全文获取类型
收费全文 | 1245篇 |
免费 | 106篇 |
国内免费 | 38篇 |
专业分类
航空 | 235篇 |
航天技术 | 952篇 |
综合类 | 29篇 |
航天 | 173篇 |
出版年
2024年 | 4篇 |
2023年 | 33篇 |
2022年 | 12篇 |
2021年 | 63篇 |
2020年 | 49篇 |
2019年 | 51篇 |
2018年 | 46篇 |
2017年 | 20篇 |
2016年 | 18篇 |
2015年 | 20篇 |
2014年 | 92篇 |
2013年 | 61篇 |
2012年 | 67篇 |
2011年 | 95篇 |
2010年 | 77篇 |
2009年 | 99篇 |
2008年 | 94篇 |
2007年 | 57篇 |
2006年 | 33篇 |
2005年 | 78篇 |
2004年 | 30篇 |
2003年 | 18篇 |
2002年 | 21篇 |
2001年 | 24篇 |
2000年 | 25篇 |
1999年 | 21篇 |
1998年 | 28篇 |
1997年 | 25篇 |
1996年 | 15篇 |
1995年 | 20篇 |
1994年 | 36篇 |
1993年 | 13篇 |
1992年 | 17篇 |
1991年 | 10篇 |
1990年 | 10篇 |
1989年 | 5篇 |
1987年 | 1篇 |
1986年 | 1篇 |
排序方式: 共有1389条查询结果,搜索用时 15 毫秒
51.
Yuri N. Kulikov Helmut Lammer Herbert I. M. Lichtenegger Thomas Penz Doris Breuer Tilman Spohn Rickard Lundin Helfried K. Biernat 《Space Science Reviews》2007,129(1-3):207-243
Because the solar radiation and particle environment plays a major role in all atmospheric processes such as ionization, dissociation,
heating of the upper atmospheres, and thermal and non-thermal atmospheric loss processes, the long-time evolution of planetary
atmospheres and their water inventories can only be understood within the context of the evolving Sun. We compare the effect
of solar induced X-ray and EUV (XUV) heating on the upper atmospheres of Earth, Venus and Mars since the time when the Sun
arrived at the Zero-Age-Main-Sequence (ZAMS) about 4.6 Gyr ago. We apply a diffusive-gravitational equilibrium and thermal
balance model for studying heating of the early thermospheres by photodissociation and ionization processes, due to exothermic
chemical reactions and cooling by IR-radiating molecules like CO2, NO, OH, etc. Our model simulations result in extended thermospheres for early Earth, Venus and Mars. The exospheric temperatures
obtained for all the three planets during this time period lead to diffusion-limited hydrodynamic escape of atomic hydrogen
and high Jeans’ escape rates for heavier species like H2, He, C, N, O, etc. The duration of this blow-off phase for atomic hydrogen depends essentially on the mixing ratios of CO2, N2 and H2O in the atmospheres and could last from ∼100 to several hundred million years. Furthermore, we study the efficiency of various
non-thermal atmospheric loss processes on Venus and Mars and investigate the possible protecting effect of the early martian
magnetosphere against solar wind induced ion pick up erosion. We find that the early martian magnetic field could decrease
the ion-related non-thermal escape rates by a great amount. It is possible that non-magnetized early Mars could have lost
its whole atmosphere due to the combined effect of its extended upper atmosphere and a dense solar wind plasma flow of the
young Sun during about 200 Myr after the Sun arrived at the ZAMS. Depending on the solar wind parameters, our model simulations
for early Venus show that ion pick up by strong solar wind from a non-magnetized planet could erode up to an equivalent amount
of ∼250 bar of O+ ions during the first several hundred million years. This accumulated loss corresponds to an equivalent mass of ∼1 terrestrial
ocean (TO (1 TO ∼1.39×1024 g or expressed as partial pressure, about 265 bar, which corresponds to ∼2900 m average depth)). Finally, we discuss and
compare our findings with the results of preceding studies. 相似文献
52.
V. S. Heber R. C. Wiens D. B. Reisenfeld J. H. Allton H. Baur D. S. Burnett C. T. Olinger U. Wiechert R. Wieler 《Space Science Reviews》2007,130(1-4):309-316
The concentrator on Genesis provided samples of increased fluences of solar wind ions for precise determination of the oxygen
isotopic composition. The concentration process caused mass fractionation as a function of the radial target position. This
fractionation was measured using Ne released by UV laser ablation and compared with modelled Ne data, obtained from ion-trajectory
simulations. Measured data show that the concentrator performed as expected and indicate a radially symmetric concentration
process. Measured concentration factors are up to ∼30 at the target centre. The total range of isotopic fractionation along
the target radius is 3.8%/amu, with monotonically decreasing 20Ne/22Ne towards the centre, which differs from model predictions. We discuss potential reasons and propose future attempts to overcome
these disagreements. 相似文献
53.
本文通过三维数值模拟研究蓄热式太阳能热光伏-热推进双模系统的蓄/释热特性和推进性能。在蓄热式太阳能热推进系统工程模型的基础上,通过射线光学的光路分析验证了聚光器设计的合理性,并获得吸热腔壁面能量分布情况,进一步研究了相变蓄热过程的影响因素。基于场协同原理对热光伏再生冷却结构进行了优化设计,使热光伏具有较好的散热特性,提高发电功率;通过整机流动换热仿真,分析了工质流体在推进器内部的换热情况,计算结果表明,蓄热式热推进器具有达到734s比冲和0.9N推力的推进性能,以及能够满足日蚀区微小卫星的供电和推力需求。 相似文献
54.
55.
为满足某型光电经纬仪的使用要求,设计了某绝对式恒光源 24位光电轴角编码器分系统。该编码器采用 16位绝对式光学码盘,码盘刻划有粗码道、通圈码道、中精码道和精码道。精码道的线对数为 16 384(14位)。方位和高低编码器的处理电路设计在一块电路板上,采用一片 DSP为主机,6个读数头输出 64路码盘光电信号分别经放大整形、A/D转换输入至 DSP。DSP完成数据采集、细分、译码、校正等处理,把轴的转角变换成 24位自然二进制角度代码输出和上传。使用情况表明:该编码器的光机结构布局合理、性能稳定,电路板和元器件少、操作简单、测角精度高,满足某型光电经纬仪对于编码器系统的要求,具有较高的实用价值。 相似文献
56.
根据准线性方程,求出了在离子持续产生并被太阳风捕获加速的情况下离子的渐近态分布函数.采用此分布函数分析了斜向传播的Alfven波的稳定性. 相似文献
57.
本文讨论了观测频率为232MHz和327MHz时,利用互谱的方法估计太阳风速度的可能性、考虑路径积分效应,结果表明在17°≤ε≤50°范围内,对于几种可能的太阳风速度分布,由互谱所得结果与太阳风速度值差别小于15%. 相似文献
58.
文章简要地叙述碳纤维复合材料刚性太阳电池阵基板的结构设计,理论分析,模态试验和振动试验。理论分析和试验结果比较一致。通过试验还解决了基板各种复合材料的力学性能测试问题,取得了必要的数据。 相似文献
59.
研究了基于RBF(Redial Basis Function)神经网络的结构光三维视觉检测方法.该方法利用RBF网络良好的非线性映射能力以及学习、泛化能力,通过所获取的高精度的样本数据来训练RBF网络,最终建立起了用于结构光三维视觉检测的RBF网络模型.与常规方法相比,该方法不需要考虑视觉模型误差、光学调整误差等因素对视觉检测系统测量精度的影响,因而能够有效的克服常规建模方法的不足,保证了检测系统具有较高的精度. 相似文献
60.
E. Echer W.D. Gonzalez A. Dal Lago L.E.A. Vieira F.L. Guarnieri A.L.C. Gonzalez N.J. Schuch 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2005,36(12):2313-2317
In this work a study is performed on the correlation between fast forward interplanetary shock parameters at 1 Astronomical Unit and sudden impulse (SI) amplitudes in the H-component of the geomagnetic field, for periods of solar activity maximum (year 2000) and minimum (year 1995–1996). Solar wind temperature, density and speed, and total magnetic field, were taken to calculate the static pressures (thermal and magnetic) both in the upstream and downstream sides of the shocks. The variations of the solar wind parameters and pressures were then correlated with SI amplitudes. The solar wind speed variations presented good correlations with sudden impulses, with correlation coefficients larger than 0.70 both in solar maximum and solar minimum, whereas the solar wind density presented very low correlation. The parameter better correlated with SI was the square root dynamic pressure variation, showing a larger correlation during solar maximum (r = 0.82) than during solar minimum (r = 0.77). The correlations of SI with square root thermal and magnetic pressure were smaller than with the dynamic pressure, but they also present a good correlation, with r > 0.70 during both solar maximum and minimum. Multiple linear correlation analysis of SI in terms of the three pressure terms have shown that 78% and 85% of the variance in SI during solar maximum and minimum, respectively, are explained by the three pressure variations. Average sudden impulse amplitude was 25 nT during solar maximum and 21 nT during solar minimum, while average square root dynamic pressure variation is 1.20 and 0.86 nPa1/2 during solar maximum and minimum, respectively. Thus on average, fast forward interplanetary shocks are 33% stronger during solar maximum than during solar minimum, and the magnetospheric SI response has amplitude 20% higher during solar maximum than during solar minimum. A comparison with theoretical predictions (Tsyganenko’s model corrected by Earth’s induced currents) of the coefficient of sudden impulse change with solar wind dynamic pressure variation showed excellent agreement, with values around 17 nT/nPa1/2. 相似文献