全文获取类型
收费全文 | 1541篇 |
免费 | 106篇 |
专业分类
公路运输 | 421篇 |
综合类 | 449篇 |
水路运输 | 426篇 |
铁路运输 | 303篇 |
综合运输 | 48篇 |
出版年
2024年 | 3篇 |
2023年 | 11篇 |
2022年 | 32篇 |
2021年 | 51篇 |
2020年 | 81篇 |
2019年 | 55篇 |
2018年 | 29篇 |
2017年 | 25篇 |
2016年 | 43篇 |
2015年 | 65篇 |
2014年 | 131篇 |
2013年 | 91篇 |
2012年 | 139篇 |
2011年 | 136篇 |
2010年 | 111篇 |
2009年 | 103篇 |
2008年 | 98篇 |
2007年 | 100篇 |
2006年 | 76篇 |
2005年 | 51篇 |
2004年 | 32篇 |
2003年 | 44篇 |
2002年 | 35篇 |
2001年 | 23篇 |
2000年 | 18篇 |
1999年 | 9篇 |
1998年 | 4篇 |
1997年 | 5篇 |
1996年 | 5篇 |
1995年 | 8篇 |
1994年 | 8篇 |
1993年 | 2篇 |
1992年 | 4篇 |
1991年 | 5篇 |
1990年 | 5篇 |
1989年 | 5篇 |
1988年 | 1篇 |
1987年 | 3篇 |
排序方式: 共有1647条查询结果,搜索用时 15 毫秒
71.
基于双时间层的有限差分方法(ADI),建立了水深平均二维浅水潮流数学模型,采用逆风格式和追赶法求解二维浅水方程,通过建立钦州湾二维潮流数值模型重现钦州湾的潮位和潮流变化状况。模拟结果与同步进行的岸边潮位及海上潮流的观测值校验结果表明,实测潮位资料与对应时间的计算结果吻合良好,实测潮流与对应时间的计算结果十分接近。模拟计算结果真实地反映钦州湾的潮位变化和潮流运动状况。钦州湾围滩工程实施前后的潮流场数值模拟研究结果表明该工程建设不会对海域水动力学条件产生较大影响。 相似文献
72.
73.
74.
75.
三维圆柱体绕流数值模拟流场选择及网格划分 总被引:2,自引:0,他引:2
文章通过数值模拟结果确定适合的三维圆柱体绕流流场的尺寸,采用不同的计算流体力学(CFD)软件对有限元模型进行网格划分,对比网格划分质量的优劣,选择适合数值模拟的软件CFX。确定采用的网格形式为六面体网格(Hex8)以及流场不同部分网格的尺寸。圆柱绕流展向各截面平均压力系数沿周向无明显变化,脉动压力系数变化显著,绕流后的旋涡发放形式具有明显的三维特性的数值模拟结果验证了本文的流场选择和网格化分尺度的合理性。 相似文献
76.
77.
78.
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
79.
80.