全文获取类型
收费全文 | 1181篇 |
免费 | 224篇 |
国内免费 | 283篇 |
专业分类
测绘学 | 96篇 |
大气科学 | 232篇 |
地球物理 | 382篇 |
地质学 | 378篇 |
海洋学 | 220篇 |
天文学 | 30篇 |
综合类 | 55篇 |
自然地理 | 295篇 |
出版年
2024年 | 2篇 |
2023年 | 14篇 |
2022年 | 30篇 |
2021年 | 28篇 |
2020年 | 52篇 |
2019年 | 58篇 |
2018年 | 52篇 |
2017年 | 46篇 |
2016年 | 47篇 |
2015年 | 67篇 |
2014年 | 77篇 |
2013年 | 65篇 |
2012年 | 56篇 |
2011年 | 53篇 |
2010年 | 46篇 |
2009年 | 57篇 |
2008年 | 117篇 |
2007年 | 86篇 |
2006年 | 84篇 |
2005年 | 60篇 |
2004年 | 50篇 |
2003年 | 66篇 |
2002年 | 60篇 |
2001年 | 48篇 |
2000年 | 46篇 |
1999年 | 47篇 |
1998年 | 50篇 |
1997年 | 38篇 |
1996年 | 37篇 |
1995年 | 24篇 |
1994年 | 35篇 |
1993年 | 17篇 |
1992年 | 14篇 |
1991年 | 14篇 |
1990年 | 13篇 |
1989年 | 6篇 |
1988年 | 7篇 |
1987年 | 2篇 |
1986年 | 7篇 |
1985年 | 3篇 |
1984年 | 1篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
1973年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有1688条查询结果,搜索用时 93 毫秒
21.
The generation and propagation of surface waves resulting from suddenly created disturbances over water surfaces is investigated. The initial boundary conditions defining the disturbance are given either by a velocity of the free surface, an initial elevation of the free surface or a pressure impulsively applied on the free surface. It is shown that the corresponding three forms of solutions are related by a simple time derivative. Linear solutions are obtained in the cases where the wave motion is assumed to be nondispersive, mildly dispersive and fully dispersive, as well as in the case where the motion is given by the method of stationary phase. Criteria are established to indicate the limit of validity of each method. 相似文献
22.
介绍了次声波的基本物理概念和次声波的传播特性,概述了次声波的研究现状,提出了利用次声波来预警海啸灾害的建议,并对其可行性进行了分析。 相似文献
23.
用一种新方法研究了三对角方程组及对称三对角方程组计算解的最佳向后扰动分析。由于这两类方程组的系数矩阵具有特殊结构 ,因而本文结果不能从已有结果直接导出。所用方法亦可用于研究 KKT及 SQD等结构线性系统的最佳向后扰动分析。 相似文献
24.
基于AHP和BP神经网络的深部地热水可持续开发能力评价 总被引:1,自引:0,他引:1
采用资料完整性、开采潜力、回灌量、平均水压下降速率、地面沉降速率、水温、水质、地热井布局8项指标构建天津地热可持续开发能力评价指标体系;运用层次分析法确定了各项指标的权重,建立起评价因素集和评语集,给出了归一化数值;建立了天津地热可持续开发能力的BP神经网络模型,以层次分析法得出的结果作为样本,对BP网络进行了训练和测试,实例评价结果表明了AHP和BP神经网络方法的可行性,为地热资源的可持续开发能力评价提供了一种新的评价方法。 相似文献
25.
Numerical studies using the displacement discontinuity method show that a single shear crack under compression propagates in its own direction, because such propagation results in the maximum release of strain energy. The methods of linear elastic fracture mechanics may not be used for such a closed crack, and the stress intensity factors are meaningless in that case. Laboratory observations of propagation by means of kinks at an angle of approximately 70° to the crack may be due to heterogeneities, to the effect of a preexisting crack, to end effects, to microcracking, or to some combination of these factors. Such kinks may thus be local phenomena which cannot release most of the strain energy, and are not incompatible with our numerical results which are based on a global energy balance. 相似文献
26.
M. Varvayanni C. G. Helmis G. T. Amanatidis D. N. Asimakopoulos J. G. Bartzis A. Soilemes K. H. Papadopoulos H. D. Kambezidis 《Pure and Applied Geophysics》1993,140(4):681-720
Field measurements of wind, air temperature and humidity were taken at the eastern part of the Attika district in June 1991, to examine the topographic influences exerted on the local sea breezes. These influences are due either to the elongated Evia island, faced by the northern half of Attica coastline some tens of kilometers offshore, or to the coast-parallel range of Hymettos mountain, rising steeply 12 km onshore. The instrumentation consisted mainly of three tethered meteorological balloons released at characteristic sires (i.e., the coast, a location between shoreline and mountain foot and the mountain top) and three autographic ground-based anemometers operating at selected locations. Data from the ground-based and upper air stations of the Hellenic National Meteorological Service, as well as the diurnal weather maps were also obtained and analyzed. Observations were made under different synoptic wind and the latter was found to determine remarkably the significance of the topographic effects. A preliminary two-dimensional numerical approach was also made concerning the sea breeze capability to reach the Hymettos mountain top in the case of a weak opposing geostrophic flow. 相似文献
27.
28.
29.
30.