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11.
Mercury’s unusually high mean density has always been attributed to special circumstances that occurred during the formation of the planet or shortly thereafter, and due to the planet’s close proximity to the Sun. The nature of these special circumstances is still being debated and several scenarios, all proposed more than 20 years ago, have been suggested. In all scenarios, the high mean density is the result of severe fractionation occurring between silicates and iron. It is the origin of this fractionation that is at the centre of the debate: is it due to differences in condensation temperature and/or in material characteristics (e.g. density, strength)? Is it because of mantle evaporation due to the close proximity to the Sun? Or is it due to the blasting off of the mantle during a giant impact? In this paper we investigate, in some detail, the fractionation induced by a giant impact on a proto-Mercury having roughly chondritic elemental abundances. We have extended the previous work on this hypothesis in two significant directions. First, we have considerably increased the resolution of the simulation of the collision itself. Second, we have addressed the fate of the ejecta following the impact by computing the expected reaccretion timescale and comparing it to the removal timescale from gravitational interactions with other planets (essentially Venus) and the Poynting–Robertson effect. To compute the latter, we have determined the expected size distribution of the condensates formed during the cooling of the expanding vapor cloud generated by the impact. We find that, even though some ejected material will be reaccreted, the removal of the mantle of proto-Mercury following a giant impact can indeed lead to the required long-term fractionation between silicates and iron and therefore account for the anomalously high mean density of the planet. Detailed coupled dynamical–chemical modeling of this formation mechanism should be carried out in such a way as to allow explicit testing of the giant impact hypothesis by forthcoming space missions (e.g. MESSENGER and BepiColombo). 相似文献
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When a micro-debris or a micrometeoroid impacts a spacecraft surface, a large number of secondary particles, called ejecta, are produced. These particles can contribute to a modification of the debris environment: either locally by the occurrence of secondary impacts on the components of complex and large space structures, or at great distance by the formation of a population of small orbital debris. This paper describes firstly, the ejecta overall production, and secondly, the lifetime and the orbital evolution of the particles. Finally the repartition of ejecta in LEO is computed. Some results describing the population as a function of size and altitude are presented. 相似文献
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空战机动动作库设计方式研究 总被引:13,自引:0,他引:13
具体阐述了两类常见空战动作库的设计 :典型战术动作库和基本操作动作库 ,详细分析了这两类空战机动动作库的不足 ,最后提出了改进动作库设计的具体意见和建议。 相似文献
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本文研究的是四维飞行性能管理系统的核心环节-飞机在终端区域内的四维下降技术,首先探讨了基于常值航迹角的定常M数/指示空速下降飞行技术,论述了其高度剖面的构成与特点,通过尤拉积分方法求解飞机运动方程,实现了高度冲面的解算。其次开发了对速度剖面的迭代过程,选取原则及方法。本文在进行理论分析的同时,还开发了满意的仿真软件,一了其应用价值。 相似文献
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逆合成孔径雷达信号处理方法研究进展 总被引:3,自引:0,他引:3
朱兆达 《南京航空航天大学学报》1995,27(1):59-66
在简要评述国内外现有的逆合成孔径雷达(ISAR)信号处理的运动补偿和成象方法之后,介绍了南京航空航天大学ISAR课题组近年来在ISAR信号处理方法研究中取得的主要进展,包括基于多散射点定位观点的雷达成象观测模型,基于最大似然原理的同时运动补偿和成象方法,基于最大似然原理的多目标成象方法和基于时频分析的多目标成象方法,以及超分辩成象方法,文末指出了在ISAR信号处理方面有待进一步研究的问题。 相似文献
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目前电子对抗系统广泛使用的数字储频技术主要是通过采样、存储和复制产生干扰信号.阐述了基于采样技术的信号重构及其基本原理,重点介绍分析了在此基础上利用信号处理技术,合成产生干扰信号的原理和方法. 相似文献