硒、维生素E对自由基损伤培养兔软骨细胞的保护作用

采用细胞培养方法,以黄嘌岭-黄嘌岭氧化酶(XXO)系统产生自由基,造成软骨细胞的自由基损伤;软骨细胞DNA及蛋白多糖的合成受到明显抑制;膜流动性降低;电镜下观察到细胞表面有大小形态各异的囊泡状突起,胞内可见线粒体肿胀或呈固缩样改变、溶酶体增多等超微病理损害。向培养基中提前1d加入硒及维生素E能对抗自由基所致的氧化性损伤。     

连续刚构0#块局部应力分析

连续刚构0#块处于墩梁固结处,该梁段构造复杂,内有大量的预应力束通过。为揭示其在各种不利工况下的空间应力分布情况,需建立相应的空间有限元模型进行分析。文章以一座连续刚构桥为工程背景,运用ANSYS有限元软件对0#块进行局部应力分析,结果表明0#块局部位置应力分布较复杂,应进行钢筋补强。     

基于Pro/E塑料顾问分析的塑料盒盖注射模具设计

针对传统模具设计的弊端,提出了采用模流分析技术对模具进行优化设计的思想。以Pro/E塑料顾问为平台,以塑料盒盖零件为实例,对其浇口位置进行计算机模拟分析,并在此基础上对塑料产品进行注射成型工艺模拟分析。综合分析结果有针对性地优化模具设计方案,避免了设计中的盲目性,提高了塑料产品的成型质量,减少了缺陷的产生,降低了生产成本,缩短了生产周期。     

京张高速铁路连续梁0^#段吊装施工技术

依托新建北京至张家口高速铁路延庆下行联络线跨大浮坨村烽火台特大桥主跨连续梁0^#段工程施工,详细地介绍了连续梁0^#段预制完成后吊装就位的施工技术,并制定了安装过程施工质量和安全控制措施。采用该技术,连续梁0^#段和桥梁主墩可同时施工,不仅能保证工程施工质量和工期,而且在北方寒冷地区高空中无法实现冬施措施的项目中具有很强的推广价值。通过新建京张高速铁路桥梁工程的连续梁工程的快速施工,验证了该技术的可行性。     

大跨度部分斜拉桥上部结构施工技术

荷麻溪特大桥主梁特大型0号块采用贝雷架作支架、水平分三层浇筑等施工技术，采用超宽三角斜拉式后支点挂篮现浇部分斜拉桥大型箱梁施工技术，以及斜拉索采用环氧涂层钢绞线成品索，工厂加工成品，现场整束安装整束悬浮式张拉技术。     

集装箱船抗横倾系统及其“0”位检验

本文简略介绍了抗横倾系统的功能,对其系统组成和工作原理进行详尽的说明,并介绍我厂对抗横倾‘0’位的检验方法。     

《白虎通义》声训的价值与不足

《白虎通义》的声训在训诂学史上有一定的地位和影响。其声训有助于音韵学研究，有助于推求语源，有助于系联同源词，有助于破假借；但也存在很多不足。文章对《白虎通义》声训的学术价值和不足之处作了简要的分析。     

Variability of the western Galician upwelling system (NW Spain) during an intensively sampled annual cycle. An EOF analysis approach

The key features of the western Galician shelf hydrography and dynamics are analyzed on a solid statistical and experimental basis. The results allowed us to gather together information dispersed in previous oceanographic works of the region. Empirical orthogonal functions analysis and a canonical correlation analysis were applied to a high-resolution dataset collected from 47 surveys done on a weekly frequency from May 2001 to May 2002. The main results of these analyses are summarized bellow. Salinity, temperature and the meridional component of the residual current are correlated with the relevant local forcings (the meridional coastal wind component and the continental run-off) and with a remote forcing (the meridional temperature gradient at latitude 37°N). About 80% of the salinity and temperature total variability over the shelf, and 37% of the residual meridional current total variability are explained by two EOFs for each variable. Up to 22% of the temperature total variability and 14% of the residual meridional current total variability is devoted to the set up of cross-shore gradients of the thermohaline properties caused by the wind-induced Ekman transport. Up to 11% and 10%, respectively, is related to the variability of the meridional temperature gradient at the Western Iberian Winter Front. About 30% of the temperature total variability can be explained by the development and erosion of the seasonal thermocline and by the seasonal variability of the thermohaline properties of the central waters. This thermocline presented unexpected low salinity values due to the trapping during spring and summer of the high continental inputs from the River Miño recorded in 2001. The low salinity plumes can be traced on the Galician shelf during almost all the annual cycle; they tend to be extended throughout the entire water column under downwelling conditions and concentrate in the surface layer when upwelling favourable winds blow. Our evidences point to the meridional temperature gradient acting as an important controlling factor of the central waters thermohaline properties and in the development and decay of the Iberian Poleward Current.     

Remotely-sensed chlorophyll a observations of the northern Red Sea indicate seasonal variability and influence of coastal reefs

The biological dynamics of the open northern Red Sea (21.5°–27.5° N, 33.5°–40° E) have not been studied extensively, due in part to both the inaccessibility of this desert region and political considerations. Remotely-sensed chlorophyll a data therefore provide a framework to investigate the primary patterns of biological activity in this oceanic basin. Monthly chlorophyll a data from the 8-year Sea-viewing Wide Field-of-View sensor (SeaWiFS) mission, and data from the Moderate Resolution Imaging Spectroradiometer (MODIS), were analyzed with the Goddard Earth Sciences Data and Information Services Center (GES DISC) online data analysis system “Giovanni”. The data indicate that despite the normal low chlorophyll a concentrations (0.1–0.2 mg m^− 3) in these oligotrophic waters, there is a characteristic seasonal bloom in March–April in the northernmost open Red Sea (24° to 27.5° N) concurrent with minimum sea surface temperature. The location of the highest chlorophyll concentrations is consistent with a linear box model [Eshel, G., and Naik, N.H., 1997. Climatological coastal jet collision, intermediate water formation, and the general circulation of the Red Sea. J. Phys. Oceanogr. 27(7), 1233–1257.] of Red Sea circulation. Two years in the data set exhibited a different seasonal cycle consisting of a relatively weak northern spring bloom and elevated chlorophyll concentrations to the south (21.5° to 24° N).The data also indicate that large coral reef complexes may be sources of either nutrients or chlorophyll-rich detritus and sediment, enhancing chlorophyll a concentration in waters adjacent to the reefs.