基于多值决策图的温储备系统可靠性建模方法

温储备系统是冷储备与热储备系统的推广,在实际中有广泛应用。针对不可修温储备系统的可靠性建模问题,已有基于多值决策图(MDD)的系统可靠性建模方法。该方法以系统中的单元故障为建模对象,分别构建故障级MDD与系统级MDD,进而获得系统可靠度的解析表达式。然而,该表达式中不同维度积分相互混杂,计算给定时刻的系统可靠度需要首先梳理系统可靠度的表达式,以利用数值方法求解其中的积分。为实现系统可靠度的程序化计算,在已有研究基础上提出将系统级MDD按故障数分解为一系列子决策图,通过对MDD中边的概率重新赋值获得每一子决策图的发生概率,得到系统可靠度的规范形式,形成一套完整的系统可靠度计算方法。      

利于减少配平损失的太阳能飞机构型设计

针对具有静稳定性的太阳能飞机一般采用尾翼配平造成气动配平损失的问题,提出了一种“T”构型太阳能飞机。概述该太阳能飞机的总体构型,分析该构型飞机巡航状态下降低重心的自配平原理,建立能量平衡和质量分析模型,给出适合于该构型太阳能飞机的概念设计方法,并优化构型设计参数。结果表明,“T”构型太阳能飞机不仅具有静稳定性,还降低了配平损失。在巡航状态下,“T”构型太阳能飞机单位面积平飞需用功率比常规构型太阳能飞机减少了6.2%,具有明显的应用效果。      

深空环境下热防护材料的研究及应用进展

随着对太空探索的深入,空间飞行器所面临的环境也越趋恶劣:太空飞行过程中的高温羽流防护,高速返回再入过程中高温气动加热;长时间日光下飞行会使飞行器表面温度越来越高;一些星球上高温的大气环境导致人类现有制造飞行器的材料无法抵挡。本文搜集国内外先进热防护系统研究资料,了解重点发展方向,介绍了我国神舟飞船热防护材料以及已经开发出的新型轻质高效热防护材料,为我国今后用于恶劣环境下的飞行器材料提供一些信息和材料基础。     

细长旋成体大迎角绕流中的头涡与卡门涡的脉动压力特性

在迎角很大时细长旋成体背部流场沿轴向通常有两个截然不同的区域,其中卡门涡脱落区域位于后体,而头涡区域靠近旋成体头部。为了寻求两者的区别与联系,在两个风洞中分别用两个细长体模型进行测压和流动显示实验,得到了沿旋成体轴向不同区域的压力脉动特征,即头涡的脉动幅度相对卡门涡较大,而频谱峰频率则较低,而且随着迎角的进一步增大,头涡区会完全消失。     

大迎角细长体头涡结构演变的非定常现象研究

细长旋成体绕流中位于尖部附近的一对头涡在迎角增至一定程度时,会表现出很强的非定常特征,而此时后体上为类卡门涡脱落区域。为了寻找这对头涡的非定常特征随迎角变化的规律,在两个风洞中分别用两个细长体模型进行测压和流动显示实验,得到了在很大迎角下旋成体头涡的脉动频率随迎角基本呈线性变化的规律,而后体上的卡门涡脱落频率则与迎角的正弦值成正比。     

航空电子设备NSEE试验评价方法

本文定义了航空电子设备大气中子单粒子效应(NSEE)硬失效、硬错误与软错误等大气中子辐射可靠性表征参数,提出了一套航空电子设备抗大气中子单粒子效应危害能力的试验评价方法,包括试验应力终止条件与起始条件的确定方法、M_NSEE预估方法、试验程序、试验评价方法等,并通过某航空用卫星导航接收机试验案例证明了该方法在工程应用中的可操作性与有效性,通过掌握数字信号处理(DSP)、静态随机存储器(SRAM)、现场可编程门阵列(FPGA)的NSEE敏感特性,可为航空用卫星导航接收机NSEE危害防控提供针对性的技术支持.本文为我国航空电子产品大气中子单粒子效应试验评价奠定了理论与应用基础,同时也为其他电子信息产品在大气中子单粒子效应试验评价方面提供了重要依据和参考.      

Using the radial basis function neural network to predict ionospheric critical frequency of F2 layer over Wuhan

Neural networks (NNs) have been applied to ionospheric predictions recently. This paper uses radial basis function neural network (RBF-NN) to forecast hourly values of the ionospheric F₂ layer critical frequency(f_oF₂), over Wuhan (30.5N, 114.3E), China. The false nearest neighbor method is used to determine the embedding dimension, and the principal component analysis (PCA) is used to reduce noise and dimension. The whole study is based on a sample of about 26,000 observations of f_oF₂ with 1-h time resolution, derived during the period from January 1981 to December 1983. The performance of RBF-NN is estimated by calculating the normalized root-mean-squared (NRMSE) error, and its results show that short-term predictions of f_oF₂ are improved.     

Cluster observations showing the indication of the formation of a modified-two-stream instability in the geomagnetic tail

This study presents several observations of the Cluster spacecraft on September 24, 2003 around 15:10 UT, which show necessary prerequisites and consequences for the formation of the so-called modified-two-stream instability (MTSI). Theoretical studies suggest that the plasma is MTSI unstable if (1) a relative drift of electrons and ions is present, which exceeds the Alfvèn speed, and (2) this relative drift or current is in the cross-field direction. As consequences of the formation of a MTSI one expects to observe (1) a field-aligned electron beam, (2) heating of the plasma, and (3) an enhancement in the B-wave spectrum at frequencies in the range of the lower-hybrid-frequency (LHF). In this study we use prime parameter data of the CIS and PEACE instruments onboard the Cluster spacecraft to verify the drift velocities of ions and electrons, FGM data to calculate the expected LHF and Alfvèn velocity, and the direction of the current. The B-wave spectrum is recorded by the STAFF instrument of Cluster. Finally, a field aligned beam of electrons is observed by 3D measurements of the IES instrument of the RAPID unit. Observations are verified using a theoretical model showing the build-up of a MTSI under the given circumstances.     

Latitudinal variation of the topside electron temperature at different levels of solar activity

A database of electron temperature (T_e) measurements comprising of most of the available satellite measurements in the topside ionosphere is used for studying the solar activity variations of the electron temperature T_e at different latitudes, altitudes, local times and seasons. The T_e data are grouped into three levels of solar activity (low, medium, high) at four altitude ranges, for day and night, and for equinox and solstices. We find that in general T_e changes with solar activity are small and comparable in magnitude with seasonal changes but much smaller than the changes with altitude, latitude, and from day to night. In all cases, except at low altitude during daytime, T_e increases with increasing solar activity. But this increase is not linear as assumed in most empirical T_e models but requires at least a parabolic approximation. At 550 km during daytime negative as well as positive correlation is found with solar activity. Our global data base allows to quantify the latitude range and seasonal conditions for which these correlations occur. A negative correlation with solar activity is found in the invdip latitude range from 20 to 55 degrees during equinox and from 20 degrees onward during winter. In the low latitude (20 to −20 degrees invdip) F-region there is almost no change with solar activity during solstice and a positive correlation during equinox. A positive correlation is also observed during summer from 30 degrees onward.