外加电流阴极保护技术在天津港滚装码头预制梁中的应用

外加电流阴极防护是钢筋混凝土结构防腐蚀的主要技术手段之一。文章结合外加电流阴极保护技术在天津港滚装码头预制梁工程中的实际应用,介绍了外加电流阴极保护的原理和保护效果,是国内工程中的首次应用,将为我国今后外加电流阴极防护技术的发展和进步提供重要的参考和借鉴。     

嵌入式ARM-Linux系统在便携式测流仪中的应用研究

随着嵌入式技术不断发展，微处理器已被应用于各种电子仪器的设计当中。近年来，ARM嵌入式微处理器技术发展迅速，并以其高性能，低功耗的特性成为嵌入式领域应用最广泛的32位微处理器。本课题将ARM微处理器技术率先引入到测流仪器的设计中来，采用基于ARM920T内核的AT91RM9200微处理器作为系统CPU；同时在软件方面，采用功能强大而源码免费开放的Linux系统，组成了基于ARM微处理器的Linux系统（简称ARM-Linux系统），并对这种先进的嵌入式系统在多普勒测流仪中的应用进行了研究，以期提高多普勒测流仪的整体性能。     

Eddies around Madagascar — The retroflection re-considered

The Agulhas Current with its retroflection and attendant eddy-shedding is the cause of some of the greatest mesoscale variability in the ocean. This paper considers the area to the south and east of Madagascar, which provides some of the source waters of the Agulhas Current, and examines the propagating sea surface height signals in altimetry and output from a numerical model, OCCAM. Both show bands of variability along the axis of the East Madagascar Current (EMC) and along a zonal band near 25°S. Sequences of images plus associated temperature data suggest that a number of westward-propagating eddies are present in this zonal band. The paper then focuses on the region to the south of the island, where ocean colour and infra-red imagery are evocative of an East Madagascar Retroflection. The synthesis of data analysed in this paper, however, shows that remotely observed features in this area can be explained by anticyclonic eddies moving westward through the region, and this explanation is consistent with numerical model output and the trajectories of drifting buoys.     

微机监测信号机点灯电流案例分析

微机监测已成为监测信号设备运用状况的主要手段。通过对微机监测采集的信号机点灯电流典型曲线进行分析,达到监测和预防的目的。     

汽车精密成型技术现状与发展趋势刍议

简述了汽车精密成型技术的内涵、特点及其在汽车制造中的地位，较深入地分析了目前国内外精密冲压、精密铸造、精密锻造和精密焊接技术等汽车精密成型技术的发展现状，并指出汽车精密成型未来发展的主要趋势。     

军用半挂汽车列车的现状和发展趋势

介绍了国内外军用半挂汽车列车的发展现状,根据军用半挂汽车列车的运载对象和使用环境,分析了其性能特点、关键技术和发展趋势.     

船舶配电系统交流智能配电关键技术研究

本文首先论述了船舶交流配电系统的发展需求,然后重点研究了船舶配电系统交流智能配电的关键技术,包括限流判断控制策略、短路故障判断策略及冲击性负载引起限流后解除限流的判断策略,最后通过原理样机,验证了船舶配电系统交流智能配电关键技术解决途径的可行性。     

海上水声信号处理算法中的物理特性仿真研究

通过研究海上水声信号的产生和海上水声信号定位系统的构成,设计水声信号处理系统流程,指出陆地上的主控中心与水中的基站如何进行信号数据传递,以及环境噪声、传输损耗、多径传输、多普勒效应等物理特性对信号偏移产生何种影响。最后通过实验验证加入消除滤波器后可以有效地控制多普勒效应产生的频率偏移。     

某雷达信号处理机的设计

信号处理是雷达系统的重要组成部分,其作用是从回波信号中提取有用信号。文章介绍了某搜索雷达信号处理机的结构及功能实现。     

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.