光能量为2.46mJ,而Nd:GdCOB输出绿光能量为1.96mJ,说明在该晶体中,铬离子对钕离子有很好的敏化作用.     

X-Ray Diffraction Study of New Organic Compound n-Tol3Sb[OC(O)CH=CHPh]2

Crystallography Reports - The bis[(2E)-3-phenylprop-2-enoate]-tris(п-tolyl)antimony n-Tol3Sb[OC(O)CH=CHPh]2 complex is obtained as a result of interaction of tri-n-tolylantimony, hydrogen...     

Study of calcium-containing orthophosphates of NaZr2(PO4)3 structural type by high-temperature X-ray diffraction

Orthophosphates Ca_0.5Ti₂(PO₄)₃, Ca_0.5Zr₂(PO₄)₃, Ca_0.75Zr₂(SiO₄)_0.5(PO₄)_2.5, and CaMg_0.5Zr_1.5(PO₄)₃ (structural type NaZr₂(PO₄)₃), having different occupancies of interframework positions by calcium, have been prepared by the sol-gel method with the subsequent thermal treatment of dried gels and investigated by IR spectroscopy and X-ray diffraction. The analytical indexing of X-ray diffraction patterns is performed within the sp. gr. $R\bar 3$ . High-temperature X-ray diffraction was used to investigate the behavior of the orthophosphates upon heating: thermal expansion in the temperature range of 20–610°C (up to 500°C for Ca_0.5Zr₂(PO₄)₃). The coefficients of thermal expansion are calculated from the shift of diffraction peaks. The unit-cell parameters of crystals at different temperatures are determined. The dependences of thermal expansion and its anisotropy on the occupancy of cation M positions by calcium are revealed.     

Surface Evolution at the Phase Transitions in (NH4)3H(SeO4)2 Crystals

Crystallography Reports - The (NH4)3H(SeO4)2 crystals in the temperature range of 296–343 K and the evolution of their surface at phase transitions have been studied by atomic force...     

Synthesis and X-ray Crystal Structure Analysis of CU2(CH3CH2COO)4(OP)2

The complex of [CU(CH₃CHCOO)₂(OPph)]₂ has been synthesized and its X-ray crystal structure determined at room temperature, M = 975.96, tetragonal, space group: 14_1/a(#88), Dx = 1.39 g/ cm³, The final R is 0.067 for 2087 independent observed reflections with 1 > 3α(I). The molecule has an inversion center on the middle of the Cu Cu axis. The bond-length of the Cu Cu is 2.61/(2) Å. The coordinate polyhedron of Cu corresponds to a tetragonal bipyramid. The angle of Cu O P is significantly smaller than that of its adducts [Cu(O₂CR)₂L]₂.     

New synthesis and X-ray diffraction study of a polymeric form of Ag(I) dithio-o-toluato, [Ag4(S2C-o-C6H4CH3)4]n

The title compound was synthesized by CS₂ insertion in the C-M bonds of the corresponding AgLi ate organomental compound. It contains flattened tetrahedral Ag₄ units, connected in polymeric chains by intermolecular Ag...S interactions. Two Ag atoms and three S atoms are in a distorted square pyramidal arrangement around each silver atom. The crystals are tetragonal, space group 14₁/a witha=23.706(2) andc=12.934(2) Å. The structure was refined toR=0.032 for 889 reflections.     

Single Crystal X-ray Diffraction Study of a Pure Natrolite Sample

The crystal structure of a pure natrolite sample, Na₂(Al₂Si₃O₁₀)·2H₂O, coming from Asheken, Ethiopia, has been analysed by single crystal X-ray diffraction. It crystallizes within the orthorhombic space group Fdd2, with the following cell constants: a = 18.2930(2) Å; b = 18.6430(5) Å; c = 6.5860(5) Å; V = 2246.07(18) Å³. The three-dimensional framework of this hydrated aluminosilicate zeolite is made up by chains of corner-sharing SiO₄ and AlO₄ tetrahedra down c; the chains are held together by sharing the external vertices of tetrahedra; water molecules and Na⁺ extra-framework cations fill up the resulting cavities, the latter forming irregular NaO₆ octahedra. Hydrogen bonds complete the array.