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131.
132.
应用GAO-YONG可压缩湍流模式,数值模拟了NACA0012,RAE2822翼型的定常跨音速粘流算例.对流项采用三阶ROE格式,扩散项采用二阶中心格式,用多步Runge-Kutta显式时间推进法求解空间离散后的控制方程.计算结果很好地预测了翼型表面的压力系数的分布、激波的位置、马赫数等值线的分布等情况,并且对翼型表面激波与边界层相互干扰以及层流向湍流的转捩问题进行了分析计算.计算结果与实验值符合很好,表明GAO-YONG可压缩湍流模式应用合适的计算方法能够高精度模拟翼型跨音粘性流动问题,并且基于GAO-YONG可压缩湍流模式各向异性湍流粘性的机理,提供了一种预测转捩起始位置的判别方法. 相似文献
133.
134.
本文研究了以平衡攻角为中心作单自由度俯仰振荡的飞船返回舱,其动态稳定形态随来流M∞的变化.设θ(t)是由平衡攻角起算的俯仰振荡角,Cm是作用在飞船返回舱上的气动俯仰力矩系数,Cμ(θ,)是机械阻尼力矩(自由飞行时为零,实验时要计入其影响),文中给出飞船返回舱在平衡攻角处的俯仰振荡动态稳定性判据,并证明λ=λ(M∞)=(Cm)/()0+Cμ(0,0)1-(Cm)/(O)0是决定动稳定形态的重要参数.如果随M∞的变化,λ(M∞)由λ<0经过λ=0变化到λ>0,则飞船返回舱将由稳定的点吸引子形态(即稳定在平衡攻 相似文献
135.
Wei Yuan Jiyao Xu Yongfu Wu Jianchun Bian Hongbin Chen 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2009
Vertical profiles of ozone have been measured at balloon altitudes. Our purpose is to examine the character of vertical wavenumber spectra of ozone fluctuations, to assess the possible roles of gravity wave field in ozone fluctuations, and to determine dominant vertical wavelengths of ozone spectra. Vertical wavenumber spectra of 12 ozone fluctuations obtained during June–August 2003 are presented. Results indicate that mean spectral slopes in the wavenumber range from 4.69 × 10−4 to 2.50 × 10−3 cyc/m are about −2.91 in the troposphere and −2.87 in the lower stratosphere, which is close to the slope of −3 predicted by current gravity wave saturation models. The consistency of the observed spectral slopes with the value of −3 predicted by current gravity wave saturation models suggests that the observed ozone fluctuations are due primarily to atmospheric gravity waves. At m = 1/(1000 m) the mean spectral amplitude is over 30 times larger in the lower stratosphere than in the troposphere. Mean vertical wavenumber spectra in area-preserving form reveal dominant vertical wavelengths of ∼2.6 km in the troposphere and ∼2.7 km in the lower stratosphere, which is consistent with the values varying between 1.5 and 3.0 km estimated from the velocity field and temperature field at these heights. 相似文献
136.
A. Borgazzi A. Lara G. Paz J.P. Raulin 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2014
In order to detect and study the ionospheric response to solar flares (transient high energy solar radiation), we have constructed a radio receiver station at Mexico City, which is part of the “Latin American Very low frequency Network” (LAVNet-Mex). This station extends to the northern hemisphere the so called “South American VLF Network”. 相似文献
137.
本文分析了在新乡、兰州两地接收Omega导航系统G台的信号。结果表明,测出的相让周期丢失是VLP远距离传播所具有的传播现象。同时,结合在兰州的测试结果,进一步分析了产生这种传播现象的原因。 相似文献
138.
K. Andreov L. Pech 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2007,40(12):1871-1880
This paper is devoted to the study of propagation of disturbances caused by interplanetary shocks (IPS) through the Earth’s magnetosphere. Using simultaneous observations of various fast forward shocks by different satellites in the solar wind, magnetosheath and magnetosphere from 1995 till 2002, we traced the interplanetary shocks into the Earth’s magnetosphere, we calculated the velocity of their propagation into the Earth’s magnetosphere and analyzed fronts of the disturbances. From the onset of disturbances at different satellites in the magnetosphere we obtained speed values ranging from 500 to 1300 km/s in the direction along the IP shock normal, that is in a general agreement with results of previous numerical MHD simulations. The paper discusses in detail a sequence of two events on November 9th, 2002. For the two cases we estimated the propagation speed of the IP shock caused disturbance between the dayside and nightside magnetosphere to be 590 km/s and 714–741 km/s, respectively. We partially attributed this increase to higher Alfven speed in the outer magnetosphere due to the compression of the magnetosphere as a consequence of the first event, and partially to the faster and stronger driving interplanetary shock. High-time resolution GOES magnetic field data revealed a complex structure of the compressional wave fronts at the dayside geosynchronous orbit during these events, with initial very steep parts (10 s). We discuss a few possible mechanisms of such steep front formation in the paper. 相似文献
139.
应用钠原子和中性大气分子的质量连续性方程来模拟突发钠层(SSL),垂直风场采用接近实际大气重力波的正弦行波模式,结果较好地反映了SSL的形成过程.SSL的形成时刻在5-15min之间并可持续到30min之后,形成高度大约在90-100km之间,峰宽为0.5-2km之间,这些都与实际观测SSL的特点相符.同时还进一步地研究了当重力波参数(主要指垂直波长和周期)、风速以及常态钠层半宽度发生变化时SSL的变化趋势. 相似文献
140.
在二维四边形结构网格下,针对时空守恒元和解元(CE/SE, space-time Conservation Element and Solution Element)方法捕捉激波需要双倍空间网格点的问题,重新对守恒元和解元进行了定义,计算点同时包含单元中心和网格节点,并推导得到了新的CE/SE方法的计算公式.以此为基础,结合非敏感克朗数(CNIS, Courant Number Insensitive Scheme)计算格式和当地时间步长方法,对激波翼型流场进行数值模拟,并与原方法及AGARD报告进行对比.结果表明,对原CE/SE方法的改进是有效的,可明显提高激波分辨能力,并且激波前后无明显的数值震荡发生,新方法适合应用于翼型流场中捕捉激波. 相似文献