桥梁结构连同地基的整体计算方法

本文提出将桥梁上部结构、下部结构和基础连同地基整体计算的方法     

时程分析法在大蒲春河特大桥主桥抗震验算中的应用

采用时程分析法对大蒲春河特大桥进行抗震分析,对主桥控制部位E1概率和E2概率地震作用下的响应进行验算,并利用验算结果指导该桥的抗震设计.     

汽车电子电气架构设计与优化

阐述汽车电子电气架构技术与发展趋势,设计与优化的指导思想、需求信息、所用工具和工作流程,以及两个标准的系统级电子电气架构。介绍汽车电子电气架构设计与优化的优点,对我国汽车行业研发该项技术提出建议。     

汉语编程在MapX二次开发中的应用

交通地理信息系统因具有强大的信息服务和管理功能,越来越受到人们的重视。MapX作为GIS设计中一个常用的功能组件．其当前的主要编程环境是英文,这对于英文程度不高的汉语软件开发者来说无疑是个羁绊。因此,通过实例详细说明在易语言汉语编程开发环境下如何利用MapX开发GIS软件的方法,对于该组件的进一步推广应用具有一定的意义。     

基于Pro/E的机械标准零件库建立的方法

介绍了在Pro／Engineer环境下利用其二次开发工具程序(Program)和族表(Family Table)建立机械标准件库的原理和方法,并通过建立六角头螺栓零件库的实例,阐明了建立标准件库的具体步骤。     

Pro/E在减速顶中的应用

通过对三维建模软件Pro／E各种强大功能的简要介绍,指出Pro／E在当今生产行业中的重要作用,同时详细介绍了Pro／E在减速顶行业中的广泛应用。     

浅议安全监理如何在拆除延安东路高架过程中发挥的监督作用

近年来,市政基础设施建设在飞速发展,城市中可用于市政建设的空间将越来越紧张。如何在不影响周边环境和交通的前提下完成工程,对原有结构部分进行拆除和新建,尤其是在上海外滩"亚洲第一弯"拆除工程中,既要按时完成又要确保安全拆除万无一失,发挥安全监理的监督作用。该文对此作了一些有益的探讨,可供参考。     

通过INMARSAT- A/B/M/MINI-M接入INTERNET

ＩＮＴＥＲＮＥＴ是目前世界上最大的计算机互联网络,它是美国正在建设中的“信息高速公路”的支柱网络之一,也是一个初具规模的全球性信息网络。ＩＮＴＥＲＮＥＴ是一个巨大的信息资源,它容许全球千百万人相互通信,共享资源。现在,Ｅ－ＭＡＬＬ和ＩＮＴＥＲＮＥＴ被广泛看作全球性商业运营的一个重要工具,作为全球商业系统一部分的船舶,近来也开始越来越多地使用这一先进的工具。本文介绍通过卫星船站接入ＩＮＴＥＲＮＥＴ的方法及操作步骤。     

Mesoscale subduction at the Almeria–Oran front: Part 1: Ageostrophic flow

This paper presents a detailed diagnostic analysis of hydrographic and current meter data from three, rapidly repeated, fine-scale surveys of the Almeria–Oran front. Instability of the frontal boundary, between surface waters of Atlantic and Mediterranean origin, is shown to provide a mechanism for significant heat transfer from the surface layers to the deep ocean in winter. The data were collected during the second observational phase of the EU funded OMEGA project on RRS Discovery cruise 224 during December 1996. High resolution hydrographic measurements using the towed undulating CTD vehicle, SeaSoar, traced the subduction of Mediterranean Surface Water across the Almeria–Oran front. This subduction is shown to result from a significant baroclinic component to the instability of the frontal jet. The Q-vector formulation of the omega equation is combined with a scale analysis to quantitatively diagnose vertical transport resulting from mesoscale ageostrophic circulation. The analyses are presented and discussed in the presence of satellite and airborne remotely sensed data; which provide the basis for a thorough and novel approach to the determination of observational error.     

Observations of the Fawn Trough Current over the Kerguelen Plateau from instrumented elephant seals

Due to its great meridional extent and relatively shallow depths, the Kerguelen Plateau constitutes a major barrier to the eastward flowing Antarctic Circumpolar Current in the Indian sector of the Southern Ocean. While most of the Antarctic Circumpolar Current transport is deflected north of the Kerguelen Islands, the remainder ( 50 Sv, 1 Sv = 10⁶ m³ s^− 1) must pass south of the islands, most probably through the Fawn and Princess Elizabeth Troughs. However, the paucity of finely resolved quasi-synoptic hydrographic data in this remote and infrequently sampled area has limited the progress in our knowledge of the regional circulation. Since 2004, a new approach using elephant seals from the Kerguelen Islands as autonomous oceanographic profilers has provided new information on the hydrography over the Kerguelen Plateau, covering the entire Antarctic Zone between the Polar Front and Antarctica, with a mean along-track resolution of about 25 km. These finely resolved bio-logged data revealed details of a strong northeastward current found across the Fawn Trough (sill depth: 2600 m; 56°S, 78°E). This so-called Fawn Trough Current transports cold Antarctic waters found mostly south of the Elan Bank, between the Ice Limit (58°S) and the Antarctic Divergence (64°S) in the eastern Enderby Basin, toward the Australian–Antarctic Basin. Our analysis also demonstrates that the Deep Western Boundary Current, which carries cold Antarctic water along the eastern flank of the southern Kerguelen Plateau collides with Fawn Trough Current at the outlet of the Fawn Trough sill. In other words, the Fawn Trough constitutes a veritable bottleneck, channelling the quasi-totality of the Antarctic Circumpolar flow found south of the Polar Front. Thanks to the unprecedented fine resolution of seal-borne data, a branch of flow centered at the Winter Water isotherm of 1 °C is also revealed along the northern escarpment of the Elan Bank, and then along the southern edge of Heard Island. Further analysis of different supplementary data reveals a complex circulation pattern in the entire Enderby Basin, with several distinctive branches of flow being strongly controlled by prominent topographic features such as the Southwest Indian Ridge, Conrad Rise, Elan Bank, and Kerguelen Plateau. This newly emerged frontal structure refines considerably previous large-scale circulation schematics of the area.