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141.
Doris Breuer Steven A. Hauck II Monika Buske Martin Pauer Tilman Spohn 《Space Science Reviews》2007,132(2-4):229-260
The interior evolution of Mercury—the innermost planet in the solar system, with its exceptional high density—is poorly known.
Our current knowledge of Mercury is based on observations from Mariner 10’s three flybys. That knowledge includes the important
discoveries of a weak, active magnetic field and a system of lobate scarps that suggests limited radial contraction of the
planet during the last 4 billion years. We review existing models of Mercury’s interior evolution and further present new
2D and 3D convection models that consider both a strongly temperature-dependent viscosity and core cooling. These studies
provide a framework for understanding the basic characteristics of the planet’s internal evolution as well as the role of
the amount and distribution of radiogenic heat production, mantle viscosity, and sulfur content of the core have had on the
history of Mercury’s interior.
The existence of a dynamo-generated magnetic field suggests a growing inner core, as model calculations show that a thermally
driven dynamo for Mercury is unlikely. Thermal evolution models suggest a range of possible upper limits for the sulfur content
in the core. For large sulfur contents the model cores would be entirely fluid. The observation of limited planetary contraction
(∼1–2 km)—if confirmed by future missions—may provide a lower limit for the core sulfur content. For smaller sulfur contents,
the planetary contraction obtained after the end of the heavy bombardment due to inner core growth is larger than the observed
value. Due to the present poor knowledge of various parameters, for example, the mantle rheology, the thermal conductivity
of mantle and crust, and the amount and distribution of radiogenic heat production, it is not possible to constrain the core
sulfur content nor the present state of the mantle. Therefore, it is difficult to robustly predict whether or not the mantle
is conductive or in the convective regime. For instance, in the case of very inefficient planetary cooling—for example, as
a consequence of a strong thermal insulation by a low conductivity crust and a stiff Newtonian mantle rheology—the predicted
sulfur content can be as low as 1 wt% to match current estimates of planetary contraction, making deep mantle convection likely.
Efficient cooling—for example, caused by the growth of a crust strongly in enriched in radiogenic elements—requires more than
6.5 wt% S. These latter models also predict a transition from a convective to a conductive mantle during the planet’s history.
Data from future missions to Mercury will aid considerably our understanding of the evolution of its interior. 相似文献
142.
跨声速工况下流体诱发叶片振动研究 总被引:2,自引:0,他引:2
对同一跨声速风扇的非定常流场进行了跨声与亚声两种工况下的数值模拟.对两个工况下流场计算得到的转子叶片表面非定常气动激振力进行频谱分析,并对其进行对比分析,从而得到跨声工况下气动激振力特性.应用ANSYS软件的瞬态分析方法进行了叶片的强迫响应分析,对跨声和亚声两种工况下的叶片强迫响应进行对比分析,从而得到跨声工况下叶片强迫响应特性. 相似文献
143.
针对航天器在轨服务任务对绕飞技术的要求,研究了航天器受迫绕飞构型设计和控制问题。基于C-W(Clohessy-Wiltshire)方程的解析解,提出了双水滴拼接绕飞构型,并将单脉冲或双脉冲受迫绕飞延展至多脉冲绕飞构型设计;推导了伴随航天器初始状态变量与绕飞构型形状参数的关系,得到了4种构型的解析表达式和脉冲控制策略。通过数值仿真算例验证了设计的4种绕飞构型能够实现伴随航天器的慢速绕飞和快速绕飞,比较了不同绕飞构型的燃料消耗和绕飞距离误差。数值结果表明,双水滴拼接绕飞构型总脉冲最小。研究成果完善了航天器受迫绕飞构型设计与控制的相关理论,为工程应用提供参考。 相似文献
144.
145.
超燃冲压发动机隔离段非对称来流下激波串受迫振荡流动研究 总被引:7,自引:0,他引:7
用非对称马赫1.98的隔离段直连实验研究了不同波形不同频率的脉动反压对隔离段内流动的影响。实验结果表明:隔离段能有效地隔离不同频率不同波形周期性反压脉动对上游进气道的影响;反压脉动以第二特征波速向上游传播,但在激波振荡区域,压力脉动主要受激波振荡的影响;厚附面层一侧的下壁面激波振荡区域内压力脉动前传时以指数规律衰减,衰减的程度随着频率和波形的改变而改变。而薄附面层的上壁面激波振荡区域内压力脉动前传时不是单调下降,而是波动的。 相似文献
146.
147.
148.
低雷诺数下,翼型表面易于出现的分离转捩现象会降低翼型的气动性能,采用数值计算方法探讨了固定转捩在改善低雷诺数下翼型气动性能中的应用。定常来流下,雷诺数为4×104时,在翼型E387上表面自由转捩位置之前的一定位置处使翼型固定转捩,计算结果表明分离区减小了,升力系数和升阻比明显提高。振荡来流下,雷诺数在8×104的50%范围内变化时,分别计算了NACA4412在0°迎角和E387在3°迎角时自由转捩及在60%弦长处固定转捩的升阻特性,结果显示自由转捩的翼型当雷诺数减小时,性能急剧恶化,而采用固定转捩的翼型受其影响要小得多,具有更加稳定的气动性能。 相似文献
149.
V.V. Mishin V.M. Mishin Z. Pu S.B. Lunyushkin L.A. Sapronova U. Sukhbaatar D.G. Baishev 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2014
The magnetic flux of tail lobes Ψ is divided in two parts of comparable values Ψ1 and Ψ02, with the first that appears during substorm and the second, observed before substorm start. The first was named “new magnetic flux”, the second – “old magnetic flux”. The first, Ψ1, is known to play a definitive role in the energy transport from the solar wind into the magnetosphere-ionosphere-atmosphere system, but the role of Ψ02 in this transport is not well known. From the 27 August 2001 substorm data we study the involvement in the above transport process of the old flux Ψ02. This involvement is observed in the polar cap (PC) area, which existed prior to the substorm and is called respectively “the old PC”. In this study, as distinct from earlier works, we use the balance equation of the energy stored in magnetosphere and energy consumed. Activation of the old PC magnetic flux Ψ02 was found to increase the energy input by ∼85% in the event under consideration. 相似文献
150.
The natural damped frequencies and the response to translational excitation of a viscous liquid in a circular cylindrical container are obtained. The response of the liquid surface elevation above its equilibrium position, as well as the viscous liquid force in x-direction due to translational excitation in this direction have been numerically evaluated. In this analysis the side wall adhesive boundary conditions have been satisfied, while only the normal bottom condition has been observed. This makes the results of the analysis applicable to liquid height ratio h/a>1. 相似文献