三维热化学非平衡流动非结构网格DSMC方法及其应用

研究了过渡流域三维热化学非平衡流动DSMC方法实现的过程.以四面体非结构网格为基本单元,提出一种新型的高效搜索算法,该算法不仅可以快速跟踪模拟分子在网格之间的迁移,而且可以准确判别分子与物面是否相互作用,避免了原有算法中分子表面反射的非确定论判据.设计了适合三维DSMC方法的动态局部时间步长技术,节约了计算时间.将碰撞距离的思想引入到非结构网格上来,有效地消除了网格尺度小于三分之一平均自由程的限制.利用Foaran90的动态分配内存技术编制了适用于任意外形的通用计算程序.最后对全尺寸航天飞机高超声速绕流进行了数值试验,计算结果验证了该算法的可行性及高效性.     

航天器振动试验中的动力吸振现象

振动环境试验是考验航天器中各分机力学品质的重要试验,分机适应力学环境的能力在设计阶段必须充分考虑。目前分机的力学环境条件往往是在考虑了一定的安全系数后,以分机安装处界面的加速度包络曲线给出的。然而一般来说,分机振动试验过程中的边界条件与分机实际工作状态的边界条件是不同的。具体地说就是在振动试验过程中分机通过试验转接托架与振动台面相连,实际工作状态是分机安装在安装件(卫星各舱板)上。由于试验转接托架与安装件的动力学特性不一样,根据多自由度弹簧质量阻尼系统的动力吸振原理,可以推出试验状态分机在固有频率处存在过试验现象。为了减少过试验对分机带来的危害,新的试验方法研究(加速度响应限幅控制、阻抗特性模拟法、限力技术等)已成为国内外航天工作者研究的热点。文章详细阐述了振动试验中动力吸振的机理及过试验产生的缘由。     

Precipitating Protons and Their Role in Ionization of the Polar Ionosphere

Spatial distributions of the electron density in the latitude range 60°–90° N were calculated on the basis of a physical model of the E and lower Fregions of the high-latitude ionosphere using statistical models of auroral proton and electron precipitation. It is shown that precipitating protons can play the key role in the ionization of the Eregion in the dusk and midnight sectors of the auroral oval. However, quantitative estimates of the contribution of protons to the ionization depend on the used statistical models of electron precipitation. Comparison of the electron density profiles calculated for two incoherent scatter radars, EISCAT (Tromsö) and ESR (Svalbard), for simultaneous precipitation of electrons and protons and for electron precipitation only show that the influence of protons is the most significant in the dusk sector over the EISCAT radar and in the midnight sector over the ESR radar. The results presented indicate the need to take protons into account when radar data are used to derive precipitating electron spectra.     

Determination of the Microacceleration Quasisteady Component onboard the International Space Station

A comparison of two methods of determination of the microacceleration quasisteady component arising onboard the International Space Station was performed. In the first method the acceleration was calculated using the relative motion of the station reconstructed on the basis of telemetry data. The second method was a direct measurement of the microacceleration by a low-frequency accelerometer and a smoothing of the data obtained. The used measurements were made by the American accelerometer MAMS. The above comparison can theoretically be used to refine the position of the station center of mass relative to its body.     

Airglow in the Visible and Infrared Spectral Ranges of the Disturbed Upper Atmosphere under Conditions of High-Velocity Plasma Jet Injection: I. Experimental data

The measurements of infrared emission from an artificial structure, which was generated during the Fluxus experiment with plasma jet injection into the atmosphere, are obtained and discussed for the first time. Additional experimental data on the airglow in the visible spectral band of the disturbed region of the atmosphere are presented. A generalized analysis of the data is given.     

柔性多体撞击系统的精细H∞控制研究

本文在柔性多体撞击系统动力学方程的基础上 ,将撞击看成是一种扰动 ,设计了一个稳定的控制器以使撞击扰动对控制输出的影响达到最小的目的 ,在分析过程中采用 H∞ 控制原理对该问题进行了研究。在计算中 ,将精细积分法应用于状态动力学方程和 Riccati方程的求解中 ,使计算精度得到大幅度提高。最后通过数值例题说明了本文方法的有效性     

固体火箭发动机地面性能换算成真空性能研究

根据固体火箭发动机内弹道计算模型，分析了使用大扩张比喷管地面静止试验性能与真空性能之间的联系，建立了由地面性能换算成真空性能的方法，计算出的真空推力、真空比冲等数据与实际相符。     

单一基准径向圆跳动误差的新测量法

用传统的测量方法不能得到单一基准径向圆跳动误差的准确值。根据单一基准径向圆跳动误差的定义建立了该项误差的正交最小二乘评定数学模型。在万能工具显微镜上得到了采样数据并给出了微机数据处理结果。     

同轴度误差的矩阵计算机法

用矩阵法建立了同轴度误差最小二乘评定数学模型,给出了一组采样数据、微机数据处理程序和同轴度误差值。     

KuaFu Mission

The KuaFu mission-Space Storms, Aurora and Space Weather Explorer-is an "L1+Polar" triple satellite project composed of three spacecraft: KuaFu-A will be located at L1 and have instruments to observe solar EUV and FUV emissions, and white-light Coronal Mass Ejections (CMEs), and to measure radio waves, the local plasma and magnetic field,and high-energy particles. KuaFuB1 and KuaFu- B2 will bein polar orbits chosen to facilitate continuous 24 hours a day observation of the north polar Aurora Oval. The KuaFu mission is designed to observe the complete chain of disturbances from the solar atmosphere to geospace, including solar flares, CMEs, interplanetary clouds, shock waves, and their geo-effects, such as magnetospheric sub-storms and magnetic storms, and auroral activities. The mission may start at the next solar maximum (launch in about 2012), and with an initial mission lifetime of two to three years. KuaFu data will be used for the scientific study of space weather phenomena, and will be used for space weather monitoring and forecast purposes. The overall mission design, instrument complement, and incorporation of recent technologies will target new fundamental science, advance our understanding of the physical processes underlying space weather, and raise the standard of end-to-end monitoring of the Sun-Earth system.