全文获取类型
收费全文 | 4747篇 |
免费 | 567篇 |
国内免费 | 574篇 |
专业分类
测绘学 | 1579篇 |
大气科学 | 498篇 |
地球物理 | 878篇 |
地质学 | 1225篇 |
海洋学 | 462篇 |
天文学 | 154篇 |
综合类 | 514篇 |
自然地理 | 578篇 |
出版年
2024年 | 7篇 |
2023年 | 47篇 |
2022年 | 123篇 |
2021年 | 149篇 |
2020年 | 192篇 |
2019年 | 188篇 |
2018年 | 132篇 |
2017年 | 225篇 |
2016年 | 220篇 |
2015年 | 221篇 |
2014年 | 244篇 |
2013年 | 307篇 |
2012年 | 365篇 |
2011年 | 335篇 |
2010年 | 278篇 |
2009年 | 302篇 |
2008年 | 308篇 |
2007年 | 375篇 |
2006年 | 283篇 |
2005年 | 241篇 |
2004年 | 231篇 |
2003年 | 203篇 |
2002年 | 149篇 |
2001年 | 126篇 |
2000年 | 123篇 |
1999年 | 94篇 |
1998年 | 103篇 |
1997年 | 56篇 |
1996年 | 56篇 |
1995年 | 35篇 |
1994年 | 27篇 |
1993年 | 40篇 |
1992年 | 27篇 |
1991年 | 16篇 |
1990年 | 15篇 |
1989年 | 11篇 |
1988年 | 7篇 |
1987年 | 10篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1980年 | 3篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1976年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有5888条查询结果,搜索用时 609 毫秒
211.
变形预测在预报工程险情方面起着关键性的作用,针对施工中需及时、准确地预测变形的问题,本文利用小波变换原理对监测数据进行降噪处理,并采用BP神经网络分析不同训练样本下的预测效果和精度水平。实验结果表明:基于小波消噪后的BP网络模型,以连续的近期观测数据作为训练样本,对下期变形预测精度高,效果好,相对误差很小。因此,小波变换和BP神经网络模型在沉降变形监测工程中能作为预测研究与应用的参考。 相似文献
212.
针对工程实践中不同坐标系下DWG数据相互变换的实际需要,通过对DWG数据存储组织结构以及AutoCAD.NET API的深入研究,采用平面四参数转换方法,基于Visual Studio 2010和AutoCAD 2008开发平台,成功开发了DWG数据坐标变换程序。以沈阳市1∶500比例尺、1954北京坐标系的DWG数据为例,实现了不同坐标系下DWG数据的互相变换,并对变换后的数据进行了要素检查和精度分析。结果证明,采用基于AutoCAD.NET API二次开发的技术能够很好地满足DWG数据在不同坐标系下互相变换的应用需求,大大地节省了工作时间,提高了工作效率。 相似文献
213.
214.
珠江口盆地珠一坳陷在中始新世裂陷期文昌组沉积早、晚期之间存在明显的构造转换,该构造事件对古近系源?汇体系的形成和演变有重大影响.基于研究区地震、钻井、测井等资料的综合分析,本文认为构造转换控制了裂陷期源?汇体系的盆山地貌、物源供给、搬运方向及沉积样式等基本要素,并影响深层古近系储层条件.而且在构造转换的制约下,研究区发... 相似文献
215.
216.
Using wavelet analysis, regression analysis and the Mann-Kendall test, this paper analyzed time-series (1959–2006) weather
data from 23 meteorological stations in an attempt to characterize the climate change in the Tarim River Basin of Xinjiang
Uygur Autonomous Region, China. Major findings are as follows: 1) In the 48-year study period, average annual temperature,
annual precipitation and average annual relative humidity all presented nonlinear trends. 2) At the 16-year time scale, all
three climate indices unanimously showed a rather flat before 1964 and a detectable pickup thereafter. At the 8-year time
scale, an S-shaped nonlinear and uprising trend was revealed with slight fluctuations in the entire process for all three
indices. Incidentally, they all showed similar pattern of a slight increase before 1980 and a noticeable up-swing afterwards.
The 4-year time scale provided a highly fluctuating pattern of periodical oscillations and spiral increases. 3) Average annual
relative humidity presented a negative correlation with average annual temperature and a positive correlation with annual
precipitation at each time scale, which revealed a close dynamic relationship among them at the confidence level of 0.001.
4) The Mann-Kendall test at the 0.05 confidence level demonstrated that the climate warming trend, as represented by the rising
average annual temperature, was remarkable, but the climate wetting trend, as indicated by the rising annual precipitation
and average annual relative humidity, was not obvious. 相似文献
217.
218.
The sensitivity of the North Atlantic gyre circulation to high latitude buoyancy forcing is explored in a global, non-eddy resolving ocean general circulation model. Increased buoyancy forcing strengthens the deep western boundary current, the northern recirculation gyre, and the North Atlantic Current, which leads to a more realistic Gulf Stream path. High latitude density fluxes and surface water mass transformation are strongly dependent on the choice of sea ice and salinity restoring boundary conditions. Coupling the ocean model to a prognostic sea ice model results in much greater buoyancy loss in the Labrador Sea compared to simulations in which the ocean is forced by prescribed sea ice boundary conditions. A comparison of bulk flux forced hindcast simulations which differ only in their sea ice and salinity restoring forcings reveals the effects of a mixed thermohaline boundary condition transport feedback whereby small, positive temperature and salinity anomalies in subpolar regions are amplified when the gyre spins up as a result of increased buoyancy loss and convection. The primary buoyancy flux effects of the sea ice which cause the simulations to diverge are ice melt, which is less physical in the diagnostic sea ice model, and insulation of the ocean, which is less physical with the prognostic sea ice model. Increased salinity restoring ensures a more realistic net winter buoyancy loss in the Labrador Sea, but it is found that improvements in the Gulf Stream simulation can only be achieved with the excessive buoyancy loss associated with weak salinity restoring. 相似文献
219.
220.