高稳定激光二极管抽运Nd∶YLF再生放大器

设计并实现了一种放大纳秒激光脉冲的高稳定的激光二极管(LD)抽运Nd∶YLF再生放大器。为了获得高稳定的输出,再生放大器工作在饱和状态。此时,再生放大器输出稳定性最好,而且注入激光脉冲能量波动引起的输出激光脉冲波动被抑制。由于增益饱和效应,再生放大器输出脉冲出现时域波形失真,附加后缀脉冲能够减弱时域波形失真。放大器工作波长1053nm,工作频率1Hz。输入240pJ的3ns方波激光脉冲,输出激光脉冲能量4.2mJ,总增益大于107,不稳定度小于1%(均方根),方波扭曲1.33。为3ns方波激光脉冲引入其本身幅度0.75倍的后缀脉冲,输出激光脉冲方波扭曲由1.33降至1.17。

中国古代玻璃的起源和发展

本文对中国古代玻璃的研究概况以及近半个多世纪来科技考古的结果作了简要的阐述。中国内地的古代玻璃技术产生于公元前500年春秋末战国初期。从中国出土的古代玻璃的化学成分的演变。阐明了中国古代玻璃的发展特点。并分析了中国内地的古代玻璃与西方古代玻璃的产生差异的原因。

Preparation and optical properties of Ag/PPy composite colloids

Ag/PPy (polypyrrole) composite colloids were prepared through the reaction of silver nitrate with pyrrole solution in DNIF either in the dark, or under the irradiation of femtosecond laser (fs) pulse or UV lamp. The UV-vis spectra of the nanocomposite colloid display an intense absorption band around 620 nm, accompanied by a weak one around 470 nm. The colors and optical absorption spectra of as-synthesized colloids can be reversibly tuned between blue and red, corresponding to absorption band of 620 urn and 526 urn, within few seconds by adding base and acid solutions or gases in turn into the composite colloid suspension. In addition, excess of H+ solution enhanced the absorption band around 470 nm and, at the same time, depressed that around 620 nm. The possible mechanism for the formation and optical absorption properties of the Ag/PPy composite colloid was proposed. (C) 2006 Elsevier B.V. All rights reserved.

Frequency upconversion fluorescence emission of Er3+-doped oxychloride germanate glass

Frequency upconversion fluorescence property of Er3+-doped oxychloride germanate glass is investigated. Intense green and red emissions centred at 525, 546, and 657nm, corresponding to the transitions H-2(11/2) -> I-4(15/2), S-4(3/2) -> 4I(15/2), and F-4(9/2) -> I-4(15/2), respectively, were simultaneously observed at room temperature. The quadratic dependence of the 525, 546, and 657nm emissions on excitation power indicates that a two-photon absorption process occurs under 975nm laser diode (LD) excitation. The Raman spectrum investigation indicates that oxychloride germanate glass has the maximum phonon energy at similar to 805 cm(-1). The thermal stability of this oxychloride germanate glass is evaluated by differential scanning calorimetry, and thermal stability factor Delta T (Delta T = T-x-T-g) is 187 degrees C. Intense upconversion luminescence and good thermal stability indicate that Er3+-doped oxychloride germanate glass is a promising upconversion laser material.

Temperature dependence of femtosecond laser induced refractive index change in Nd3+-doped phosphate glass

We report refractive index change in a femtosecond laser irradiated Nd3+-doped phosphate glass. The effects of annealing temperature on the refractive index change of the glass have been investigated. Absorption spectra of the glass sample before and after femtosecond laser irradiation and subsequent annealing were measured. The results indicate that multiphoton absorption can undertake although there are intrinsic absorption for the glass in irradiation wavelength. The results may be useful for fabrication of three-dimensional integrated optics devices and waveguide laser devices in this glass. (c) 2004 Elsevier B.V. All rights reserved.

山东山旺中新世孢粉植物及古气候和古生态研究

本文对山旺中新世孢粉植物群进行了详细的研究。在22，95米厚的山旺硅藻土剖面上系统地采集了130块孢粉样品，样品之间的采样距离为10-30厘米。鉴定出孢粉类型111种。以此为基础，对山旺碰藻土沉积期间的古气候和古生态进行了高分辨率定量的恢复和重建。 根据每种孢粉类型的生物地层信息，山旺中新世孢粉植物群形成的时代为中中新世。这个年龄值也与同位素测年的结果16.78-14.11 Ma，以及根据哺乳动物划分的生物地层带MN4-MN5相一致。 运用共存分析法定量重建了山旺中新世孢粉植物群形成时的各项气候参数的定量值。所包括的10个古气候参数值分别为： 年平均温度(MAT) 15.6-17.2ºC，最冷月平均温度(TCM)5.0-6.6 0 C，最热月平均温度(TWM) 24.6-27.8 ºC，温度的年较差( TD) 20. 0-25.5 0 C，年平均降雨量(MAP) 1162-1308mm，最热月份的平均降雨量( PwarmM)108-lllmm，最湿月份的平均降雨量(PwetM) 148-180mm，最干月份的平均降雨量(PDM) 16-59mm，最干及最 湿月份降雨量的差值(DP) 81-153mm，平均相对湿度(RH) 72-74%，共存分析的结果表明，在整个22.95米厚的研究剖面上，从底部到顶部的古植物群形成期间的古气候有一个轻微的波动，其中年平均温度的波动范围大约在3度左右，最热月平均温度的波动范围在l度左右， 最冷月平均温度的波动范围在4度左右， 年平均降雨量的波动范围在100毫米左右。 山旺中新世时的气候应属于Koppen's的“Cfa”气候类型，与现今武汉与芜湖地区的气候相似。 与现代山旺地区气候上的区别主要在于年平均降雨量、降雨量的分配，以及最冷月份的平均温度。 通过应用多元分析的方法，对山旺中新世时期的植被进行了重建。山旺中新世时期的古植被为“混交中生林”，在研究剖面从底部到顶部的时间轴上，“混交中生林”经历了“湿润环境下的混交中生林”，“干旱环境下的混交中生林”，“湿润湖岸环境下的混交中生林”，“山地、湿润及碱性环境下的混交中生林”，和“碱性环境下的混交中生林”等5个阶段的变化。山旺剖面所代表的山旺湖周围的地形在断裂构造运动的控制下，也经历了一系列的变化。