全文获取类型
收费全文 | 878篇 |
免费 | 98篇 |
国内免费 | 137篇 |
专业分类
测绘学 | 41篇 |
大气科学 | 8篇 |
地球物理 | 324篇 |
地质学 | 219篇 |
海洋学 | 377篇 |
天文学 | 24篇 |
综合类 | 30篇 |
自然地理 | 90篇 |
出版年
2024年 | 2篇 |
2023年 | 5篇 |
2022年 | 17篇 |
2021年 | 19篇 |
2020年 | 14篇 |
2019年 | 33篇 |
2018年 | 21篇 |
2017年 | 37篇 |
2016年 | 21篇 |
2015年 | 24篇 |
2014年 | 31篇 |
2013年 | 40篇 |
2012年 | 38篇 |
2011年 | 60篇 |
2010年 | 53篇 |
2009年 | 55篇 |
2008年 | 57篇 |
2007年 | 91篇 |
2006年 | 68篇 |
2005年 | 46篇 |
2004年 | 47篇 |
2003年 | 48篇 |
2002年 | 41篇 |
2001年 | 22篇 |
2000年 | 22篇 |
1999年 | 22篇 |
1998年 | 24篇 |
1997年 | 20篇 |
1996年 | 22篇 |
1995年 | 22篇 |
1994年 | 22篇 |
1993年 | 18篇 |
1992年 | 20篇 |
1991年 | 6篇 |
1990年 | 6篇 |
1989年 | 4篇 |
1988年 | 4篇 |
1987年 | 3篇 |
1986年 | 2篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1979年 | 1篇 |
排序方式: 共有1113条查询结果,搜索用时 31 毫秒
851.
利用不同年份的水深地形资料进行冲淤计算,结合实测水文泥沙、现场岸滩沉积地貌观察、新老海堤分布位置及以往浅地层探测和考古等资料综合分析发现,岸滩地貌形态从大约距今7 000 a前的一个古基岩港湾经受细颗粒泥沙长期不断地充填、淤积转化为近乎平直的岸段.在自然和人类活动的共同作用下,近370 a来海岸线以5.3 m/a的速度向海推移,潮滩以0.25 cm/a的速率沉积.近40余年来水下岸坡平均冲淤速率为-3.8~2.4 cm/a,横向冲淤调整有类似砂质海岸剖面塑造的特性,泥沙经受了在横向剖面"上部微淤、下部微冲"和纵向总体"东侧微冲、中西部微淤"的交替重复调整过程,目前朝着"上部微淤、下部微冲"的均衡剖面调整方向发展. 相似文献
852.
853.
854.
江苏近岸海域悬沙浓度的时空分布特征 总被引:9,自引:1,他引:9
2006—2007年间的四个季节在江苏近岸海域69个站位采集水样,获取悬沙浓度。通过对TM遥感数据反演,获取该海域四季大面悬沙浓度,并与调查的实测悬沙浓度进行对比。结果显示,大面调查的非同步数据基本可正确反映大区域悬沙浓度的季节与空间分布趋势。悬沙浓度等值线由高至低、由陆向海分布,底层浓度约为表层的2—3倍;废黄河口和长江口外海域为悬沙浓度高值区,而海州湾为低值分布区,东南部陆架区受台湾暖流影响出现低值中心。冬季整个海域悬沙浓度均较高,其次为春季,夏季最低;废黄河口海域的高值中心在不同季节分布位置有所移动。海底沉积物的再悬浮是苏北近岸悬沙最主要的来源,河流输沙量的季节变化是影响长江口海域悬沙浓度变化的关键因子。相关分析结果表明,潮流为影响悬沙浓度分布的主要控制因子;季风、风暴潮和风浪虽对悬沙的分布具有一定的影响,但冬季的低温环境是形成该季节整个海域悬沙浓度显著偏高的重要因素。 相似文献
855.
856.
红树林是全球极为重要的生态与环境资源, 在储存有机碳、增加滩面高程及防御海洋灾害等方面富有成效。然而, 因高强度人类活动与海面上升作用, 世界沿海红树林潮滩出现大规模损失。基于此, 本文从红树林消能及泥沙捕集、红树林潮滩生物地貌行为, 以及红树林潮滩对风暴潮与海面上升的响应三个方面, 对红树林潮滩沉积动力研究进行分析与回顾, 提出红树林潮滩沉积动力研究的关键问题应着重于红树林潮滩波流联合动力的衰减与潮滩动力、沉积、地貌及植被的耦合过程。此外, 针对全球沿海红树林生境的差异, 还应从区域尺度加强红树林潮滩沉积过程与驱动机制的研究。 相似文献
857.
Numerical simulation of tidal current and erosion and sedimentation in the Yangshan deep-water harbor of Shanghai 总被引:2,自引:1,他引:1
ZUO Shu-Hua ZHANG Ning-Chuan LI Bei ZHANG Zheng ZHU Zhi-Xia Ph.D c idate State Key Laboratory of Coastal Offshore Engineering Dalian University of Technology Dalian China Key Laboratory of Engineering Sediment of Ministry of Communications Tianjin Research Institute of Water Transport Engineering Tianjin China. Dr. Prof. China Research Scientist Key Labor... 《国际泥沙研究》2009,24(3):287-298
Yangshan near-shore sea area is the multi-island and multi-channel area with strong flow velocity and high suspended sediment concentration. Based on the characteristics of tidal currents, waves, and sediment in the Yangshan area, a two-dimensional numerical model of tidal currents, sediment transport, and sea bed deformation is developed. In the model, the effects of tidal currents and wind waves on sediment transport are considered. According to characteristics of the study area, unstructured grids are applied to fit the boundaries of the near-shore sea area. The results show that the calculated values are in good agreement with the measured data. The field of tidal currents, suspended sediment concentrations, and the deformation of the seabed can be successfully simulated. 相似文献
858.
Patrick L. Murphy Amy F. Waterhouse Tyler J. Hesser Allison M. Penko Arnoldo Valle-Levinson 《Continental Shelf Research》2009
Spatial and temporal variability of the subtidal exchange flow at West Pass, an inlet at the entrance to a subtropical lagoon (St. Andrew Bay, Florida), was studied using moored and towed current velocity profiles and hydrographic data. Towed and hydrographic measurements were captured over one diurnal tidal cycle to determine intratidal and spatial changes in flow. Hydrographic profiles over the tidal cycle showed that tidal straining modified density stratification asymmetrically, thus setting up the observed mean flow within the inlet. During the towed survey, the inlet's mean flow had a two-layer exchange structure that was moderately frictional and weakly influenced by Coriolis accelerations. Moored current profiles revealed the additional contribution to the dynamics from centrifugal accelerations. Along channel residual flows changed between unidirectional and exchange flow, depending on the forcing from the along-estuary wind stress and, to a lesser extent, the spring–neap tidal cycle. Increases in vertical shear in the along channel subtidal flow coincided with neap tides and rain pulses. Lateral subtidal flows showed the influence on the dynamics of centrifugal accelerations through a well-developed two-layer structure modulated in magnitude by the spring–neap tidal cycle. 相似文献
859.
Modeling the tidal channel morphodynamics in a macro-tidal embayment,Hangzhou Bay,China 总被引:2,自引:0,他引:2
The Hangzhou Bay is a macro-tidal bay located to the south of the Changjiang estuary in China. Along its northern shore, a large-scale tidal channel system has developed, which includes a main northern tidal channel, with a length of more than 50 km and a width up to 10 km, and a secondary southern tidal channel. A process-based morphodynamic model, incorporating the cohesive sediment transport module of Delft3D, is used to analyze the physical processes and mechanisms underlying the formation and evolution of this tidal channel system. The results show that spatial gradients of flood dominance, caused by boundary enhancement via current convergences, is responsible for the formation of the channel system, due to a combination of the various factors such as funnel-shaped geometry hindering associated with the presence of islands, and flow deviation by the southern tidal flat and so on. The model results agree well with the real morphological features. This study also indicates that the reclamation of the southern tidal flat imposes a profound influence on the morphological evolution of the tidal channel system in the Hangzhou Bay. It is feasible to use the model to simulate long-term estuarine morphological changes with cohesive sediment settings. 相似文献
860.