铒掺杂钠铝硅玻璃成分对其光谱性质的影响

研究了Na2O含量对Na2O-Al2O3-SiO2(NAS)玻璃的光谱性质的影响。利用Judd-Ofelt(J-O)理论和吸收光谱计算了Er^3+掺杂的铝硅酸盐玻璃的Ωt参数、自发辐射几率和自发辐射寿命，分析了Ωt参数与Na2O含量的关系以及与吸收截面，Er^3+离子^4I13 2能级的自发辐射几率和荧光半峰全宽(FWHM)等性质的关系。随Na2O含量的增加．J-O参数Ωt(t=2，4，6)减小，Er^3+离子1533nm的吸收截面和荧光半峰全宽．Er^3+离子^4I13 2能级的自发辐射几率也减小，而E

Preparation and spectroscopic properties of Er3+-doped high silica glass fabricated by sintering nanoporous glass

A compact nonporous high silica (SiO2 % > 96%) glass containing 3400 ppm Er3+ ions, which was about ten times higher than that in Er-doped silica fiber amplifier (EDSFA), was synthesized by sintering porous glass immersed into erbium nitrate solution. The 1532 nm fluorescence has a FWHM (Full Width at Half Maximum) of 45 nm wider than that of EDSFA and possesses the glass with potential application in broadband fiber amplifiers. The Judd-Ofelt theoretical analysis reflects that Er3+ ions are located in a higher covalent environment which are comparable to those of aluminosilicate glass. (c) 2005 Elsevier B.V. All rights reserved.

The fabrication of TiO2-supported zeolite with core/shell heterostructure for ethanol dehydration to ethylene

The TiO2-supported zeolite with core/shell heterostructure was fabricated by coating aluminosilicate zeolite (ASZ) on the TiO2 inoculating seed via in situ hydrothermal synthesis. The catalysts were characterized by transmission electron microscope (TEM), X-ray diffraction (XRD), nitrogen physisorption (BET), and Fourier transform infrared spectroscopy (FT-IR). The surface acidity of the catalysts was measured by pyridine-TPD method. The catalytic performance of the catalysts for ethanol dehydration to ethylene was also investigated. The results show that the TiO2-supported zeolite composite catalyst with core/shell heterostructure exhibits prominent conversion efficiency for ethanol dehydration to ethylene.

硅铝酸盐纳米管（imogolite）的合成与组装

纳米管是重要的一维纳米材料，在催化、分离、光电子材料、生物医药、超分子组装及复合材料等领域的应用前景广阔。探索新型的纳米管材料、研究它们的性质以及与高分子体系的杂化行为对该领域的发展具有重要意义。 Imogolite是一种纳米管状结构的硅铝酸盐，结构规整、具有独特的亲水性以及在水溶液中的分散性，是一种理想的纳米管研究对象。本论文采用正硅酸乙酯水解法合成了imogolite纳米管。使用光学显微镜，TEM，SEM，FTIR，WAXD，TGA等手段系统地研究了imogolite纳米管的生长机理、imogolite纳米管在液滴干燥过程中的自组装行为、imogolite纳米管与聚电解质的组装行为，以及imogolite纳米管/水溶性聚合物体系在液滴干燥过程中的组装行为。 Imogolite纳米管在液滴蒸发过程中可发生有序排列的自组装行为，这与液滴干燥过程中的毛细管流动、表面张力效应及润湿性质等有关。在空气中干燥imogolite液滴时，溶液浓度、pH、离子强度均会影响纳米管在液滴干燥斑中的聚集形态。低浓度液滴干燥后形成的取向纳米管束结构很好地验证了环状干燥斑的形成机理。而在乙醇气氛下干燥imogolite液滴时，毛细管流动被抑制，体系的表面能降低，因此可获得在基底上单根均匀分散的imogolite纳米管。 利用上述结果，首次实现了对合成imogolite纳米管聚合生长过程的直接观察。发现imogolite纳米管在生长过程中，直径尺寸均匀稳定；而长度的多分散性始终存在，且长度多分散性指数小于2。聚合反应初期，纳米管数量和长度均增长迅速；反应后期，纳米管长度和体系浓度的增大致使纳米管运动受限，反应为扩散控制，但体系内仍有大量imogolite短管生成并持续生长，使纳米管数量和长度在反应后期仍可继续增长。这表明合成imogolite纳米管是由扩散控制的硬棒状分子单元逐步聚合形成。 基于imogolite纳米管独特的表面性质，研究了imogolite与水溶性聚合物之间的组装行为。首次发现imogolite纳米管能够与聚电解质(PAA，PAH，PSS，PDDA)在水溶液中组装形成稳定的微米管结构。此类微米管是由椭球形的囊泡相互连接形成的超分子组装体。微米管结构稳定，骨架为无规的imogolite纳米管，聚电解质起粘结作用。微米管的形成不依赖于聚电解质的电荷性质或氢键作用，但聚电解质的浓度和分子量、聚电解质与imogolite的配比、温度、外力场以及pH均能够影响微米管的生长及最终形态。 聚阴离子聚电解质PAA和PSS与imogolite纳米管之间存在较强的相互作用，这阻碍了纳米管在液滴蒸发过程中的自组装行为，使其无法有序排列。Imogolite纳米管在PEO液滴干燥过程中的自组装行为与PEO浓度、分子量和端基性质有关。对于低浓度PEO体系，PEO能通过被氧化的端羟基与imogolite纳米管相互作用，吸附到imogolite纳米管外壁的PEO分子可以改变纳米管的排列间距。这表明在聚合物/imogolite体系中，通过改变聚合物分子的结构参数，可调控imogolite纳米管在液滴干燥过程中的排列方式。

Growth mechanism. of synthetic imogolite nanotubes

By controlling the surface effects during droplet evaporation of imogolite solutions, imogolite nanotubes were dispersed individually and directly observed by transmission electron microscopy (TEM), and the structure evolution of imogolite nanotubes in the synthetic process was investigated. It was found that the number of imogolite nanotubes continuously increased with time in the whole reaction. The average length grew slowly over time after a remarkable increase in the initial 24 h, and the length distribution experienced a similar variation with the polydispersity index always below 2. No appreciable changes in tube diameters were detected under TEM observation.

Microtubes via assembly of imogolite with polyelectrolyte

We report the self-assembly of polyelectrolyte homopolymers such as poly(acrylic acid) with imogolite to generate stable tubular structures, which were several micrometers in diameter and millimeters in length with no hierarchical ordered structure. No special polymer architecture or interaction was required for the assembly.

Individual dispersion of synthetic imogolite nanotubes via droplet evaporation

Morphology of synthetic imogolite nanotubes formed in droplet evaporation was investigated by transmission electron microscopy and electron diffraction. The nanotubes form a dense entangled network at higher concentrations, while at lower concentrations the nanotubes are liable to form oriented bundles. Under enthanol atmosphere, individual dispersion of nanotubes was observed for the first time, which reveals the length polydispersity of synthetic imogolite nanotubes.

Long lasting phosphorescence of Eu2+ in reduced SrO-B2O3 glasses

The blue long-lasting phosphorescence (LLP) phenomenon was observed for Eu2+-doped SrO-B2O3 glasses prepared in the reducing atmosphere. The phosphorescence peaks at about 450 nm due to the 4f5d -> 4f transition of Eu2+. With the doping of different amounts of Eu2+, the concentration-quenching phenomenon was observed for both the LLP and photoluminescence of the glasses, and the critical concentration for the two cases was same, i.e., 0.02 mol% Eu2+. And by the investigation of the TL curves, the content of Eu2+ had an effect on the trap depth of the samples. At last the possible mechanism of the LLP of the samples was suggested.

Luminescence properties of CdSiO3 : Mn2+ phosphor

A novel long-lasting phosphor CdSiO3:Mn2+ is reported in this paper. The Mn2+-doped CdSiO3 phosphor emits orange light with CIE chromaticity coordinates x = 0.5814 and y = 0.4139 under 254 nm UV light excitation. In the emission spectrum of 1% Mn2+-doped CdSiO3 phosphor, there is a broad emission band centered at 575 nm which can be attributed to the,pin-forbidden transition of the d-orbital electron associated with the Mn2+ ion. The phosphorescence can be seen by the naked eyes in the dark clearly even after the 254 nm UV irradiation have been removed for about 1 h. The mechanism of the origin of the long-lasting phosphorescence was discussed using the thermoluminescence curves.

Long lasting phosphorescence, thermoluminescence and electron spin resonance property of Mn2+ activated ZnO-Al2O3SiO2 ceramic

The long lasting phosphorescence (LLP) phenomenon in Mn2+-doped ceramic based on ZnO-Al2O3-SiO2 (ZASM) is observed. After irradiation by a UVP standard mercury lamp peaking at 254 nm with a power of 0.6 mW/cm(2) for 15 min, the ceramic sample emits a bright green light peaking at 519 nm, which can be seen in the dark even 15 h after the removal of UVP standard mercury lamp by the naked eyes whose limit of light perception is 0.32 mcd/m(2). The initial afterglow intensity reaches about 1900 mcd/m(2), and the color coordinate (X, Y) is (0.2280, 0.5767) at about 10 s after stopping irradiation. The thermoluminescence (TL) spectra show that there are at least three kinds of trap centers with different trap levels while electron spin resonance (ESR) spectra indicate that there are electron- and hole-trapping centers induced after irradiation by a UVP standard mercury lamp. Based on these measurements, the LLP is considered to be due to the recombination of electrons and holes at trapping centers with different levels, which are firstly thermally released back to Mn2+ and then give rise to the bright green LLP at room temperature.

俯冲带深部流体特征——以西南天山变质俯冲杂岩为例

The subduction zone is an important site of the fluid activity and recycling of chemical elements. The fluid characteristic of deep subduction zones is a top scientific problem attracting the petrologists, geochemists and tectonists. In this dissertation, the characteristics of fluid activity within a deep subduction zone have been explored on the basis of the studies on the petrography, mineral chemistry, fluid inclusions, geochemistry and metamorphic P–T conditions of the omphacite-bearing high-pressure veins and related hosts from the low-temperature/high-pressure metamorphic belt in southwestern Tianshan, China. Multiple high-pressure veins are exposed in host eclogites and blueschists. The veins are composed predominantly of omphacite, garnet, quartz, and other minerals. Some veins contain cm-sized rutiles. In general, the vein can be divided into three types, the ‘in situ dehydration’ vein, the ‘external transport’ vein and the ‘composite’ vein. The omphacites within the veins and related host rocks contain lots of two-phase or three-phase primary fluid inclusions. The final melting temperature (Tfm) of fluid inclusions varies mainly from -0.6 to -4.3 °C, the homogeneous temperature (Th) varies from 185 to 251 °C, the salinity varies from 1.1 to 6.9 wt.% NaCl equivalent and the density varies from 0.81 to 0.9 g/cm3. The fluids were released under the conditions of T = 520–580°C and P = 15–19 kbar at blueschist facies to eclogite facies transition. The fluids include not only Li, Be, LILE, La, Pb-enriched and HFSE- and HREE-depleted aqueous fluids but also HFSE (Ti-Nb-Ta)-rich aqueous fluids. The complex composed of aluminosilicate polymers and F was the catalyst which had caused the Ti-Nb-Ta to be dissolved into the fluids. During the transport of the LILE-rich and HFSE- and HREE-poor fluids, they can exchange some chemical elements with country rocks and leach some trace elements in some extent. The rutile could be precipitated from the HFSE (Ti-Nb-Ta)-rich aqueous fluids when CO2 was added into the fluids. The host rocks could obtain some elements, such as Ca, Cs, Rb, Ba and Th, from the external fluids. The fluids with complex composition had been released within the deep subduction zone (>50 km) in Early Carboniferous during the subduction of the South Tianshan Ocean under the Yili–Central Tianshan Plate. The results obtained in this dissertation have made new progress compared with the published data (e.g. Tatsumi, 1989; Becker et al., 1999; Scambelluri and Philippot, 2001; Manning, 2004; Hermann et al., 2006; Spandler and Hermann, 2006).

Stable tetrahedral aluminum sites in hexagonal mesoporous aluminosilicates

A unique templating approach for the synthesis of hexagonal mesoporous aluminosilicates via self-assembly of pre-formed aluminosilcate nanoclusters with the templating micella formed by cetyltrimethylammonium bromide (CTAB) is described. The obtained materials of MAS-5 are hydrothermally stable, which is shown by X-ray diffraction (XRD) analysis. Furthermore, as characterized by NMR technique, MAS-5 has stable tetrahedral aluminum sites that is the major contributions to the acidity of aluminosilicate molecular sieve, and on non-framework aluminium species in the samples was observed.