A complete sequence and comparative analysis of a SARS-associated virus(Isolate BJ01)

Severe Acute Respiratory Syndrome (SARS) is a newly identified infectious disease[1—5]. The global outbreak of SARS has been threatening the health of people worldwide and has killed 353 people and infected more than 5462 in 27 countries, as reported by WHO on April 29, 2003 (http://www.who.int/csr/sarscountry/en). Although it has been recognized that a variant of virus from the family of coronavirus might be the candidate pathogen of SARS[1—5], its identity as the unique pathogen sti…     

金属基体表面热熔敷玻璃涂层耐蚀性研究

利用斑点试验、点蚀试验、电化学测试及扫描电镜等方法 ,研究了熔敷温度、保温时间和稀土添加量等工艺参数对热熔敷法制备的玻璃涂层耐蚀性的影响 ,探讨了添加稀土提高玻璃涂层耐蚀性的机理。试验结果表明 ,采用热熔敷法制备的玻璃涂层有较好的耐蚀性。随着熔敷温度的提高和保温时间的延长 ,形成了一定量的晶相后会降低涂层的耐蚀性。试验结果表明 ,熔敷温度为 70 0℃、保温 5min后能够得到耐蚀性良好的玻璃涂层。添加稀土提高了釉料的软化温度和熔融釉料的粘度 ,阻止了结晶形核和晶核长大 ,减少了晶相 ,同时提高了涂层的电极电位 ,使涂层耐蚀性显著提高。当稀土含量为 2 %时 ,涂层的耐蚀性较好。     

Discovery of the granulite xenoliths in Cenozoic volcanic rocks from Hoh Xil,Tibetan plateau

Two-pyroxene granulite and clinopyroxene granulite xenoliths have been recently discovered in the Late Paleogene toNeogene volcanic rocks (with ages in the range of 4.27～44.60 Ma) that outcropped in Hoh Xil, central Tibetan plateau. Based on theelectron microprobe analysis data, the xenoliths provide constraints for the formation equilibrium temperatures of the two-pyroxene gran-ulite being about 783 to 818℃ as determined by two-pyroxene thermometry and the forming pressure of the clinopyroxene granulite beingabout 0.845 to 0.858 GPa that is equivalent to 27.9～28.3 km depth respectively. It indicates that these granulite xenoliths represent thesamples from the middle part of the thickened Tibetan crust. This discovery is important and significant to making further discussion onthe component and thermal regime of the deep crust of the Tibetan plateau.     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6～1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.     

小波分析在管道泄漏信号识别中的应用

利用多尺度小波变换 ,把管道泄漏产生的负压波信号作为瞬态信号 ,来识别管道的局部泄漏特征。以光滑函数的一阶导数作为小波母函数 ,研究了管道泄漏特征信号拐点区间的敏感性 ,突出小波变换系数的局部极值性。分析表明 ,检测信号的小波变换系数极值的奇异性准确地反映了管道检测信号的泄漏特征 ,并且从局部描述了管道泄漏信号的瞬态正则性。对各级尺度系数进行了S形曲线拟合 ,此曲线能够完整地描述管道泄漏瞬变特征 ,其拐点区间描述了管道发生泄漏时的瞬变过程。     

边水驱油藏调剖技术

针对边水驱油藏的地质及开发特点 ,提出了边水调剖技术 ,同时对调剖井点的选择、调剖剂的筛选、调剖剂用量的确定、调剖施工工艺等配套技术进行了研究。通过向优选的调剖井注入调剖剂 ,可以控制边水的侵入方向和推进速度 ,从而增大波及系数 ,提高最终采收率。 2 0 0 0年 5月到 1 1月 ,对高 1 0 4 5区块 8口井进行了边水调剖试验 ,共注入调剖剂 1 851 6m3。调剖后 ,内部井的含水率下降、产量回升 ,明显提高了区块的采收率。数值模拟预测结果表明 ,调剖增油超过 70 0 0t,投入产出比大于 1∶2。     

Bi含量对SrBi4Ti4O15铁电材料性能的影响

~~Bi含量对SrBi_4Ti_4O_(15)铁电材料性能的影响@朱骏$扬州大学物理科学与技术学院!江苏扬州,225002 @毛翔宇$扬州大学物理科学与技术学院!江苏扬州,225002 @卢网平$扬州大学物理科学与技术学院!江苏扬州,225002 @惠荣$扬州大学物理科学与技术学院!江苏扬州,225002 @陆文峰$扬州大学物理科学与技术学院!江苏扬州,225002 @陈小兵$扬州大学物理科学与技术学院!江苏扬州,225002~~~~~~~~     

舟桥丙丁接头接触分析的计算机模拟

深入考察接触行为的特点，并以舟桥纵向连接件丙丁接头为例，建立了两种接触计算模型。采用大型通用有限元程序进行分析，模拟丙丁接头受力时的应力应变。与经验合成计算结果和常规有限元分析的结果进行对比，证明接触分析方法对连接件塑性变形、疲劳分析和优化设计有重要的指导意义。     

高校学科导航资源的知识组织模式及优化

就目前国内外学科资源导航建设现状 ,CALIS学科导航项目建设进展 ,导航库知识组织模式 ,Web站点信息资源的维护方案 ,信息技术对组织模式的影响 ,网络信息资源评价体系的建设方法、指标 ,建立信息质量控制机制和体系 ,信息的优化方案等问题做了探讨 ,分析了网络信息组织的发展趋势 .由此为用户提供具有较高可信度的网络信息资源的有效服务     

New geological evidence of crustal thickening in the Gangdese block prior to the Indo-Asian collision

Recent mapping in the Gangdese block has revealed many leucogranites that are similar to those in the High Himalaya. These leucogranites formed at ～140 Ma as indicated by monazite Th-Pb ion-microprobe dating and cooled at ～130 Ma as indicated by muscovite ^40Ar/^39Ar dating. In conjunction with previous structural and paleogeographic studies, the new data indicate that the Gangdese block underwent crustal thickening and associated exhumation during ～140—130 Ma. In this regard, the southern margin of Eurasia continent was comparable to the modern South American Altiplano-Puna plateau, the prime example of active ocean-continent subduction and associated thickened crust. Specifically, the early stages of crustal thickening and uplifting of the Gangdese block may result from subduction of the Neo-Tethyan Ocean. If the Tibetan Plateau would form by accretion of a series of blocks with thickened crust, an elevated topographic plateau similar to the Altiplano-Puna plateau had formed before collision between the Indian and Eurasian plates. Then the Tibetan Plateau would have quickly thickened, uplifted, and begun to extend soon after onset of the collision. Thus, the deformational mechanism of the Tibetan Plateau is not distributed shortening, but rather concentrating deformation within regions of thin crust between the accreted blocks.