沙尘环境下复合绝缘子表面积污特性的仿真

文中着眼于沙尘环境下复合绝缘子的积污特性的研究，基于Fluent仿真平台的仿真计算和依托沙尘暴模拟系统的模拟试验，将研究结果进行对比，可为沙尘暴环境下复合绝缘子的选型使用、优化设计、运行维护等提供前期预研和开拓经验，且在研究方法上也首次采用仿真的方式，有重大的借鉴意义及实用价值。     

船用螺旋桨三维建模方法研究

从分析船用螺旋桨三维模型主要几何特征入手,阐述其三维坐标计算方法。在探讨了螺旋桨某些特殊部位的处理方法后,运用三维模型设计软件,以某螺旋桨建模实例演绎其方法步骤。     

弄福屯危岩体发育特征及稳定性分析

百色市凌云县弄福屯危岩体发现已久，近年来多次发生零星崩塌掉块现象，严重威胁山下村民的生命财产安全。通过工程地质调查，查明了弄福屯危岩体发育区的工程地质特征，分析了危岩体形成的原因、破坏方式及主要影响因素。根据其破坏方式分别进行稳定性计算，评价危岩体的稳定性并提出治理措施。     

力学-经验路面设计指南（MEPDG）简介

主要介绍美国力学一经验路面设计指南（MEPDG）的背景、设计主要步骤、输入参数、材料特性、柔性路面分析和性能预测及MEPDG推广应用,可为道路工程人员参考和借鉴。     

浅谈冷弯薄壁型钢房屋建筑技术

随着人口增长和城市化进程的加快,引发并刺激了对住宅的巨大需求。而我国采用高投入、高消耗、高污染的传统砖石住宅结构体系,已难以满足市场、消费者的要求和建筑＂可持续发展＂的时代主题。冷弯薄壁住宅钢结构发展潜力巨大,作为传统住宅结构体系的理想替代品,其具有更加明显的综合经济效益。     

240火花塞式燃气机预燃燃烧技术研究

针对目前国内外气缸直径200 mm,单缸排量10 L以上火花塞式4冲程燃气机热效率低、热负荷高、可靠性低等问题,以南车资阳机车有限公司240系列火花塞式燃气机(燃气主要成分为CH4)为例,简要介绍对解决这些问题进行的预燃燃烧技术研究.     

气动燃油混合动力汽车的发展现状与展望

为了缓解能源和环境双重压力，汽车行业正处于多元化时代，提出了电动汽车技术、燃料电池汽车技术、燃气汽车技术、生物质能源汽车技术等多种新能源汽车技术，这些新技术都有各自的优势和不足。文章对气动动力系统和气动燃油混合动力系统分别进行研究，同时介绍了这2种动力系统国内外发展状况，得出把气动动力系统和传统内燃机有机的结合起来，可以起到优势互补的效果，可见气动燃油混合动力汽车具有广泛的市场和美好的前景。     

浅析内河船舶碰撞事故的若干特性

文中提出了内河船舶碰撞事故所具有的一些基本特性，列举了大量具体数据、实例，从事实上进行了详细的分析，并结合水上交通碰撞事故某些个性从管理的基本原理出发加以探析。只有关注和研究船舶碰撞事故特性，才能减少或避免碰撞事故的发生。     

独立旋转车轮动力学性能研究

独立旋转车轮的结构型式与传统轮对相比具有很大的差别，在直线和曲线上的轮轨接触动力学性能也有明显差异。独立旋转车轮理论上不存在纵向蠕滑，具有较高的临界速度和较低的轮轨磨耗，其直线对中性能和曲线导向性能较差。利用计算机仿真，对独立旋转车轮和传统轮对的动力学性能进行了比较分析。     

Habitat characteristics as determinant of the structure and spatial distribution of epibenthic and demersal communities of Le Danois Bank (Cantabrian Sea, N. Spain)

The purpose of this paper is to detect and describe general trends in the spatial distribution of epibenthic and demersal communities of Le Danois Bank (El Cachucho) in relation to the environmental variables that characterize their habitat by means of multivariate ordination. Data were derived from two multidisciplinary surveys carried out in October 2003 and April 2004 included in the ECOMARG project. The surveys were focused on the study of the physical scenario, including both geological (seabed characterization from bathymetry and backscatter data) and hydrographic features, and the different compartments of the benthic fauna (endobenthic, epibenthic, suprabenthic and demersal communities). For the present study, epibenthos and demersal species were sampled using two different gears, a 3.5 m beam trawl and a Porcupine 39/52 type baca otter trawl respectively. The total species richness combining both samplers ascended to 221, including 71 species of fishes, 65 crustaceans, 35 molluscs, 29 echinoderms, 10 cnidarians and 5 sponges.Multivariate methods were used for the study of the characteristics of communities and habitats. Hierarchical cluster analysis was applied to calculate and visualize similarities between samples in terms of species composition. To assess the amount of variation of faunal densities related to a set of eight environmental variables, a redundancy analysis (RDA) was used. The set of environmental variables used were: depth, near-bottom temperature and salinity, sedimentary typology (dry weight percentages of coarse sands, medium and fine sands, silt and organic matter) and seafloor reflectivity. Using the spatial distribution of the ranges of depth and seafloor reflectivity that characterize the habitats of the faunal assemblages we defined the spatial distribution of the different communities.The multivariate analysis of 18 beam-trawl samples and 15 otter trawl samples showed the existence of 4 main assemblages associated with the more characteristic habitats of the area. The Callogorgia–Chimaera community live mainly in the areas at the top of the Bank (425–550 m depth), where the sediment coverage is lower and there exists a high presence of rocky outcrops. The Gryphus–Galeus community were found in the areas at the top of the Bank covered by medium and fine sand sediments with low organic matter content. The Phormosoma–Trachyrincus community live on the sedimentary terraces that characterize the Bank break (550–800 m) and the Pheronema–Deania community occupy all the deeper (800–1050 m) sedimentary grounds of the inner basin.