舰载机着舰时航迹稳定性研究

本文讨论了舰载飞机以小于有利速度着舰时的航迹稳定性问题。在分析飞机航迹稳定性的同时,还对油门杆控制、机动襟翼控制对改善航迹稳定性的作用进行了初步探讨;在此基础上还讨论了舰载飞机加装波束导引系统对着舰过程的影响原理。结果表明:采用油门杆控制、机动襟翼控制来改善着舰阶段的航迹稳定性是可行的:而且用以上两控制系统作为内环的自动驾驶仪在波束导引系统自动导引飞机着舰过程中,能控制飞机的飞行速度、高度,帮助驾驶员操纵。     

Emergence of a Habitable Planet

We address the first several hundred million years of Earth’s history. The Moon-forming impact left Earth enveloped in a hot silicate atmosphere that cooled and condensed over ∼1,000 yrs. As it cooled the Earth degassed its volatiles into the atmosphere. It took another ∼2 Myrs for the magma ocean to freeze at the surface. The cooling rate was determined by atmospheric thermal blanketing. Tidal heating by the new Moon was a major energy source to the magma ocean. After the mantle solidified geothermal heat became climatologically insignificant, which allowed the steam atmosphere to condense, and left behind a ∼100 bar, ∼500 K CO₂ atmosphere. Thereafter cooling was governed by how quickly CO₂ was removed from the atmosphere. If subduction were efficient this could have taken as little as 10 million years. In this case the faint young Sun suggests that a lifeless Earth should have been cold and its oceans white with ice. But if carbonate subduction were inefficient the CO₂ would have mostly stayed in the atmosphere, which would have kept the surface near ∼500 K for many tens of millions of years. Hydrous minerals are harder to subduct than carbonates and there is a good chance that the Hadean mantle was dry. Hadean heat flow was locally high enough to ensure that any ice cover would have been thin (<5 m) in places. Moreover hundreds or thousands of asteroid impacts would have been big enough to melt the ice triggering brief impact summers. We suggest that plate tectonics as it works now was inadequate to handle typical Hadean heat flows of 0.2–0.5 W/m². In its place we hypothesize a convecting mantle capped by a ∼100 km deep basaltic mush that was relatively permeable to heat flow. Recycling and distillation of hydrous basalts produced granitic rocks very early, which is consistent with preserved >4 Ga detrital zircons. If carbonates in oceanic crust subducted as quickly as they formed, Earth could have been habitable as early as 10–20 Myrs after the Moon-forming impact.     

Modelling of Ejecta as a Space Debris Source

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.     

一种改进的翼型设计方法

本文将翼型的设计问题转化成多元函数求极值问题来求解,提出了一种改进的翼型设计方法,可用于考虑粘性影响时的亚临界翼型设计。     

Numerical Simulation of Impact Loading on Solid Propellant Within an Orthotropic Shell

The strain–stress state of the solid propellant rocket engines (SPREs) is simulated under impact. The effect of orientation of elastic and strength properties of orthotropic organoplastic shell material on the strain–stress state of the solid propellant is investigated. Normal and oblique impact of single steel cylinder projectiles, both simultaneous and at different times of multiple, converging steel spheric particles with SPRE are investigated in this study. The investigation is conducted numerically. The numerical modeling was carried out in a three-dimensional formulation by the method of finite elements for the continuous approach of the mechanics of a deformable solid. The destruction of the anisotropic material is described by the tensor-polynomial criterion of the fourth degree, which takes into account the influence of hydrostatic pressure.     

基于双目视觉的返回舱着陆横向速度测量

通过分析返回舱在着陆时所具有的水平速度也可能对着陆安全构成威胁的事实，论述了为返回舱增加横向缓冲装置的必要性，由此提出亟需解决的问题——在返回舱着陆下降过程中测量其水平运动速度。提出了全新概念的以视觉图像为唯一信息来源的返回舱水平速度测量方法，仅以双目摄像机系统作为传感器，避免了对返回舱原有传感器系统的改造。通过对着陆区域地面图像的采集和在线处理，利用双目交会测量原理得到返回舱当前的大地坐标和姿态。仿真实验证明，方法简单易行，测量结果可靠。     

大型弹体发射速度测量方法的研究

大弹体的发射速度是各种弹体飞行控制中的重要参数。由于弹体尺寸大、发射时间短等原因，因而对发射速度的快速实时测量难于保证精度。本文提出一种“双测头光电反射式速度测量系统”，它采用“双路平衡式光电传感系统”接收信号，可实现各种大型物体（如导弹、火箭）的发射速度测试，在0－50m/s内，其相对误差小于1％，且安装调工方便，方法具有实用价值。     

非线性PD型比例导引鲁棒性研究

为研究存在视线角速度测量噪声时非线性比例微分(PD)型比例制导方案的鲁棒性,以近距大离轴角发射和目标大机动为拦截条件,对四种视线角速度测量噪声方差进行蒙特卡罗仿真模拟。结果表明,非线性PD型比例制导方案抗视线角速度测量噪声的鲁棒性强,对机动目标拦截制导精度高,是一种具工程应用价值的高精度末制导方案。     

关于多普勒频率转换成距离变化率公式的讨论

利用多普勒效应原理对雷达测速的转换公式进行了讨论，指出在飞行器高精度轨道测量中，现行的测速转换公式存在较大的误差；给出了新的包含二阶项的测速转换公式，并导出了一个简便实用的直接在测量数据上进行该项误差修正的方法，同时进行了误差特性分析。实际计算表明：轨道测量数据进行二次修正后，匹配程度明显优于修正前。     

0.4C-铬镍钼硅钢多冲疲劳裂纹起始寿命估算

 本文采用局部应力一应变法,结合Coffin公式,忽略弹性应变。考虑应变速率的影响,导出了在给定的试验条件下,根据材料的拉伸性能估算其多冲疲劳裂纹起始寿命的表达式,经试验结果验证表明,对不同冲击能量,不同热处理状态以及不同缺口形状的多冲试样,估算式均具有较高的准确性。