基于多可信度代理模型的尾喷管优化设计

尾喷管是飞行器机体/推进一体化设计中的关键部件之一,直接影响着飞行器的推阻匹配、俯仰力矩配平等特性。为了提高尾喷管优化设计效率,建立基于多可信度代理模型的多目标优化模型。以基于粗网格、无黏模型的CFD 结果作为低可信度数据,以基于细密网格、SST k-ω 湍流模型的CFD 结果作为高可信度数据,将最大化推力系数、升力系数和俯仰力矩系数作为优化目标,构建Cokriging 模型,并结合NSGA-Ⅱ算法得到Pareto 解集。结果表明：以上三个目标分别提升了2.94%、13.0% 和40.6%,误差低于0.5%,并进行了敏感性分析;优化后流场波系结构更为复杂,改变了壁面压强分布规律;与Kriging 模型相比,Cokriging 模型具有相当的预测性能,构建时间成本节省了62%。     

歼击机纵向多模态控制规律设计方法初探

一、问题的提出 多模态控制规律在现代飞行控制系统中得到广泛应用。由于采用多控制面控制飞机的机动运动,仅仅采用仿真的方法来选择控制律的参数是很困难的。在此,我们对AFTI/F-16飞机多模态飞行控制规律按已知控制律结构及基本设计思想进行设计,探索其主要通道的基本功能及参数选择方法,以便对其系统设计方法进行深入探讨和分析。     

卫星表面接触式加热法

本文从电加热片模拟空间外热流技术的原理出发,介绍了这一技术的特点和具体的实施方法,并详细讨论了试验中可能引起的误差和预防的措施。     

并行加工系统一类排序问题的最优解

讨论了将多个零件分派给并行加工系统加工的排序问题.假设同一零件分配给不同的设备,其加工时间不同,分析了使所有零件的总花费时间(加工时间与等待时间之和)最小的排序方法.首先建立了该类问题的数学模型,然后将其转化为指派问题,通过匈牙利算法可以得到最优解.所得算法的时间复杂性是多项式界的.最后给出了一个数值例子说明求解过程.     

液体火箭发动机环境因子的修正逆矩估计

对文献 [1]提出的适用于大样本失效数据的逆矩估计法进行修正 ,针对液体火箭发动机飞行及地面试车数据的特点 ,提出了其天地环境因子的修正逆矩估计方法。与现有方法相比 ,本文提出的方法更加适用于小样本失效数据情形下环境因子问题的研究。最后用数值例说明了该方法的应用     

真空汽相焊冷却速率对多层板焊点质量的影响

为解决多层印制板真空汽相焊由于焊后冷却不足导致的焊点纹路问题,本文确定多层板焊点纹路出现的根本原因,对焊后冷却区进行改造,进而研究不同焊接工艺对焊点表面形貌、内部组织形貌及焊点力学性能的影响。实验结果表明,快冷下焊点形成的界面金属化合物（IMC）更薄,焊点组织也更加均匀,即Pb在Sn中的分布更弥散。快冷下形成的IMC层晶粒直径在1μm左右,剪切强度为17.26 MPa,较慢冷提高了43%,达到细晶强化的目的。此外,由于冷却速度过慢导致的焊点表面纹路缺陷也得到明显改善。     

考虑测量约束的非合作目标近距离快速导引控制方法

研究了考虑测量约束的非合作目标近距离快速导引控制方法。首先,基于C-W方程建立了解析形式的径切联合近距离快速导引控制模型,并采用微分修正方法将解析结果进行修正;然后推导了任意初始条件下,径切联合控制双脉冲与视场角的解析关系;最后基于相对偏心率矢量建立了径切联合控制的控后效果评估模型。仿真结果表明:提出的控制方法和控后效果评估模型有效。     

天基微小空间碎片探测研究

随着空间碎片数量的不断增多,天基微小空间碎片探测已经成为一个热点．首先介绍了空间碎片在低地球轨道上的分布情况以及它对于航天器的危害,然后介绍了国外微小碎片探测器的基本情况,并在这些探测结果的基础上提出了一个探测器方案．这种探测器的传感器采用了新型的压电材料聚偏二氟乙稀(PVDF),使用了飞行时间法(TOF)准确测定空间碎片的飞行速度,以及快脉冲分析系统分析碎片的质量．     

A self-similar solution of a curved shock wave and its time-dependent force variation for a starting flat plate airfoil in supersonic flow

The problem of aeroelasticity and maneuvering of command surface and gust wing interaction involves a starting flow period which can be seen as the flow of an airfoil attaining suddenly an angle of attack. In the linear or nonlinear case, compressive Mach or shock waves are generated on the windward side and expansive Mach or rarefaction waves are generated on the leeward side. On each side, these waves are composed of an oblique steady state wave, a vertically-moving one-dimensional unsteady wave, and a secondary wave resulting from the interaction between the steady and unsteady ones. An analytical solution in the secondary wave has been obtained by Heaslet and Lomax in the linear case, and this linear solution has been borrowed to give an approximate solution by Bai and Wu for the nonlinear case. The structure of the secondary shock wave and the appearance of various force stages are two issues not yet considered in previous studies and has been studied in the present paper. A self-similar solution is obtained for the secondary shock wave, and the reason to have an initial force plateau as observed numerically is identified. Moreover, six theoretical characteristic time scales for pressure load variation are determined which explain the slope changes of the time-dependent force curve.     

Validation on MERSI/FY-3A precipitable water vapor product

The precipitable water vapor is one of the most active gases in the atmosphere which strongly affects the climate. China's second-generation polar orbit meteorological satellite FY-3A equipped with a Medium Resolution Spectral Imager (MERSI) is able to detect atmospheric water vapor. In this paper, water vapor data from AERONET, radiosonde and MODIS were used to validate the accuracy of the MERSI water vapor product in the different seasons and climatic regions of East Asia. The results show that the values of MERSI water vapor product are relatively lower than that of the other instruments and its accuracy is generally lower. The mean bias (MB) was ?0.8 to ?12.7?mm, the root mean square error (RMSE) was 2.2–17.0?mm, and the mean absolute percentage error (MAPE) varied from 31.8% to 44.1%. On the spatial variation, the accuracy of MERSI water vapor product in a descending order was from North China, West China, Japan -Korea, East China, to South China, while the seasonal variation of accuracy was the best for winter, followed by spring, then in autumn and the lowest in summer. It was found that the errors of MERSI water vapor product was mainly due to the low accuracy of radiation calibration of the MERSI absorption channel, along with the inaccurate look-up table of apparent reflectance and water vapor within the water vapor retrieved algorithm. In addition, the surface reflectance, the mixed pixels of image cloud, the humidity and temperature of atmospheric vertical profile and the haze were also found to have affected the accuracy of MERSI water vapor product.