考虑层间接触状态的横观各向同性结构动力响应解析解

基于线弹性体动力学基本方程,结合坐标变换、Buchwald势函数,建立了移动荷载作用下层状横观各向同性结构的动力控制方程,利用傅里叶变换及其微分性质得到了在Fourier变换域内单层有限厚度刚度矩阵和半空间无限体刚度矩阵.考虑层间接触条件组装各刚度矩阵得到总刚度矩阵,并根据边界条件求解总刚度矩阵在变换域内的解.然后,进行Fourier逆变换将变换域内的解转化为物理域内的解.通过与已有文献结果的对比验证了本文理论推导的正确性,随后通过参数的变化来模拟层间接触状态的改变,并分析了面层与基层层间接触状态对路面结构动力响应的影响.计算结果表明:基、面层层间接触状况越差,路面结构的整体性耐久性越差.     

"得"句中主语S的构成

从句法结构方面考察和分析“得”字句中“得”前的主语S。根据主语S是否出现,“得”句可分为主语未省略句和主语省略句两类,其中,主语省略的情况比较普遍。在主语未省略的情况下,主语大多由体词和体词性短语充当;在主语省略的情况下,主语承某一句省略占了相当的比例。     

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。     

Ehresmann型rpp半群的最小C-rpp半群同余

本文定义Ehresmann型rpp半群,它是纯正群并在rpp半群类中的推广,我们给出了此类半群的最小C-rpp半群同余.     

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.