跨海火车客滚船机动性探讨

利用船舶机动性的概念及机动性指标,说明火车滚装客船具有良好机动性的必要性,从我国第一艘跨海火车渡船的设备配备性情况说明跨海火车渡船船舶动力装置设计上考虑操纵机动性的特点。     

第三方物流企业信息平台的研究与开发

分析了港口发展第三方物流及构建其物流信息平台(LIP)的必要性，对策三方物流企业LIP的开发方法和应用体系结构进行了探讨，从功能需求、系统平台及开发工具选择、数据库平台设计和程序实现等方面对LIP的开发过程进行了阐述。     

超级电容器在直流电力系统中应用研究

本文介绍了以超级电容器作为储能元件的储能系统在直流电力系统中的应用.通过对储能系统运行状态的分析,给出了储能系统中各主要元件取值的计算方法,并利用SimPlorer6.0对所介绍的系统进行了仿真,仿真结果验证了分析的正确性.     

船用柴油主发电机弹性底座安装工艺改进

本文主要阐述了船用柴油主发电机弹性支撑底座安装的特点,从而针对一般施工工艺中的问题进行总结并改进与完善,达到提高作业效率,缩短生产周期的目的。     

基于ASP的在线考试系统的设计及应用

一个完整的在线考试系统应该包括考试用户注册系统、在线考试系统、分级账户及试卷管理系统、用户成绩查询系统、帮助系统等。本文提出了一种基于Asp的在线考试系统解决方案,具有移植性好、易于实现等优点。     

加强CAD/CAM技术教育,培养现代工程技术人才

本文探讨了我国目前工程教育中存在的问题,提出了一些利用现代CAD/CAM技术,推进工程教育改革的具体措施,增强学生工程实践能力和创新能力。     

分局机车调度管理系统的设计与实现

基于分局机车调度日常工作,探讨采用计算机网络与通信技术实现分局机车调度管理系统的设计方案.     

VRH法在铸钢水玻璃砂中的应用

本文通过对 VRH 法在铸钢水玻璃砂中应用的研究,提出了该法在生产中确定型芯砂成分及硬化工艺参数的原则,为解决铸钢件落砂与清理问题提供了新的途径.     

3D轴焊接构架式转向架重车过曲线轮轨横向力超标原因分析

根据转向架结构理论分析和动力学仿真计算,对3D轴焊接构架式转向架通过曲线时重车轮轨横向力偏大的原因进行分析。认为3D轴焊接构架式转向架的主、副摩擦面摩擦系数偏大,使重车通过曲线时斜楔处于卡死状态,轮对轴箱纵向呈刚性定位,从而导致重车过曲线时轮轨横向力偏大。提出只要将斜楔副摩擦面的摩擦系数减小至0.1左右,则在轮轨纵向蠕滑力的作用下,轴箱斜楔纵向就不会被卡死,而且轮对纵向定位刚度只由轴箱弹簧提供,可以有效地降低重车过曲线时的轮轨横向力。线路动力学试验证明理论分析和仿真计算的结果是正确的。     

Seasonal variability in sea surface oceanographic conditions in the Aegean Sea (Eastern Mediterranean): an overview

Seasonal variability and the spatial distribution of sea surface temperatures (SST) and salinities (SSS) are reviewed, in relation to the prevailing climatological conditions, heat fluxes, water budget and general water circulation patterns. Within this context, consideration is given to: sea surface temperatures; air temperatures; precipitation; evaporation; wind speeds and directions; freshwater (mainly riverine) discharges throughout the Aegean; and the exchange of water masses with the Black Sea and eastern Mediterranean Sea. The investigation of satellite images, covering a 6-yr period (1988–1994), has enabled a synthesis of the monthly sea surface thermal distribution to be established.The climate of the Aegean Sea is characterised by annual air temperatures of 16–19.5°C, precipitation of about 500 mm yr⁻¹ and evaporation of some 4 mm d⁻¹. The Aegean has a negative heat budget (approximately −25 W m⁻²) and positive water balance (+ 1.0 m yr⁻¹), when inflow from the Black Sea is considered. During the summer, the (northerly) Etesians are the dominant winds over the Sea.Mean monthly sea surface temperatures (SST) vary from 8°C in the north during winter, up to 26°C in the south during summer. SST depends mainly upon air temperature; there is a month's delay between the former and latter maxima. The sea surface salinity (SSS) varies also spatially and seasonally, ranging from less than 31 psu, in the north, to more than 39 psu, in the southeast; lower values (< 25 psu) occur adjacent to the river mouths. SSSs present their maximum differences during summer, whilst during winter and autumn the distribution of SSS is more uniform. The overall spatial SST and SSS distribution pattern is controlled by: distribution of the (colder) Black Sea Waters; advection of the (warmer) Levantine Waters, from the southeastern part of the Aegean; upwelling and downwelling; and, to a lesser extent, but locally important, freshwater riverine inflows.