面向21世纪文献检索课教学内容改革初探

本文分析了文献检索课国内外现状及发展趋势，探讨了面向２１ 世纪文献检索课的教学内容     

面向服务集成的厦门火炬园建设地理信息系统

在开发区建设过程中,常面临土地建设规划、土地征用、农用地流转、项目建设及建成后的土地集约利用评价等问题,由于相关数据源自多个部门,数据共享与互操作困难.针对厦门火炬园开发区建设管理部门面临的上述问题,提出采用网络服务技术实现数据共享与互操作,管委会部门数据以Web Service形式发布,通过调用测绘部门基础地理信息共享服务平台实现基础地理信息共享.使用Web Service实现Auto CAD数据Web端动态浏览与叠加.基于Flex技术实现网络服务的富客户端聚合,开发了建设处地理信息系统.结果表明:系统能够有效管理各种原始规划、规划变更、土地利用、土地开发红线等信息,在统一地理信息框架下实现了多部门分布式数据的叠加与分析.     

新疆卡拉脚古牙锑金矿床赋矿地层时代和成矿时代

采用Rb Sr同位素定年方法 ,对新疆卡拉脚古牙锑金矿床赋矿地层的含炭泥质千枚岩进行测定 ,获得Rb Sr等时线年龄 379± 1 9Ma ;成矿时代采用主成矿期与锑金共生的石英 ,利用4 0 Ar- 39Ar法获得成矿时代为 1 1 8.2± 3.2Ma .研究结果表明 :卡拉脚古牙锑金矿床的赋矿地层时代为中泥盆世 ,该锑金矿床的主成矿时代为燕山晚期     

泌尿结石分析标样二水草酸钙的制备与表征

在卵磷脂和柠檬酸钠存在下,以氯化钙和草酸钠为原料制备了尿路结石分析标样——二水草酸钙(COD).采用扫描电镜、元素分析、热失重测定及X射线衍射、红外光谱分析,证实样品COD含量达99%以上,可作为仪器分析的标准样品使用.用制备的COD绘制红外光谱一阶导数,在1320cm-1处,光谱强度I与浓度C的线性回归方程I=5.5×10-5C 9.2×10-5,r=0.9966.     

湖北省七姊妹山自然保护区华南虎考察初报

报道了国家Ⅰ级保护动物华南虎（Panthera tigris amoyensis)在湖北省七姊妹山自然保护区活动的证据，并提出了保护对策。     

BBO四倍频全固态Nd:YVO4紫外激光器

报道了用BBO晶体对激光二极管抽运Nd:YVO₄晶体声光调Q产生的1.064μm激光 进行四倍频,实现平均功率为63mW准连续波266nm紫外激光运转,重复频率为12.5kHz、单 脉冲能量5μJ、峰值功率达252W,绿光-紫外光转换效率达11%. 关键词： 266nm紫外激光 四倍频 全固态     

丹酰氯SiO2纳米发光标记物的制备

通过合成丹酰氯的荧光单体硅酯前驱物,采用油包水的反相微乳液法,以丹酰氯的荧光单体硅酯前驱物为核材料,成功地制备了丹酰氯的荧光纳米颗粒,克服了传统方法制备核壳荧光纳米颗粒中存在的荧光染料泄漏问题.通过透射电子显微镜表征该纳米粒子呈球形,大小均匀,直径为40nm左右.所制得纳米颗粒荧光性质稳定,受外界环境的影响小,且潜在生物亲和性,是一种新型的荧光标记物.     

Quantum entanglement transition in vertically coupled two single-electron quantum dots with charged impurity

Effects of a charged impurity on the ground state of two vertically coupled identical single-electron quantum dots with and without applied magnetic field are investigated. In the absence of the magnetic field, the investigations of the charged impurity effect on the quantum entanglement (QE) in some low-lying states are carried out. It is found that, both the positive charged impurity (PCI) and the negative charged impurity (NCI)reduce the QE in the low-lying states under consideration except that the QE in the ground state is enhanced by the NCI. Additionally, in the domain of B from 0 Tesla to 15 Tesla, the ground state energy E, the ground state angular momentum L and the ground state QE entropy S are worked out. As far as the ground state are concerned, the PCI (NCI) blocks (induces) the angular momentum phase transition and the QE phase transition besides the known fact (i. e., the PCI/NCI decreases/increases the energy) in the magnetic field.     

脉冲激光制备ZnO薄膜的结构和光学特性

通过脉冲激光沉积方法在1.3 Pa氧氛围,石英衬底上制备了ZnO薄膜.用X射线衍射(XRD)谱,原子力显微镜(AFM),光致发光谱(PL)表征了薄膜的结构和光学特性.XRD谱显示在生长温度500℃时获得了六方结构的单晶薄膜;AFM显示出随着温度的提升,晶粒提升,而表面粗糙度变小;PL谱显示出强烈的紫外发射和蓝光发射.随着温度的提升,薄膜的结构和光学特性得到显著提高.     

Centennial changes of drought/flood spatial pattern in eastern China for the last 2000 years

The statistical characteristics of the bicentennial changes of the drought/flood spatial pattern over the eastern part of China have been analyzed from 101 AD to 1900 AD, and their relationship with the cold/warm climatic variation in the same time span are discussed as well. The main conclusions are as follows. (I) During the period of the 2nd ～ 11th centuries, the spatial pattern of drought/flood in the eastern part of China was characterized by thc east-west differentiation. Namely, it was dry in the west (northwest) while it was wet in the east (southeast). (ii) From the 12th to 15th centuries, the east-west differentiation coexisted with the south-north differentiation, and the former was still the dominant pattern. (iii) However, the dominant spatial pattern changed to the south- north differentiation during the 16th ～ 19th centuries, namely, it was dry in the north and wet in the south. As for the dry-wet demarcation line. It shifted westward in warn times, and once reached Datong-Taiyuan-Xi' an-Hanzhong; whereas in cold times, it retreated southeastward and reached Ji' nan-Heze-Nanyang. Furthermore, the transmeridian (W-E) dry-wet demarcation line was replaced by the meridian (N-S) dry-wet demarcation line during the two coldest periods. Moreover, in cold times, it was dry in northern China, and it was wet in the middle and lower reaches of Changjiang River and regions south of Changjiang River; in warm times, however, it was wet in northern China, and was dry in eastern China, especially in the lower reaches of Changjiang River and regions south of Changjiang River.