首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   17727篇
  免费   2898篇
  国内免费   4857篇
测绘学   1428篇
大气科学   5879篇
地球物理   2714篇
地质学   5906篇
海洋学   1774篇
天文学   5335篇
综合类   844篇
自然地理   1602篇
  2024年   104篇
  2023年   265篇
  2022年   569篇
  2021年   701篇
  2020年   756篇
  2019年   969篇
  2018年   673篇
  2017年   760篇
  2016年   722篇
  2015年   872篇
  2014年   1172篇
  2013年   1256篇
  2012年   1232篇
  2011年   1340篇
  2010年   1255篇
  2009年   1563篇
  2008年   1429篇
  2007年   1465篇
  2006年   1319篇
  2005年   1115篇
  2004年   924篇
  2003年   818篇
  2002年   639篇
  2001年   577篇
  2000年   548篇
  1999年   470篇
  1998年   358篇
  1997年   231篇
  1996年   231篇
  1995年   208篇
  1994年   197篇
  1993年   166篇
  1992年   107篇
  1991年   99篇
  1990年   62篇
  1989年   58篇
  1988年   56篇
  1987年   15篇
  1986年   27篇
  1985年   33篇
  1984年   25篇
  1983年   18篇
  1982年   17篇
  1981年   11篇
  1980年   15篇
  1979年   4篇
  1978年   6篇
  1977年   16篇
  1954年   4篇
  1875年   1篇
排序方式: 共有10000条查询结果,搜索用时 156 毫秒
11.
12.
13.
14.
Optimal deflection of NEOs en route of collision with the Earth   总被引:1,自引:0,他引:1  
Ralph Kahle  Gerhard Hahn 《Icarus》2006,182(2):482-488
Recently, a method for the n-body analysis of the velocity change required to deflect a hazardous near-Earth object (NEO) was presented by Carusi et al. [Carusi, A., Valsecchi, G.B., D'Abramo, G., Boattini A., 2002. Icarus 159, 417-422]. We extent this method in order to optimize the velocity change vector instead of its along-track magnitude. From an application of both methods to a fictitious NEO we find Carusi's parallel approach to be reasonable for phases of unperturbed two-body motion. But, for orbit phases inhering third-body perturbations, i.e., for planetary close approaches or prior to a collision, the results obtained from the new method show the radial component of deflection impulse to play a major role. We show that a fivefold greater efficiency can be achieved by a deflection impulse being non-parallel to orbital velocity. The new method is applied to two possible 99942 Apophis impact trajectories in order to provide constraints for future Apophis deflection mission analysis.  相似文献   
15.
16.
17.
We present results from a new simulation code that accounts for the evolution of the reservoirs of carbon dioxide on Mars, from its early years to the present. We establish a baseline model parameter set that produces results compatible with the present (i.e., Patm?6.5 mbar with permanent CO2 ice cap) for a wide range of initial inventories. We find that the initial inventory of CO2 broadly determines the evolutionary course of the reservoirs of CO2. The reservoirs include the atmosphere, ice cap, adsorbed CO2 in the regolith, and carbonate rocks. We track the evolution of the free inventory: the atmosphere, ice cap and regolith. Simulations begin at 4.53 Gyr before present with a rapid loss of free inventory to space in the early Noachian. Models that assume a relatively small initial inventory (?5 bar) have pronounced minima in the free inventory of CO2 toward the end of the Noachian. Under baseline parameters, initial inventories below ∼4.5 bar result in a catastrophic loss of the free inventory to space. The current free inventory would be then determined by the balance between outgassing, sputtering losses and chemical weathering following the end of the late bombardment. We call these “thin” models. They generically predict small current free inventories in line with expectations of a small present CO2 ice cap. For “thick” models, with initial inventories ?5 bar, a surplus of 300-700 mbar of free CO2 remains during the late-Noachian. The histories of free inventory in time for thick models tend to converge within the last 3.5 Gyr toward a present with an ice cap plus atmospheric inventory of about 100 mbar. For thick models, the convergence is largely due to the effects of chemical weathering, which draws down higher free inventories more rapidly than the low. Thus, thick models have ?450 mbar carbonate reservoirs, while thin models have ?200 mbar. Though both thick and thin scenarios can reproduce the current atmospheric pressure, the thick models imply a relatively large current CO2 ice cap and thin models, little or none. While the sublimation of a massive cap at a high obliquity would create a climate swing of greenhouse warming for thick models, under the thin model, mean temperatures and pressures would be essentially unaffected by increases in obliquity.  相似文献   
18.
19.
20.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号