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液压转向系统冷启动沉故障在北方冬季是比较常见的一个故障,论文针对故障产生的机理进行了深入分析,并对产生故障的常见原因及改进方法进行了简单介绍,最后对如何确定故障源从测试方面提供了方法. 相似文献
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深圳北站交通枢纽功能齐全、接口复杂。结合北站枢纽的建设实践,通过分析交通枢纽各交通功能的建设规模、主次地位和换乘关系,提出"功能布局立体化和流线组织管道化"的设计理念。通过集约化的方式统筹规划建设,充分利用有限的土地资源,拓展城市发展空间,形成功能齐全、运营高效、换乘便捷的综合交通枢纽。自2011年6月建成投入使用以来,客流快速增长,换乘方便,步行距离短,服务设施齐全,各方评价较高。全面阐述其相关原则、重点、要求和具体措施等设计实践,为其他交通枢纽的规划设计提供参考和借鉴。 相似文献
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Hydrographic cruises off northwest Africa: the Canary Current and the Cape Ghir region 总被引:3,自引:0,他引:3
J.L. Pelegrí A. Marrero-Díaz A. Ratsimandresy A. Antoranz J. Cisneros-Aguirre C. Gordo D. Grisolía A. Hernndez-Guerra I. Liz A. Martínez G. Parrilla P. Prez-Rodríguez A. Rodríguez-Santana P. Sangr 《Journal of Marine Systems》2005,54(1-4):39
We present hydrographic data for several sections located along the African coastline and off Cape Ghir, carried out at times of weak surface winds (October 1995 and September 1997). The main sections are near the continental slope, at mean distances between 100 and 150 km from the coastline. North of Cape Ghir (31°N) the geostrophic transport (referenced to 650 m) of North Atlantic Central Water through these sections is 3.7 and 2.0 Sv for 1995 and 1997, respectively. This confirms that a major fraction of the water transport by the Canary Current flows east, into the continental slope off northwest Africa, at latitudes above Cape Ghir. Most of this flow continues south past Cape Ghir, along the coast and probably through the eastern passages of the Canary Archipelago. A significant fraction, however, may escape through surface Ekman transport (0.3–0.5 Sv during the early fall season) and by offshore flow at Cape Ghir (1.1 Sv in September 1997, referenced to 650 m). Despite the weak winds the Cape Ghir filament was clearly visible, characterized by localized coastal upwelling associated to a cyclonic shallow structure and cold (and fresh) waters stretching offshore as a very shallow feature (50–100 m deep). The satellite images show that the surface temperature field is highly variable, in rapid response to the surface winds, always with a core region of relatively cold water and commonly with one or two associated eddies. Our results support the existence of two recirculation cells in the area: a horizontal one that connects the interior eastern boundary currents with the coastal region and a vertical one related to both wind-induced and filament upwelling. The data also show a salinity subsurface maximum at the root of the filament, linked to water inflow from northern latitudes, and a subsurface anticyclonic eddy over the Agadir canyon, likely related to the poleward slope undercurrent. 相似文献
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北美铁路降低轮轨接触应力新进展 总被引:2,自引:0,他引:2
介绍了北美铁路在降低轮轨接触应力和轮轨作用力方面的研究成果. 相似文献
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Observations of the Fawn Trough Current over the Kerguelen Plateau from instrumented elephant seals 总被引:2,自引:1,他引:1
Fabien Roquet Young-Hyang Park Christophe Guinet Frdric Bailleul Jean-Benoît Charrassin 《Journal of Marine Systems》2009,78(3):377
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. 相似文献
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基于考虑水体斜压的MIKE3数值模型的HD模块和Ecolab模块,对长江口及附近海域水动力环境进行数值模拟,并将验证好的模型用于分析预测实施北支中束窄工程对周边水动力环境造成的影响。研究结果表明:中束窄工程围填后,北支流速均有一定程度的降低,北支上段汊口处受到南支涨潮的影响,涨急流速有增大趋势;北支束窄工程对盐度的影响趋势为北支区域盐度值有明显的降低,对枯季北支的盐度倒灌南支起到了明显的控制作用;工程实施后,北支河口处磷酸盐、无机氮与叶绿素a含量增加明显;北支中上段磷酸盐与无机氮平均浓度略有降低,而叶绿素a含量整体有上升趋势。工程围填对南支及外海区域的水动力特征及营养盐含量影响较小。 相似文献
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